.
EXTRA DIVISION, INNER HOUSE, COURT OF SESSION
|
Lord Osborne
Lord Kingarth
Lord Wheatley
|
[2008] CSIH 18
A304/01
OPINION OF THE COURT
delivered by LORD OSBORNE
in
RECLAIMING MOTION
in the cause
KELLY ELIZABETH MORTON
(A.P.)
Pursuer and Reclaimer;
against
WEST LOTHIAN COUNCIL
Defenders and Respondents:
_______
|
Act: D. Batchelor Q.C,
Primrose, Balfour + Manson LLP. (Pursuer
and Reclaimer)
Alt: L. Murphy Q.C, McBrearty, Simpson
& Marwick W.S. (Defenders and Respondents)
20 February 2008
The background
circumstances
[1] At about 9 a.m. on Saturday 23
December 1995,
the reclaimer was driving a Vauxhall Astra motor car in an easterly direction
along the B9080 road from Linlithgow to Kirkliston. The road is a two-way road, carrying a single
lane of traffic in each direction. She was travelling behind a bus. As the bus reached a junction, which may be
referred to as the "Bridgend junction", between that road and an unclassified
road leading to Bridgend, which may be referred to as the "Bridgend Road", the
driver of the bus indicated his intention to turn right and moved into the
filter lane which allowed traffic intending to turn right to wait in the middle
of the two carriageways until it was safe to do so. The bus was unable to turn right immediately,
due to the presence of an oncoming vehicle.
As the bus moved into the filter lane, the reclaimer passed it on its
nearside. As she did so, her car skidded
on a patch of black ice, as a result of which she lost control of it. Her car skidded broadside across the road and
into the path of a Rover 800 vehicle coming in the other direction. The Rover struck the passenger door of the
reclaimer's car. As a result of the collision,
the passenger in the reclaimer's car was killed and she herself sustained
serious head injuries. In the present
action, the reclaimer seeks damages in respect of those injuries. It should be recorded that the circumstances
of the accident, just narrated, are the subject of admission on record. Further, a Joint Minute has been lodged in
process, in which, first, quantum of
damages has been agreed, in the event of the respondents being found liable; and
secondly, it is agreed that, in consequence of the head injuries sustained by
her, the reclaimer has no memory of the circumstances of the accident. No issue is raised in the pleadings
concerning any fault on the part of the reclaimer, or on the part of the driver
of the Rover 800 vehicle.
[2] At the time
of the accident, the former Lothian Regional Council, as roads authority for
the relevant area in terms of the Roads (Scotland) Act 1984, were responsible for the
management and maintenance of the B9080 road.
In terms of the Local Government (Scotland) Act 1994, the respondents have now
succeeded to the rights and liabilities of Lothian Regional Council, in respect
of their management and maintenance of roads in West Lothian, including the B9080 road. In this action, the reclaimer contends that
the accident was caused by the fault and negligence of Lothian Regional Council,
for whose acts and omissions the respondents are now liable. Since there is no dispute that the respondents
are indeed liable for the acts and omissions of Lothian Regional Council in the
area of responsibility concerned, it is convenient to refer to the respondents
and to their predecessors, Lothian Regional Council, as "the Council".
[3] The reclaimer
contends, in Condescendence 3, that the Council were under several duties: to
take reasonable care for the safety of those, such as the reclaimer, using the
roads for which they were responsible in terms of the 1984 Act; to take reasonable care to have regard to the
prevailing weather conditions within the area and to salt the road as
necessary; to take reasonable care to
ensure that the system of salting they operated provided for the salting of all
areas of carriageway on the primary routes such as the B9080 road; to take reasonable care to ensure that the
routes adopted by their gritting lorries were such that all areas of
carriageway on primary routes, such as that road, were salted; to take reasonable care to ensure that no
areas of carriageway were missed by the gritting lorries as a result of the
route taken by them; and to take reasonable care to ensure that the area of the
eastbound carriageway of the B9080 road opposite the Bridgend junction was
salted. The reclaimer contends that the
Council failed in such duties and thus caused the accident. Seperatim,
in Condescendence 4 the reclaimer avers that the accident was caused by the
fault and negligence of the gritting crews who had undertaken the gritting at
the material time, for whose acts and omissions the Council were vicariously
liable. She avers that they were under
the following duties: to take reasonable care to ensure that all areas of the
B9080 carriageway were salted: to take reasonable care not to miss out any
areas of carriageway from their route when gritting the road; to take reasonable care to ensure that they
adopted a route that allowed all areas of the carriageway to be salted; and to
take reasonable care to salt areas of the carriageway such as the area of the
eastbound carriageway opposite the Bridgend junction, to ensure that all such
areas received a coating of salt.
[4] By way of
explanation of the background to the form of certain of the averments of duty
which we have quoted it should be noted that the reclaimer averred that, when
the gritting lorries approached the locus of the accident from the direction of
Linlithgow, lying to the west of the locus, they turned up the westernmost arm
of the Y junction with the road to Bridgend, thereby leaving the traffic island
at the junction to the nearside of the vehicles. The gritting crews proceeded to Bridgend,
turned round and proceeded back down the unclassified road to the junction with
the B9080 road. When they reached the
junction they proceeded to exit back onto the B9080 road by means of the
easternmost arm of the Y junction, again leaving the traffic island on the
nearside of the gritting lorry. When the
gritting lorries approached the locus from the east, the reclaimer believes and
avers that they turned left up the unclassified road to Bridgend, or passed by
the locus on the westbound carriageway.
Due to the route adopted by the gritting lorries, the area of eastbound
carriageway opposite the north side of the traffic island and beyond the filter
lane was outwith the reach of the spreading device on the lorries and was not
treated with salt. Ice was accordingly
liable to build up on the surface of the carriageway in that area creating a
hazard to motorists such as the reclaimer.
The route adopted around the traffic island did not allow grit to reach
the area of the eastbound carriageway opposite the north side of the traffic
island.
[5] It should
also be recorded that the Council aver that the B9080 road formed part of a
prescribed gritting route, known as L3, for vehicles on salting duties. That route had been salted by gritting crews employed
by the Council between 5.23 pm and 6.30 pm on 22
December 1995,
between 11.15 pm on 22 December 1995 and 1.30 am on 23
December 1995,
and between 5.40 am and 7.00 am on 23
December 1995. They also aver that on each occasion, the L3
route, including the locus of the accident had been adequately salted on both
lanes of the carriageway. The L3 route
was a circular route. The road between
the B9080 road and Bridgend did not form part of the L3 route. Accordingly, the whole of the L3 route had
been salted, including the carriageway opposite the traffic island at the
junction to Bridgend. At points on the
route where the carriageway consisted of two lanes, the gritter was set so as
to spread a sufficient quantity of salt over both lanes. On each occasion that route was salted, the
gritter was driven in the opposite direction to the direction in which it had
last been driven, thereby ensuring an even spread of salt. On approaching the filter lane in the middle
of the carriageway, to be used by traffic intending to turn right towards
Bridgend, the drivers of the gritting lorries altered the gritters' settings so
that a wider area with a greater amount of salt was covered. That change in setting allowed the entire
carriageway at that junction to be salted.
[6] It is also of
importance to note that the reclaimer avers at the end of Condescendence 2
that, had the L3 route been adequately salted on both lanes of the carriageway
by the Council in the manner that they averred and, in particular, salted
between 5.40 am and 7.00 am on 23 December 1995, black ice would not have
formed at the locus by the time of the accident. In these circumstances, it is averred that
the employees of the Council did not take reasonable care to see that all areas
of the B9080 road and, in particular, the locus of the accident were adequately
treated with salt so as to prevent the formation of black ice by the time of
the said accident.
[7] The reclaimer
also avers that the Council had obtained a 24 hour weather forecast for the relevant
area at midday on 22 December 1995.
That forecast covered the period from mid-day on that date to mid-day on
23 December 1995. The forecast
was updated by later bulletins at 3.55 pm and 9.00 pm.
The initial forecast was that rain would turn to sleet overnight with
snow above five hundred feet. The
minimum road temperature was forecast to be 0 degrees centigrade. The road temperature was identified as a
hazard to traffic. The update obtained
at 3.55 pm suggested a slight deterioration compared with the previous
weather forecast, with snow expected at lower levels and earlier than
previously forecast. The updated
forecast at 9.00 pm suggested further deterioration predicting slight snow at
all levels by morning and icy stretches on roads. The minimum expected temperature was reduced
to -1 degree centigrade. The Code of
Practice "Winter Maintenance for Trunk Roads", published by the Scottish Office
in 1993 and in accordance with which the Council operated their gritting
policy, stated that it was good practice to grit when the temperature fell to 1
degree above freezing. Accordingly, having regard to that code and the
meteorological information in their possession, the council knew or ought to
have known that it would be necessary to treat the roads within the relevant
area with salt.
[8] It is a
matter of admission by the Council that they were in possession of the 24 hour
weather forecast for the relevant area issued at midday on the 22 December
1995. They aver that the system for the salting of
roads in operation at the material time was in accordance with the Code of
Practice referred to. In consequence of
the information received as regards meteorological conditions, the Council aver
that it had been decided that the roads in the West Lothian area, including the B9080 at the
locus of the accident, were to be treated with salt through the night of 22 to
23 December 1995. The L3 route was
a priority to be salted, second only to the M9 motorway. That route was indeed salted at the times
referred to.
The decision of the
Lord Ordinary
[9] Having heard the evidence in the case in
a lengthy proof, the Lord Ordinary in paragraphs [5] to [13] of his Opinion
gives an account of the Council's winter maintenance policy operated in
1995. In paragraph [13] he also deals
with the meteorological situation on 22 December 1995 concluding that, in the light of the
forecasts received by the Council, it was clear that, among others, the L3
route was likely to be affected by sleet or snow and to be subject to freezing
temperatures. He then proceeded to
consider the evidence which he had heard relating to the records kept by the Council
of winter road maintenance for the night of 22 to 23 December 1995, which
appears in paragraphs [14] to [16] of his Opinion. He narrates the decisions taken by the Council
as regards gritting at that time and narrates the relevant entries in the
gritting logs, which he was satisfied provided, in general, an accurate summary
of the gritting runs carried out. These
demonstrated three runs on the L3 route, the first between 1723 and 1830 hours
on 22 December, the second between 2315 hours on 22 December and 0130 on 23 December,
and the third between 0540 and 0700 hours on 23
December 1995. In paragraph [16] of his Opinion the Lord Ordinary
refers to other records which were the subject of evidence, but he did not
regard them as undermining the essential reliability of the gritting logs, as
the primary source of contemporaneous evidence.
[10] In paragraphs
[17] to [22] of his Opinion, the Lord Ordinary seeks to define the issues which
emerged at the proof. There was no
dispute that, having regard to the information in the possession of the Council
at the material time the Council knew that it would be necessary to treat the
L3 route with salt. Their position was
that they had done so. The reclaimer
made no criticism of the decisions made as to the routes to be gritted, the
instructions given as a result of such decisions, or the times when the
gritting was shown to have been carried out.
Indeed, the Lord Ordinary observes that she relied upon those decisions
as showing what ought to have been done.
Her case was that something had gone wrong in the execution of those
instructions; the road had not been treated properly in accordance with the
policy and instructions. The Lord
Ordinary observes that, underlying the reclaimer's case was the assumption
that, had gritting been carried out properly and in accordance with the policy
adopted by the Council and the gritting instructions given pursuant thereto,
black ice would not have been present on the road at the time of the
accident. The fact that there was black
ice there meant that the roads had not adequately been gritted. It is to be observed that that contention is
reflected in the averments at the end of Condescendence 2.
[11] The Lord Ordinary
informs us that the reclaimer's primary case on record sought to specify what
had gone wrong. That case - and it was
for a considerable period seen as her only case on record - was that the
drivers of the gritting lorries had deviated from the L3 route at the Bridgend
junction and, by so doing, had left untreated that part of the B9080 road where
the accident occurred. He narrates that,
in the course of the proof, objection was taken by the respondents to certain
lines of evidence sought to be adduced by the reclaimer and it became clear
that the case which the reclaimer wished to advance was not so limited. The reclaimer relied on the averments to
which we have just referred. The reclaimer's
contention came to be that the existence of black ice at the location at the
time of the accident showed that the system operated by the Council had not
properly been followed by its employees.
That failure amounted to a failure by the Council's employees, for which
the Council was liable, to take reasonable skill and care. It was explained specifically in that
connection that the alternative case was an "inferential" one; it did not
involve any criticism of the Council's policy.
Nor did it involve any criticism of decision making at a management
level; of instructions given by management to the Council's employees, or of management's
supervision of the Council's employees.
On the contrary, it was explained to the Lord Ordinary that the
inference of fault arose from the fact that the Council's policy was a
reasonable policy for the Council to adopt to deal with foreseeable winter
weather conditions; and, further, that it was a policy which, if implemented by
the Council's employees, would have been effective to prevent the formation of
ice on the relevant roads.
[12] The Lord
Ordinary's conclusion in relation to this issue which had arisen in the course
of the proof was that it seemed to him that, while the Record did not entitle
the reclaimer to lead evidence of specific failings, for which there was no
fair notice, it did allow this inferential case to be so advanced. He so ruled.
[13] In paragraphs
[20] to [22] the Lord Ordinary explains how matters developed at the proof
thereafter. He states that the
inferential case proceeded upon the assumption that, contrary to her primary
case, the reclaimer could not show what had gone wrong. The argument for the reclaimer was developed
along the lines that, in the weather conditions then prevailing, ice should not
have formed. It could not have formed
had there been adequate salt spread on the road. The mere fact, therefore, that the road was
icy meant that there had been a failure of some kind. This, it had been submitted, was sufficient
to put the onus on the Council to show how this failure could have occurred
without their negligence. Since no
explanation was either offered or proved by the Council, the reclaimer was
entitled to succeed.
[14] The Lord
Ordinary also explains that he had to rule upon the respondents' case on record. They had averred that the Council's gritting
policy had been followed. The site of
the accident had been salted, but after it had been salted between 5.40 am and 7.00 am on 23 December
1995, ice
formed in isolated patches on the road.
The respondents had claimed that they had taken all reasonable
precautions in the circumstances in treating the roads in this way. However, at one point in the
cross-examination of one of the reclaimer's witnesses, senior counsel for the respondents
had asked questions about the mechanism by which salt on the road could be
washed off by water landing on the road surface in the form of rain, sleet or
snow. Objection had been taken to this
questioning on the ground that there was no record for it. The Lord Ordinary understood that the
objection had been taken mainly out of concern that senior counsel had been
going to develop a case, based on a satellite meteorological photographic
image, of some abnormal weather event which was not reflected in the agreed
rainfall data, which had not been put to the reclaimer's previous witnesses,
and which might require expert meteorological evidence. The Lord Ordinary concluded and ruled that
the respondents' case on record in answer to the reclaimer's inferential case
was sufficient to instruct a case that ice might form even after salt had been
applied, because inter alia the
beneficial effect of the salt spread on the road could be dissipated by the
ordinary action of traffic, or rainfall, or a combination of the two. However, he concluded that the respondents'
record gave no fair notice of a case based on a freak weather event, or
abnormal meteorological occurrence; accordingly he ruled that the respondents
were not entitled to develop a case along those lines, although it had to be
recognised that the line between the normal and abnormal in this context might
be hard to draw with precision. It was
then upon this basis that the proof proceeded.
[15] It will be
evident from what we have said so far that the Lord Ordinary's conclusions as
regards the evidence of gritting at the material time are important. The evidence regarding these matters came
from two witnesses, Andrew Green and Thomas Allen Brown. The former was the driver of the gritting
lorry which treated the L3 route on the run beginning at 1723 hours on 22
December 1995. He explained that sometimes, in addition to
gritting the L3 route, he would also grit the road to Bridgend, but only by
coming back to do it after he had finished the L3 route. He was adamant that no part of the L3 route
would be missed for that reason. Thomas
Allen Brown treated the L3 route on the two occasions after Mr Green's round
and before the accident. On the first
occasion he treated the L2 and L3 routes in one run. He had been on the nightshift on the night of
22 December and the morning of 23 December 1995.
He explained that, when approaching the Bridgend junction, the road
widened, as a result of which it was necessary for him to operate the controls
of the gritting lorry so as to ensure a wider spread with more salt. He went on to explain that, during the night
in question, he had seen one of his colleagues, a Tony Foss, at a bus stop at
around midnight or shortly thereafter.
He had picked him up and continued on the L3 route past the point at
which he had started gritting that route.
He then continued on the B8090 until the Bridgend junction, when he
turned left to drop off Mr Foss in Bridgend.
It was this driver who conducted the gritting of the L3 route beginning
at 5.40 am and ending at 7.00 am on 23 December. On this occasion he had gritted the L3 route
in an anti-clockwise direction. It is
important to note that this witness testified that it had started to rain about
half an hour before he had started gritting the L3 route for the last time, in
other words shortly after 5.00 am. The
witness said the rain started as a fine drizzle, changing into normal
rain. He said that the rain continued
during the gritting of the route. He
said that it was not until the route started turning back east, when on the
outskirts of Queensferry, that he had realised how heavily it was raining. By the time he reached a junction near Duntarvie,
the rain was so heavy that he could hardly see a thing. He described it as "torrential", "really,
really heavy", during the course of the gritting. He could see the rain being swept along the
road. In cross-examination he insisted
that the rain was "bouncing"; it could have formed puddles if it had not been
so hard. Despite this, he had carried on
to complete the route. He explained that
there was no issue concerning carrying on; once the task had been started, it
was finished. In paragraph [25] of his
Opinion the Lord Ordinary sets out his assessment of the evidence from the
drivers of the gritting lorries. He
said:
"I am satisfied that both were
truthful witnesses endeavouring to assist the Court. However, there were moments in their evidence
when it was clear that they were having difficulty in recalling the details of
their actions leading up to the accident and even in recalling what system was
operating in 1995. I did not find this
surprising since it all happened so long ago.
But it did make me cautious in accepting their evidence where it
differed from the information contained in the contemporaneous documents."
[16] It will be
evident from what has already been said that the explanation for the existence
of ice on the road at the location of the accident is a crucial matter. As was appreciated by the Lord Ordinary, the
condition of the road surface at the Bridgend junction at or around the time of
the accident, in the event, was capable of casting light on that crucial
question. Accordingly the Lord Ordinary
considered its condition in some detail between paragraphs [36] and [39] of his
Opinion. It is appropriate to summarise
his conclusions in that regard. He
records that he heard evidence from a number of witnesses who were at the locus
on the morning of 23 December, either at the time of the accident, or
immediately before or after it. These
included a Mr and Mrs Brown who farmed at Bridgend Farm on the north side of
the road, opposite the junction; Mr Farren, the driver of the bus involved;
Mr Blanch and Ms Dunleavie, who had arrived on the scene in a motor car
just after the accident; Mr Gray, who attended the scene with the fire service;
Mr Christie who lived nearby and was out for his morning walk; Mrs Connor, who
lived in Bridgend and was driving to a nearby Post Office; and two police
officers, Police Sergeant Colin Barnes and Police Constable Alistair Bain. The Lord Ordinary's assessment of these
witnesses was that they all gave their evidence carefully and honestly and he
was satisfied that each was doing his or her best to assist the Court. However,
he took into account the fact that the accident had happened some ten years
before the proof and inevitably recollections might have been clouded by the
passage of time. As regards the
observations of the witnesses as to the approximate positions of the vehicles
involved in the accident, there was virtual agreement between them all. So also there was when they spoke of
slipping, or seeing others slipping on the road, or of skidding, or seeing
others skidding, when braking. The Lord
Ordinary considered their evidence on those matters as likely to be
reliable. He considered that the
evidence of one witness tended to complement that of the others and to build up
a fairly clear picture. The Lord
Ordinary explains that he was not able to accept uncritically observations to
the effect that "the whole road" was "a sheet of ice", as distinct from there
being large patches of ice covering a large part of the road surface. In paragraph [37] of his Opinion, the Lord
Ordinary deals with the evidence of Police Constable Bain, which he found
particularly valuable. That witness had
testified that there was physical evidence that he observed that the road had
been treated. He had noticed it
particularly on the eastbound carriageway.
He could see the grit and feel it and hear it crunching underfoot. He agreed that the road surface was very
slippery due to ice, but according to his observation, the whole road was not a
"sheet of ice"; there were extensive patches of ice on the road but other parts
were not affected. He was sure that his
observations of grit on the road surface were made within half an hour of his
arrival and before any gritter arrived following the accident. It followed that the grit that he observed on
the road, according to his evidence, must have been grit spread on the road
before the accident. The Lord Ordinary
accepted his evidence, both as to the extent of the ice cover on the road and
his observations of grit. Having done
that, the Lord Ordinary, of course, recognised that it did not follow from this
particular evidence that this was grit spread on the gritting run commencing at
0540 hours on the morning of 23 December.
However, the evidence did signify that there was grit on the road
effective, to some extent at least, to prevent or restrict the formation of
ice. In paragraph [38] of his Opinion
the Lord Ordinary summarises his conclusion as regards the state of the road
surface at the material time. He
concludes that:
".....it is clear that the road surface
of the B9080 was very slippery over an area extending at least 50 yards to the
east of the Bridgend junction and possibly 150 yards or more to the west. The precise extent of the slippery road
surface may not matter. What does matter
is that the slippery area extended far beyond the junction and was not confined
to the narrow diamond shape that might have been left untreated had the gritter
diverted from the B9080 in the course of doing the L3 route to treat the
Bridgend road as alleged by the pursuer as part of her primary case"
[17] Quite
extensive meteorological evidence was led at the proof. The issue of its significance was the subject
of extensive submission, both before the Lord Ordinary and in the course of
this reclaiming motion. It is therefore
appropriate to consider it in some detail.
[18] Iain Farquhar
was called as an expert witness by the reclaimer. His evidence was directed towards the weather
conditions prevailing at locations in the general area of the locus of the
accident on 22 and 23 December 1995; and the inferences that could be
drawn from that information as to the conditions at the locus itself. Mr Farquhar had worked at the
Meteorological Office from 1964 until 2001.
Towards the end of that time he had been the Enquiries Officer in the
Scottish Climate Office, originally at Edinburgh and latterly at Glasgow
Weather Centre, dealing with a large number of enquiries concerning past
weather. He was familiar with the B9080
road, having lived in the area since 1978.
He had kept his own rainfall record at his home in Linlithgow since that
time. He had prepared a report in
connection with the present action in October 1997, which was spoken to by him
in evidence.
[19] The Lord
Ordinary expresses the opinion that Mr Farquhar was an impressive witness; it
was clear that both his report and his oral evidence were based on thorough
research. The Lord Ordinary observes,
however, that, in a number of respects, Mr Farquhar's evidence appeared to
be at odds with the evidence given by Council employees, particularly that of
Thomas Allen Brown. For that reason he
thought it necessary to consider those aspects of Mr Farquhar's evidence with
particular care.
[20] In his report,
Mr Farquhar described the general weather situation in the relevant area as
follows:
"During the 20th and the
first half of the 21st December 1995 a cold airstream from the Arctic and a ridge of high pressure over Scotland combined to give dry weather in West Lothian.
There were frosts night and morning but the ground was snow free in the
Linlithgow area.
Later on the 21st, a
frontal zone (a band of thick cloud and precipitation), associated with an
Atlantic depression, pushed northwards from England into the cold air over
Scotland, consequently by 1800 GMT (6.00 pm) that evening, eastern parts of
Linlithgow had a two inch deep snow cover.
Overnight 21/22, the front from the
south crossed the Lothians introducing a thaw and periods of rain. The snow on the ground had turned to slush at
Linlithgow by 0730 GMT on the morning of the 22nd. The rain continued throughout the 22nd
and, almost certainly, cleared all the snow.
In the evening (22nd), rising atmospheric pressure to the
north of the front pushed the cold air back southwards into the Central Belt of
Scotland, turning the rain back to sleet by the early hours of the 23rd. The front and its thick cloud and
precipitation continued to move away southwards and by 0800 GMT, the weather
had become dry at Turnhouse.
The wintry precipitation falling on
the ground early on the 23rd, combined with breaks in the cloud
sheet and an easing wind, almost certainly, allowed ground temperatures to dip
to just below freezing-point over the hour or so before the time of the
accident."
[21] Mr Farquhar's
report was elaborated in oral evidence.
There had been a very disturbed spell of weather from 20 to 23
December 1995. On the morning of
23 December a severe
Arctic spell set in which lasted until 1 January 1996.
Although that spell had not arrived until after the accident, the
conditions at around 0800 to 0900 hours on 23rd
December 1995
would have led to a "hazardous situation" with icy conditions on the
ground. Mr Farquhar's conclusion as to
the conditions at about 0900 hours in the general area of Linlithgow and
Bridgend was that the countryside was under a sprinkling of snow and hail and
air temperature was around +2 or 3 degrees centigrade. The Lord Ordinary records that Mr Farquhar
expressed the following opinion:
"Adequately salted roads will have
been soaking wet. Many stretches of
insufficiently salted road will have been affected by a thin coating of a
combination of slush, snow and hail with clear (or 'black') ice in places"
Mr Farquhar said that the conditions which he thought likely
to have obtained at the Bridgend junction were consistent with black ice on an
insufficiently salted road and the existence of extensive black ice on an
unsalted road. He explained the use of
the words "adequately" and "insufficiently" as meaning adequately or
sufficiently "in time and quantity". A
road that had insufficient salt on it at 0900 hours might have had adequate
quantities some hours earlier.
[22] The Lord
Ordinary opined that the principal question arising from Mr Farquhar's
evidence was whether, in the conditions which prevailed on the morning of 23
December 1995, both in terms of temperature and of rainfall, the effect of
which might, depending upon its intensity, be to wash away salt spread by the
gritters, the existence of black ice at the road junction in question was
inconsistent with salt having been spread by the gritters in the manner
indicated in the Council records.
[23] The Lord
Ordinary records that the data spoken to by Mr Farquhar came from three
sources: first, the manned Meteorological Office at Edinburgh Airport at
Turnhouse, which was situated about 12 kilometres to the east of the Bridgend
junction; second, the manned Climatological Station at Falkirk, about 15
kilometres to the west; and, third, the manned Rainfall Station at Linlithgow,
about 4 kilometres to the west. This
latter station was maintained personally by Mr Farquhar at his home. He took rainfall readings once a day at 0900
hours. The Falkirk Climatological
Station was situated at the Council sewage works there; employees at the sewage
works took readings of rainfall and temperature and also recorded observations
as to the state of the ground. Again,
they did this once a day at 09.00 hours.
By contrast, the manned Meteorological Office at Edinburgh Airport, in addition to providing daily data
recorded at 0900 hours, carried out a much wider range of observations on a
routine basis every half hour. All of
these three stations were situated lower than the Bridgend junction, Turnhouse
being about 35 metres above sea level, Falkirk about 3 metres and Linlithgow
just under 60 metres, compared with a height of 80 metres above sea level at
the junction.
[24] The rainfall
recorded for the twenty four hours up to 0900 hours on 23
December 1995
was 12.3 millimetres at Falkirk, 17.7 millimetres at Linlithgow and 15.4 millimetres at
Turnhouse. As regards these records the
Lord Ordinary comments that, in so far as any such readings might be used to
say what the rainfall was likely to have been at the Bridgend junction a few
kilometres away from each of the weather stations, it was cautionary to note the
significant differences between the three places. He goes on to explain that the hourly
readings taken at Turnhouse bore to show continuous or, very occasionally,
intermittent rain throughout that 24 hour period, mainly recorded as moderate
or slight. There were, however,
recordings of "moderate/heavy sleet" and "recent sleet" between 0100 and 0300
hours on 23 December, and of "recent sleet" becoming "moderate/heavy
sleet" between 0400 and 0600 hours. The
hour to 0700 hours is recorded as "slight rain and drizzle." The hourly recorded rainfall at Turnhouse for
each hour on the morning of 23 December 1995 until the time of the accident at
about 0900 hours, starting with the hour between midnight and 0100 hours, was :
0.6 millimetres, 0.6 millimetres, 0.8 millimetres, 0.2 millimetres,
0.8 millimetres, 0.4 millimetres, 0.4 millimetres, 0.2 millimetres and
nil. As regards these measurements of
rainfall, it is relevant to note that Mr Farquhar in evidence explained that
there were two main methods of taking readings of rainfall. Daily readings were taken by the use of a
standard daily rain gauge consisting in a copper bucket with a five inch
diameter turned brass rim. The amount of
water was recorded and the bucket was then emptied manually. Hourly readings, on the other hand, were
taken by a dipping bucket rain gauge.
This type of rain gauge worked in relation to units of 0.2
millimetres. When the gauge was full
with 0.2 millimetres of water in it, it tipped automatically, emptying itself,
and then returning to the upright position.
The hourly readings were recorded by reference to the number of times
that the gauge had tipped within an hour.
Thus, for example, if the gauge were empty at the beginning of hour one,
filled up with nearly 0.2 millimetres of rainfall during the hour, but did not
finally tip until one minute into hour two, the reading for hour one would be
nil. If the rain continued at about the
same intensity in hour two but the gauge tipped again momentarily before the
end of hour two, the reading for hour two would be 0.4 millimetres. Accordingly the margin of error of each
reading was just short of plus or minus 0.2 millimetres. For meteorological and record purposes, that
was not considered to matter. However it
might be a matter of significance if the search was for a precise reading by
reference to which to test other observations.
The readings given in the recorded data at Turnhouse for the hours up to
0600 and 0700 hours on 23 December were both 0.4 millimetres. Accordingly one or both of these readings
could represent a true hourly rainfall of up to 0.6 millimetres.
[25] The Lord
Ordinary records that the Turnhouse meteorological records contain observations
as to the state of the weather for those two hours, the observations were
respectively "moderate/heavy sleet" and "slight rain and drizzle", and yet
those were both descriptions associated with a recorded rainfall of 0.4
millimetres. He concludes that it was
possible that the records for the two hours between 0500 and 0700 hours
reflected a period when the rain or sleet intensified for a short period around
0600 hours. He considered the
description "moderate/heavy sleet" for the hour to 0600 hours was consistent
with this possibility.
[26] Minimum and
maximum daily air temperatures were recorded at the Falkirk and Turnhouse weather stations, but
not at the Linlithgow station. Hourly
temperatures were also recorded at Turnhouse.
In Mr Farquhar's opinion, these readings were only indicative of the
likely temperatures at the Bridgend junction.
He would have expected both air temperatures and ground temperatures to
be lower at the Bridgend junction than at Turnhouse. There were a number of reasons for that. Turnhouse was nearer the sea. It was nearer sea level. There was a culvert under the road at the
junction. The junction was in a dip and
shaded. Mr Farquhar considered that
ground temperature at the junction might be 0.4 degrees centigrade lower than
at Turnhouse. Using the ground
temperature readings at Turnhouse as a reference point, the minimum ground
temperature at the junction in the twenty four hours leading up to 0900 hours
on 23 December was likely to be in the region of -0.9 degrees centigrade. This compared with a minimum air temperature
at Turnhouse of about +1.4 degrees centigrade for that same period. The ground temperature at the junction at any
time was, therefore, likely to be about 2.3 degrees centigrade below air
temperature at Turnhouse. Applying that
differential to the recorded hourly air temperatures at Turnhouse, it was
considered quite probable that freezing ground conditions existed at the
junction by 0500 hours on 23 December lasting through until 1000 hours. The ground temperature at the junction might
have reached as low as -0.4 degrees centigrade or even -0.9 degrees centigrade
over the course of the night and early morning.
The coldest time tended to be around dawn. Rain and sleet could lower the
temperature. Dawn was at 0844 hours on
23 December. Mr Farquhar considered that
it was likely that there were freezing conditions in being then. The Lord Ordinary says that he was inclined
to accept the figures given by Mr Farquhar as broadly indicative of the
temperatures likely to be experienced at Bridgend junction in the hours leading
up to the accident.
[27] Evidence was led
on behalf of the respondents from Mr Neil Maloney, the station manager at
Dundee Satellite Receiving Station (DSRS) at Dundee University.
This witness spoke to a satellite image lodged in process by the
respondents, which focused on the area around Linlithgow and Bridgend over one
or two minutes at around 08.15 hours on 23 December 1995.
He explained that this was a section from one complete recording
covering an area from Europe to the North Pole. On
one view, this image showed the possibility of there having been heavy precipitation
over the locus at the relevant time. However,
the Lord Ordinary did not consider that a single image from such a range
offered a useful insight into the weather conditions with which he was
concerned in this case.
[28] Evidence was
led on behalf of the reclaimer from a Mr Patrick Wingfield, a chartered
engineer, who had been involved in highways meteorological issues, including thermal
mapping, since the 1980s. In the first
instance, his investigations had centred on whether and, if so, to what extent,
water from field drains draining down to the road in question might have washed
away salt spread by the gritting lorries.
He had concluded that the field drains had had no effect on the salt on
the road in question. His investigations
had therefore turned to discovering how black ice could have formed on the road
surface consistently with it having been gritted in the manner alleged by the Council. In his evidence, if salt were applied at a
spread rate of ten grams per square metre before the road temperature dropped
to freezing, it would be totally effective, down to temperatures of -6 degrees
centigrade, to prevent the formation of black ice. It would remain effective, without any time
limit, so long as it were not washed away.
If the salt were spread after the ice had formed, it would not be so
effective, but it would still disperse the ice relatively quickly. This witness said that if the lowest
temperature at the locus was -0.9 degrees centigrade, there should have been no
black ice at all. Had the road been
gritted as alleged by the council, it should have been free from ice down to a
temperature of -5 degrees centigrade.
Mr Wingfield rejected the notion that the salt could have been
washed away in sufficient quantities to account for the existence of ice, if
gritting had been carried out as alleged.
That opinion was based upon the recorded rainfall at Turnhouse of
2.4 millimetres over the four hour period between 2200 hours on 22
December and 0200 on 23 December 1995.
This witness said that according to the same records only about one
millimetre of rain fell in the four hours between 0500 hours and 0900 hours
on 23 December. It was not likely that
that amount of rain would have washed the salt away. The only explanation for the existence of
black ice at 0900 hours on 23 December was that, for whatever reason, salt
had not been present at all, or in a sufficient quantity. At this point in the evidence, Mr Wingfield
was invited to speculate as to how that might have come about. However, objection was taken to that line of
questioning upon the ground that it went beyond the inferential case open to
the reclaimer on record. That objection
was upheld. Mr Wingfield, in cross-examination,
was asked about the evidence of vehicles skidding when still a considerable
distance from the Bridgend junction. He
agreed that, if that evidence were accepted, it would indicate a general
problem rather than one restricted to ice at the junction itself. He agreed that, if rain had been "torrential"
for a significant period, that would have been relevant in regard to washing
salt off the road, but the rainfall figures did not indicate torrential
rain. His view was that conditions at
the Bridgend junction would not have been exactly the same as those at
Turnhouse, but he would not have expected them to be wholly different.
[29] Mr Adrian
Runacres was called as an expert witness by the Council. He had had considerable experience in highway
maintenance and provided investigation and risk management services to the
highway industry, including advice on highway maintenance and was head of the
Advisory Services Department at the Transport Research Laboratory and remained
principal consultant to that body. He
had undertaken a site visit in July 2002 and was familiar with the L3
route. He had prepared a report in
January 2004. He testified that the
junction was in an open valley. The
altitude, the water course under the road, and the possibility that the
junction was in shadow, all tended in his opinion to point to this area of the
road being colder than other areas at the time of the accident. The clearing skies at dawn could also have
been a significant factor in reducing road surface temperature. He was unable to say what the likely
difference in temperature between the locus and Turnhouse would have been on
the morning in question. While Turnhouse
was not very far away and the data from the station there would assist greatly
in any investigation, it was necessary to be careful in using data from a
single point. As evidence of that he
drew attention to the differences in rainfall recorded at the three
stations. The variations were
significant. This witness had known of a
temperature difference of 3 or 4 degrees centigrade between stretches of road
quite close together.
[30] In his report,
Mr Runacres expressed the opinion that:
".....the precipitation falling
overnight and during the early morning hours of Saturday 23
December 1995
appears to have been heavy enough to have diluted and washed away even very
significant amounts from the road surface.
This precipitation would have rendered de-icing salt significantly less
effective in preventing ice formation than it otherwise would have been.
Due to the fact that the
surface temperature of even the coldest sections of road in that region is not
likely to have been very much below 0 degrees centigrade around the time of the
accident, I consider that, had the precipitation not been so heavy or prolonged,
then even moderate amounts of de-icing salt could have remained effective
during the period of concern."
At a later stage in his report he
observed:
"It should be noted that there is
reported to have been heavy rain and sleet in the material area following the
previous precautionary salting operation undertaken [on the early evening of 22
December)]. As such, I consider it
highly likely that, by the time of the second operation, the intensity of the
precipitation may well have rendered the previously applied salt ineffective in
preventing the formation of ice on road surfaces."
[31] The Lord Ordinary
considered that the same reasoning would apply, although Mr Runacres had not
said so, to the third operation, if it were found that the precipitation occurred
with its greatest intensity just after that operation. Mr Runacres explained that, when salt was
spread as grit, the particles could be washed away mechanically from the road
by water and also by the action of vehicles. As regards the likely intensity of
the rain at the locus, Mr Runacres considered it unsafe to rely on data from
one site to infer conditions a few kilometres away. Precipitation clouds were typically 2 to 3
kilometres across. It could not
necessarily be said that conditions were the same even 3 kilometres away.
[32] Mr Runacres,
in cross-examination, accepted that the temperature at the locus would not have
gone so low as to render ineffective salt spread at a rate of 20 grams per
square metre. In other words, he did not
think that temperature - other than the fact that it was about 0 degrees
centigrade - was a significant factor in the salt not working to prevent the
formation of black ice at the junction.
For ice to form at that temperature, there could not have been adequate
quantities of salt on the road at the time it formed. If salt had been spread at the rate spoken to
by the Council, ice could not have formed unless the salt had been
substantially removed. To remove the
salt required a flow of water. He did
not consider that traffic flow alone could account for the dispersal of salt in
sufficient quantities to allow the formation of ice at the locus at the
time. There would have required to have
been enough precipitation to create a flow of water in the road. Mr Runacres accepted that, if the rainfall
had been as little as 0.2 millimetres per/hour for an hour or less, that would
have been insufficient to eliminate the de-icing effect of any salt spread on
the road. But, on the other hand, if
there had been 1.2 millimetres of rainfall over the previous three hours, that
rainfall combined with the action of traffic would have been sufficient to wash
the salt off the road, or at least wash of sufficient quantities of salt to
allow the formation of ice.
[33] Against this
background of evidence, it was submitted to the Lord Ordinary on behalf of the reclaimer
that he should not place any reliance on the evidence given by Mr Thomas Allen
Brown of torrential rain near Duntarvie.
It was contended that not only was that evidence inconsistent with the
hourly recorded rainfall at Turnhouse, but it was also of doubtful weight
because Mr Brown had been first asked about this level of detail in 2002, over
six years after the accident. It was
said that he had then given a statement, revised it and subsequently
contradicted what he had said. He was
unlikely to have had such a precise recollection of the weather. His evidence had been that the night was dry
until about 0500 hours on 23 December, but that was inconsistent with the
records relating to Turnhouse. Further,
he had been shown to have been wrong in other aspects of his evidence given in
his earlier statement, for example about where he started the L3 route on the
night and morning in question.
[34] The Lord
Ordinary has concluded, after carefully considering this submission, that he
was not prepared to reject Mr Brown's evidence.
He was satisfied that he was an honest witness doing his best to give an
accurate recollection of events. His
view was that there was a sound explanation for his failure, in his earlier
statement, to recall where he had started his run, and he did not consider that
that change reflected adversely upon the reliability of other parts of his evidence. The Lord Ordinary states that the difference
in the data recorded by the weather stations, all situated within a few
kilometres of each other, suggested to him that such data, on its own, was
insufficiently certain to form the basis for rejecting Mr Brown's evidence
about the intensity of the rainfall which he had experienced on a particular
part of his route. Furthermore, he
considered that the method of arriving at the figures for the hourly rainfall
at Turnhouse, whilst perfectly acceptable for the purpose for which it was
designed, did not itself give rise to data which was sufficiently sure to put
in the scales against the credibility or reliability of this witness. That method was, of course, described in the
evidence of Mr Farquhar. Of the
Turnhouse data the Lord Ordinary states that the recorded levels of rainfall
were not consistent with some twenty minutes of torrential rain at
Turnhouse. But they did not appear to
him to be inconsistent with a short period of moderate to heavy rain or sleet
there. The Lord Ordinary's view was that
those figures certainly did not require him to reject evidence of a more
prolonged and more intense downpour on a stretch of road between eight and
fourteen kilometres away from Turnhouse, that is to say the area around
Duntarvie, to which Mr Brown's evidence related.
[35] As regards
other cogent matters, the Lord Ordinary found that, at the time of the
accident, the road at the Bridgend junction was adversely affected by black
ice, which extended for at least 50 yards to the east of the junction and for 150
yards to the west, but the whole carriageway within such bounds was not found
to be covered in black ice. On the
contrary, he concluded that the black ice was patchy, covering the greater part
of the road within such bounds, but broken by areas where the road was simply
wet. He considered that, given the
weather conditions over the night of 22 December and into the morning 23
December 1995, the black ice was likely to have formed sometime between 0600
and 0900 hours on the latter date. He
also considered it established that, had there been sufficient salt in solution
at the locus between 0600 hours and the time of the accident, black ice would
not have formed, or remained on the carriageway. As regards the route followed by the gritter
drivers, the Lord Ordinary was not prepared to hold that there was a deviation
from the prescribed gritting route. In this regard, he accepted the evidence of
both gritter drivers that they did not drive to Bridgend until after they had
completed route L3. He also accepted the
evidence of Police Constable Bain that he observed grit on the road at the
junction when he inspected the site within half an hour or so of his arrival
just after the accident. The Lord
Ordinary decided that his conclusion in relation to the extent of the black ice
at the locus of the accident for a considerable distance on both sides of the
junction made it impossible for him to link the presence of black ice with any
alleged deviation by the gritters. Had
they deviated from the route, his view was that the area left untreated would
have been significantly smaller than that which he found to have been affected
by black ice. The consequence of that
finding was that he rejected the pursuer's primary case on the facts.
[36] As regards the
reclaimer's inferential case, it was submitted to the Lord Ordinary that that
case could be established on the basis of circumstantial evidence if the
existence of the black ice could be attributable only to a failure to grit, or
grit adequately, the road, or at least the relevant part of it. It was
submitted that the reclaimer had established a prima facie case of negligence, which it was for the Council to
rebut. The submission on behalf of the
reclaimer had been that no explanation inconsistent with the Council's fault
had been pled or proved.
[37] The position
taken up on behalf of the Council before the Lord Ordinary was that, looking at
the evidence concerning weather conditions, information concerning conditions
at the locus was limited. This was not
truly a case res ipsa loquitur since the accident had not happened in
circumstances which were entirely within the control of the Council. Accordingly, it was necessary for the
reclaimer to demonstrate on a balance of probabilities that fault lay with the
Council. The only case of that sort
advanced by the reclaimer was the deviation from route case. On the facts it was submitted to the Lord
Ordinary that that case must fail.
[38] The Lord
Ordinary's reasons for his decision to grant decree of absolvitor are set out
in paragraphs [64] to [80] of his Opinion.
In paragraphs [64] to [67], the Lord Ordinary discusses the nature and
scope of the duties of care owed by the Council to road users. In paragraph [68] he records that the
respondents conceded that, if it were established on the evidence that the
driver of the gritting lorry at the material time had deviated from the route
that he was instructed to follow, and had, in so doing, left a stretch of the
road unsalted so that ice formed, they would be liable. He records that they made no similar
concession if failure to grit the relevant stretch of road was due to some
other problem within the operation.
Turning to what has been called the reclaimer's inferential case the
Lord Ordinary opined that, if the reclaimer were able to establish that the
temperatures and the amount of precipitation could not in the ordinary course
of things have resulted in the presence of black ice at the junction, had the Council
exercised proper care, then the onus would shift to the respondents. As regards temperature, the Lord Ordinary
considered that the evidence seemed to be substantially in agreement. It was not possible to say precisely what the
temperature was at the locus between 0600 and 0900 hours on 23
December 1995. That was likely to have been the coldest part
of the night. It was likely that the
ground temperature at the junction was zero or just below, perhaps as low as -1
degree centigrade, during part or all of this period. That was cold enough for ice to form, but it
was not cold enough to account for the formation of ice, if there was a
significant amount of salting solution on the road; and certainly not cold
enough to account for the formation of ice if the road was, at the time of
formation, covered in salt in the concentration of 20 or even 10 grams per
square metre. Hence the Lord Ordinary
concluded that the temperatures over the night in question were not
sufficiently low to render ineffective the presence of any significant quantity
of salt in solution on the roadway.
However, he observed that there was no evidence as to precisely what
amount of salt in solution was necessary to prevent freezing at -1 degree
centigrade. It would therefore be a
mistake to have a picture of a consistent covering of water or salt in solution
across the entire width and length of the relevant part of the road. There could be some patches of the road with
more salt on them than others. The Lord
Ordinary then went on to consider, if there was insufficient salt at the locus
at the material time to stop the formation of ice, or to remove any ice that
might have formed, how that was to be explained. The Lord Ordinary observes that, according to
the evidence of Mr Thomas Allen Brown, which he accepted, that driver would
have passed the Bridgend junction going in an anti-clockwise direction just
before 0600 hours on 23 December.
His gritter had been set so as to spread at 20 grams per square
metre. If all had gone as it should, the
road in the area of the junction would have had that amount of salt spread on
it then. The reclaimer's contention was
that for whatever reason, salt was not spread on that run at all, or at least
not in any significant quantities. That
was sought to be proved by showing that the precipitation falling in the vicinity
between 0600 and 0900 hours was insufficient to have washed away or diluted the
salt at the locus by the time of the accident.
The Lord Ordinary had been invited by the reclaimer to hold that the
quantity and intensity of the precipitation in the vicinity of the Bridgend
junction between the hours mentioned were not such as would have washed away or
diluted the effect of salt in solution at the locus by the time of the
accident. His conclusion however was that he was not prepared to make such a
finding.
[39] The Lord Ordinary
in paragraph [77] observes that the assessment of the evidence about precipitation
differed in a material way from that of the evidence about temperature. In the case of temperature, records had been
kept and it was possible with some certainty to make a judgement on the likely
differential between the temperature at Turnhouse and that at the Bridgend junction. On that the experts were in close
agreement. The Lord Ordinary considered
that it was therefore possible to make a finding about the likely temperature
at the junction at the material time in isolation from any consideration of
other evidence and then to use that finding as a fixed point in the
consideration of what had occurred.
However he was not persuaded that the same exercise could be relied upon
in relation to precipitation. There were
significant divergencies between the readings for precipitation at the three
weather stations. That persuaded the
Lord Ordinary that to make an estimate of how much rain had fallen at the
relevant time at the junction was by no means an exact science. In those circumstances, the Court had to
assess the evidence about precipitation, not only by reference to the data at
certain points and the extrapolation by experts from such data, but it also had
to look at all the other evidence of circumstances which might have a bearing
on its conclusion. Finally, the Lord
Ordinary observes in paragraph [78] of his Opinion that he did not regard the
rainfall readings at Turnhouse as a sufficient basis for refusing to accept the
evidence of Mr Thomas Allen Brown as to the heavy rain which he claimed to have
encountered on the route not long after 0600 hours. For the same reason, he states that he was
unable to find, even on a balance of probabilities, that the rainfall at the
junction was insufficient to wash away or dilute salt at the junction. To arrive at that conclusion would have
required him to reject the evidence of Police Constable Bain that there was
grit on some parts of the road, because, if his evidence was to be believed, it
must mean that salt had been spread but in substantial part dispersed. On the whole matter, the Lord Ordinary held
that the reclaimer had failed to establish a case which threw the onus on the
respondents to explain how the accident had happened without their negligence.
Submissions
[40] The
submissions in this reclaiming motion ran over a period of ten days and
involved extensive and detailed references to the evidence that had been led
before the Lord Ordinary. The primary
contention of the reclaimer was that the Lord Ordinary's conclusions in
relation to crucial issues of fact had been plainly wrong. Accordingly, those issues were now to be
decided by us in the light of the whole available evidence. Submissions were then made to us on that
evidence, in which the reclaimer contended that, on those crucial issues, we
should make findings different from those of the Lord Ordinary. It is quite impracticable for us to attempt to
narrate those submissions in detail within any reasonable limits in this
Opinion. In any event, we find it
unnecessary to do so. Accordingly, what
we intend to do now is to provide a brief summary of what we understand to have
been the core elements in the submission to the effect that the Lord Ordinary's
conclusions were plainly wrong.
The Reclaimer's
Contentions
[41] As it appeared
to us, the reclaimer advanced two principal submissions. The first of these related to the approach of
the Lord Ordinary to the evidence led concerning the condition of the road
surface at or about the locus of the accident.
The Lord Ordinary had preferred the evidence of Police Constable Bain to
that of other witnesses. It was
contended that, in doing so, he had erred.
The second principal contention advanced on behalf of the reclaimer was
that the Lord Ordinary had erred in holding that he was not satisfied that the
precipitation at the locus of the accident had been insufficient to wash off
grit spread there during the course of the third gritting operation, had that
operation been effectively carried out.
[42] We were
referred on behalf of the reclaimer to a number of authorities. In general, these related, first, to the
approach which this Court ought to take to findings or conclusions in fact reached
by the Lord Ordinary. Secondly,
authorities were put before us relating to the principle of res ipsa loquitur. In the first category, our attention was
drawn to Thomas v Thomas 1947 S.C. (H.L) 45, and
particularly to the speech of Lord Thankerton at page 54, where the well-known
passage dealing with the proper approach to be taken by an appeal court to
findings of fact made by a judge of first instance is to be found. Our attention was also drawn to Dingley v Chief Constable, Strathclyde Police 2000 S.C. (H.L.) 77, a case in
which the absence of any detailed reasoning in relation to findings in fact on
part of the Lord Ordinary had resulted in the First Division requiring to reach
a decision based entirely on the printed evidence. At page 81, the point was made that the Lord
Ordinary had failed to give reasons to justify his decision to accept some
parts of the evidence and to reject other parts. Reliance was also placed upon Jordan v Court
Line Limited 1947 S.C. 29 where
once again, in that case, the importance of a judge of first instance giving
reasons for his acceptance or rejection of evidence was emphasised. In Morrison
v J.Kelly & Sons Limited 1970 S.C. 65, the importance of a Lord Ordinary
giving reasons for his decisions on the evidence of witnesses was reiterated. We were also referred to Curry v Clamp's Executor 2002
S.L.T. 196, a case concerned with, among other things, the need for the
cross-examination of witnesses, in the interests of fairness.
[43] Among the
authorities relating to the principle res
ipsa loquitur and issues of onus of
proof put before us were Rhesa Shipping
Company S.A. v Edmunds [1985]
W.L.R. 948; Caledonia North Sea Limited v
London Bridge Engineering Limited
2000 S.L.T. 1123, a case which emphasised the need for a Lord Ordinary,
confronted with the need to make a decision of fact, to review all sources of
relevant evidence and draw from them such inferences and conclusions as he
considered appropriate; the well-known case of O'Hara v The Central S.M.T.
Company Limited 1941 SC 363, particularly at pages 376 to 379; and Moore v R.Fox and Sons [1956] 1Q.B.
596, a case concerned with the application of the principle res ipsa loquitur.
[44] Coming to the
principal criticisms of the approach of the Lord Ordinary made on behalf of the
reclaimer, it was said that the Lord Ordinary had preferred the evidence of
Police Constable Bain regarding the condition of the road surface at the locus
of the accident, as opposed to the evidence of other witnesses who had given
evidence of the condition of the locus, without having given sufficient reasons
for his preference in the form of explanations concerning the evidence of the
relevant witnesses.
[45] The second
main area in which it was contended that the Lord Ordinary had erred was in
holding that the records of precipitation at the Turnhouse Weather Station did
not prevent him from accepting as reliable the evidence of Thomas Allen Brown,
one of the two gritter lorry drivers who gave evidence, concerning the weather
conditions he claimed to have experienced in the vicinity of Duntarvie. The importance of this issue had been that
the Lord Ordinary had relied upon the evidence of Thomas Allen Brown to
conclude that the reclaimer had failed to prove that there had been
insufficient precipitation at Bridgend at the material time to bring about the
diminution of effectiveness of the grit revealed by the presence of black ice
there at the time of the accident. The
contention was that, in the light of the evidence of precipitation at the
weather station at Turnhouse, the Lord Ordinary should have regarded the
evidence of Thomas Allen Brown as unreliable and rejected it. Our narrative of these contentions has perforce
been much attenuated, but we trust that we have in fact identified the core
contentions of the reclaimer.
Contentions of the
Respondents
[46] In paragraph [58] of his Opinion, the
Lord Ordinary had rejected the only case specifically pled on behalf of the
reclaimer, the so-called "deviation case".
That part of the Lord ordinary's decision had not been challenged. Accordingly, what was under consideration in
the reclaiming motion was the Lord Ordinary's handling of what had been called
the reclaimer's inferential case, based upon the averments in condescendence 2
between page 7E and 8A of the reclaiming print.
That case was simply to the effect that, had the L3 route been
adequately salted on both lanes of the carriageway by the Council in the manner
that they had averred and, in particular, salted between 5.40 am and 7.00 am on 23 December
1995, black
ice would not have formed at the locus by the time of the accident. The reclaimer had contended that, since black
ice existed at the locus at the material time, it could be inferred that
insufficient salt had been spread there.
If the cause of that insufficiency was dilution through precipitation,
the reclaimer's case failed; if not, then the onus passed to the respondents to
show that the insufficiency of salt was not due to the Council's
negligence. The Lord Ordinary had held
that he could not find that there had been insufficient precipitation at the locus
and accordingly the reclaimer's case had failed. That conclusion was a result of the global
assessment of the evidence. The
respondents' overall submission was that the Lord Ordinary was entitled to
reach the conclusions that he did. It
could not be said that he had been plainly wrong to do so. In connection with this matter the evidence
of Police Constable Bain had been important.
It was submitted that the Lord Ordinary had been quite entitled to
prefer his evidence as to the state of the locus at the material time, as
opposed to evidence from other sources about that matter. He had provided adequate reasons for the view
of the evidence that he had taken in that connection.
[47] In support of
these submissions, senior counsel for the respondents drew our attention to
certain authorities. These were Thomas v Thomas; and Clarke v Edinburgh and District Tramways Co. Limited 1919 SC (HL) 35. In this latter case it
had been indicated that an appeal court, which did not have the advantage of
seeing and hearing the witnesses, should not interfere with the conclusion
reached by the judge of first instance, unless it could conclude that that
judge was plainly wrong. Reliance was
also placed on Thomson v Kvaerner Govan Limited 2004 SC (HL) 1.
[48] Some reliance
had been placed by the recliamer on Jordan v Court
Line Limited, Morrison v J.Kelly & Sons Limited and Rhesa Shipping Company S.A. v Edmunds.
Essentially these cases were concerned with what might be described as
extreme situations. The decisions
reached were not helpful in the present context for that reason.
[49] The fact was
that the Lord Ordinary had explained why he had preferred the evidence of
Police Constable Bain to that of the other witnesses who had given evidence of
the state of the road at the locus at the material time. In essence, Constable Bain had given a
careful and detailed description of the circumstances, while other witnesses
had given what might have been described as impressionistic and anecdotal
evidence.
[50] As regards the
cross-examination of witnesses on this particular topic, it had to be borne in
mind that these witnesses had been heard prior to the Lord Ordinary's decision
in relation to the inferential case.
When the witnesses were being examined, the respondents had regarded
themselves as facing only the so-called deviation case. The circumstances of Currie v Clamp's Executor were
so far removed from the present circumstances that what was said there was not
helpful.
[51] Turning to the
issue of sufficiency of precipitation, the contention was that the Lord
Ordinary had not been prepared to make the finding in fact sought by the
reclaimer that the quantity and intensity of the precipitation in the vicinity
if the Bridgend junction between the hours of 6.00 am and 9.00 am on 23
December 1995 were not such as would have washed away or diluted the effect of
salt in solution at the locus by the time of the accident. That was evident from what was said in
paragraphs [76] to [78] of his Opinion.
In that situation, while the case was not truly one of res ipsa loquitur, the onus of proof
determined the outcome of the case, as had occurred in Rhesa Shipping Company S.A. v Edmunds. The position was that the Lord Ordinary was
not making a finding that there had been torrential rainfall at the relevant
time and place, but he was accepting the evidence of Thomas Allen Brown and
concluding that the records of precipitation at Turnhouse were insufficiently
certain to be a reliable indication of the conditions at Bridgend. In any event, leaving aside Mr Brown's
evidence, the evidence showed material divergencies in results between the
records of the three meteorological stations.
It could not properly be said that the Lord Ordinary had not considered
all the relevant evidence. He had also
considered the significance of the measuring mechanism in use at the Turnhouse
station and its impact upon the records.
In any event, the records indicated only the conditions at the location
of the measuring instruments. The
Turnhouse records could certainly not be seen as constituting a certain
indication of conditions twelve kilometres away.
[52] Something had
been made in the course of the debate concerning the evidence of the East-West
front. However, the evidence showed that
there were variations within that front; in this connection reference was made
to the evidence of Mr Iain Farquhar and Mr Adrian Runacres. This material showed that the Lord Ordinary
had been quite entitled to reach the conclusion that he did.
[53] Senior counsel
went on to submit that the onus of proof rested with the reclaimer. With the failure of her primary case, she was
forced into reliance upon the so-called inferential case. The Lord Ordinary had not been prepared to
hold that the precipitation at Bridgend had been insufficient to account for
the existence of the black ice there. In
effect, that meant that the onus reverted to the reclaimer to demonstrate
negligence on the part of the respondents'.
However, having regard to the terms of the inferential case, that could
not be done. With a view to showing that
the present case was not one involving the principle of res ipsa loquitur, senior counsel relied upon The Law of Evidence in Scotland Walker and Walker 2nd edition,
paragraph 2.10; Ballard v North British Railway Company 1923 S.C.
(H.L.) 43; O'Hara v The Central S.M.T. Company Limited; Woods v Duncan and others [1946] A.C. 401 and Devine v Colvilles Limited 1969 SC (HL) 67. In short, the reclaiming
motion should fail, since the reclaimer had failed to discharge the onus
resting on her in relation to the only case available to her on the evidence,
the inferential case.
The decision
[54] It will be
evident from the narrative which we have given of the background to this case
and of the submissions made to us that the reclaiming motion involves an attack
upon the Lord Ordinary's decision on the facts of the case as found by him; there
is no contention that he has erred in law in any respect. Accordingly, this Court requires to adopt the
well-known approach to findings of fact made by a judge of first instance. That approach has been explained on many
previous occasions, but it is worth once again summarising it here.
[55] In Clarke v Edinburgh and District Tramways Co, at page 36 Lord Atkinson said
this:
"It is quite true that a Judge who
hears the witnesses has a great advantage in determining the question of their
credibility, but when you have to deal with the inference which he draws from
the evidence given before him, I think, before his finding is disturbed, it is
absolutely necessary that the Court of appeal
should be clear that he has drawn a wrong conclusion from the evidence"
In the same case, at pages 36 and 37, Lord Shaw of Dunfermline expressed his view thus:
"When a Judge hears and sees
witnesses and makes a conclusion or inference with regard to what is the weight
on balance of their evidence, that judgement is entitled to great respect, and that
quite irrespective of whether the Judge makes any observation with regard to credibility
or not. I can of course quite understand
a Court of appeal that says it will not interfere in a case which the Judge has
announced as part of his judgement that he believes one set of witnesses,
having seen them and heard them, and does not believe another. But that is not the ordinary case of a cause
in a Court of justice. In Courts of
justice in the ordinary case things are much more evenly divided; witnesses without
any conscious bias towards a conclusion may have in their demeanour, in their
manner, in their hesitation, in the nuance of their expressions, in even the
turns of the eyelid, left an impression upon the man who saw and heard them
which can never be reproduced in the printed page. What in such circumstances, thus
psychologically put, is the duty of an appellate Court? In my opinion, the duty of an appellate Court
in those circumstances is of each Judge of it to put to himself, as I now do in
this case, the question, Am I - who sit here without those advantages,
sometimes broad and sometimes subtle, which are the privilege of the Judge who
heard and tried the case - in a position, not having those privileges, to come
to a clear conclusion that the Judge who had them was plainly wrong? If I cannot be satisfied in my own mind that
the Judge with those privileges was plainly wrong, then it appears to me to be
my duty to defer to his judgment."
That dictum of Lord Shaw of Dunfermline was approved by Lord Thankerton in Thomas v Thomas, at page 55. At pages
59 and 60, the same view was expressed by Lord Macmillan in these terms:
"The appellate Court has before it
only the printed record of the evidence.
Were that the whole evidence, it might be said that the appellate Judges
were entitled and qualified to reach their own conclusion upon the case. But it is only part of the evidence. What is lacking is the evidence of the demeanour
of the witnesses, their candour or their partisanship, and all the incidental
elements so difficult to describe which make up the atmosphere of an actual
trial. This assistance the trial Judge
possesses in reaching his conclusion, but it is not available to the appellate
Court. So far as the case stands on
paper it not infrequently happens that a decision either way may seem equally
open. When this is so, and it may be
said of the present case, then the decision of the trial Judge, who has enjoyed
the advantages not available to the appellate Court, becomes of paramount importance
and ought not to be disturbed........The judgement of the trial Judge on the facts
may be demonstrated on the printed evidence to be affected by material
inconsistencies and inaccuracies, or he may be shown to have failed to
appreciate the weight or bearing of circumstances admitted or proved, or
otherwise to have gone plainly wrong............If the case on the printed evidence
leaves the facts in balance, as it may be fairly said to do, then the rule
enunciated in this House applies and brings the balance down on the side of the
trial Judge."
[56] Then more
recently these well-known views have been affirmed in Thomson v Kvaerner Govan
Limited 2004 SC (HL) 1 by Lord Hope of Craighead in paragraphs [16] and
[17].
[57] As already pointed
out, in paragraph [58] of his Opinion, the Lord Ordinary has rejected the
recliamer's primary case, indeed the only case specifically pled by her, the
so-called deviation case. In argument
before us, no attempt was made to challenge that part of the Lord Ordinary's
decision. Accordingly the focus of
attention is necessarily directed to what was referred throughout the
submissions as the inferential case. The
only basis in averment for that case is to be found in the passage, to which we
have already referred, between pages 7E to 8A of the reclaiming print. It will be evident from those averments that
this case was stated in the briefest terms; it is not elaborated in averment by
the reclaimer or the respondents.
However, as matters developed in the course of the proof, the requirements
of that case came to be more fully appreciated.
In particular, the level of precipitation at the time of or following
the third gritting on the L3 route in the vicinity of Bridgend came to be seen
as crucial. If that level of
precipitation were sufficient to wash away or substantially dilute the effect
of the salt laid during the course of that gritting, so that black ice could
form, the inference of fault based upon the existence of black ice at the locus
at the time of the accident, arising from some unspecified failure for which
the Council was responsible in connection with the third gritting, would
disappear and with it the inferential case.
Realising, no doubt, the importance of these considerations, in the
course of submissions to the Lord Ordinary, senior counsel for the reclaimer
invited him to make a finding in fact in the terms set out on page 75 of the
reclaiming print as finding 6. It was in
these terms:
"That the quantity and intensity of
the precipitation in the vicinity of the Bridgend junction between the hours of
06.00 and 09.00 on 23 December were not such as would have washed away or
diluted the effect of salt in solution at the locus by the time of the
accident."
As appears from paragraphs [78] and [79] of the Lord Ordinary's
Opinion, he declined to make that finding.
If that finding was essential to the recliamer's case, so far as that
case survived, which it was, it appears to us that the onus lay upon the
reclaimer to prove it. Thus what is
contended for in this reclaiming motion is that the Lord Ordinary was not
entitled to refuse to make such a finding.
Putting the matter otherwise, the contention must be that the Lord
Ordinary was bound to have made the finding desiderated, having regard to the
evidence. Plainly the difficulties
involved in that contention for the reclaimer are formidable.
[58] It will be
evident from what has already been said that there were two areas of fact which
bore directly upon the crucial matter.
These were the condition of the locus, as it was observed immediately or
within a short time of the occurrence of the accident and, secondly, the likely
level of precipitation in the vicinity of Bridgend during the material period
of time. It is appropriate for us to
examine these matters and the Lord Ordinary's approach to them in greater
detail.
[59] The matter of
the condition of the locus of the accident was explored in evidence at some
length. At the time when evidence
relating to it was led, the primary case averred by the reclaimer was very much
in contention. No doubt, therefore,
attention was focused upon the question of whether anything observable at the
locus did or did not support the deviation case. These matters are of course dealt with by the
Lord Ordinary in paragraphs [36] to [38] of his Opinion. It is in paragraph [37] that the Lord
Ordinary expresses his preference for the evidence of Police Constable Bain in
relation to the matter in question. The
formation of that preference on the part of the Lord Ordinary was, of course,
attacked. The question for us is
whether, having regard to the approach which we must take to the Lord
Ordinary's findings, that preference can survive. Looking at what is said by the Lord Ordinary
in that part of his Opinion, we have reached the conclusion that we cannot
interfere. The Lord Ordinary describes
the evidence given by the several other witnesses, who were at the locus on the
morning in question, and concludes that he could safely rely only on the
observations of witnesses as to that part of the road surface on which they
walked or drove, or which they inspected carefully. However, in relation to Police Constable Bain,
the Lord Ordinary observes that his interest on his arrival was primarily to
investigate the crash. He was qualified
in the investigation of such matters. He
examined the locus carefully. He walked
on both carriageways of the road over a considerable length on either side of
the junction. He indicated that there
was physical evidence that the road had been treated. He had noticed that particularly on the
eastbound carriageway. He could see the
grit and feel it and hear it crunching underfoot. The surface of the road was very slippery due
to ice, but according to his observation, the whole road was not a "sheet of
ice"; there were extensive patches of ice on the road, but other parts were not
affected. Against this background the
Lord Ordinary accepted his evidence, both as to the extent of the ice cover on
the road and his observations of grit.
In view of the reasons given by the Lord Ordinary for his reliance on
Police Constable Bain and his qualifications in relation to the evidence of other
witnesses, all of whom the Lord Ordinary had had the chance to hear and
observe, we can see no basis upon which we could interfere with his
decision. It would be quite impossible
for us to say that, in this regard, the Lord Ordinary was plainly wrong.
[60] It is plain
that the Lord Ordinary's findings based upon the evidence of Police Constable
Bain have a dual significance. First,
the extent of the ice cover on either side of the junction plainly undermines
the idea that the appearance of ice at the locus of the accident was the result
of the alleged diversionary manoeuvres which formed the basis of the reclaimer's
primary case. Secondly, the patchy
nature of the ice cover is capable of being seen as supporting a conclusion
that gritting had taken place but that precipitation had rendered it
ineffective in certain parts of the road surface.
[61] Turning now to
the second main area of factual controversy, the level of likely precipitation
in the vicinity of Bridgend during the material period of time, the Lord
Ordinary deals with these matters in paragraphs [74] to [78] of his
Opinion. It is evident that from
paragraph [78] that, in reaching the conclusions which he did, the Lord
Ordinary relied heavily upon the evidence of Mr Thomas Allen Brown, the driver
of the gritting lorry used to undertake the third gritting on route L3. The Lord Ordinary gives his reasons for
accepting Mr Brown's evidence in paragraph [44] of his Opinion. It was a fundamental part of the reclaimer's
criticism of the Lord Ordinary's
decision in this respect that Mr Brown's evidence conflicted with the records
of rainfall derived particularly from the meteorological station at
Turnhouse. The Lord Ordinary deals with
that contention in some detail. In the
first place, he lays emphasis upon the distance between the meteorological
station at Turnhouse and the stretch of road in the vicinity of Duntarvie in the
direction of Linlithgow over which Mr Brown indicated that there had been a prolonged
and intense downpour. As appears from
paragraph [45] that distance was between 8 and 14 kilometres. In the second place, in the same paragraph
the Lord Ordinary goes into considerable detail in making findings as to the
method of measurement of rainfall at the Turnhouse meteorological station,
which led him to the conclusion which he states in that paragraph. The readings recorded in the Turnhouse data
for the hours up to 0600 and 0700 on 23 December 1995 were both 0.4 millimetres. However, because of the method of measurement
involved, he considered that one or both of those records could represent a true
hourly rainfall of up to 0.6 millimetres.
In the third place, in relation to the significance of meteorological
data derived from one location, as a basis of reaching a conclusion as to the
conditions at another, the Lord Ordinary relied upon the evidence of Mr Adrian
Runacres, whose qualifications he describes in paragraph [53] of his
Opinion. In paragraph [55] the Lord
Ordinary relies upon the opinion expressed by Mr Runacres to the effect that,
in terms of the likely intensity of the rain at the locus, it was unsafe to rely
upon data from one site to infer conditions a few kilometres away. Precipitation clouds were typically two to
three kilometres across. It could not
necessarily be said that conditions were the same even three kilometres
away. Mr Runacres would not have been
surprised to find that witnesses spoke of conditions at one place which
differed from conditions recorded at another only a few miles away. In the fourth place, as already explained in
connection with this aspect of the case, the Lord Ordinary relied upon the
implications of what had been said by Police Constable Bain as regards the
patchy ice cover at the locus of the accident.
[62] Looking at the
reasons which the Lord Ordinary gives for his refusal to make the finding
desiderated on behalf of the reclaimer, we conclude that it is not open to us
to interfere with his decision. The
reasons which the Lord Ordinary gives for his conclusion appear to us to have a
proper basis in the evidence set before him.
On any view of the matter, we are quite unable to say that in this
regard the Lord Ordinary was plainly wrong.
We think that it is right to comment that, throughout the course of the
debate before us, on behalf of the reclaimer, undue emphasis seemed to us to be
placed upon the data available from the meteorological station at Turnhouse. The assumption appeared to be made that what
had been recorded there furnished an unassailable indication of what conditions
were at Bridgend. Although it is not a
matter for us to form our own view on the printed evidence, it appears to us
that there are insuperable difficulties involved in such an approach. We need only refer to the Lord Ordinary's
reasoning in this regard. For all of
these reasons, we conclude that we are unable to interfere with the Lord
Ordinary's conclusions on fact in relation to this crucial aspect of the reclaimer's
inferential case. It follows that we
cannot interfere with the Lord Ordinary's conclusion as to the disposal of that
case. In all these circumstances it is
unnecessary for us to consider the submissions made as to what findings we ourselves
should make on the evidence, in the event of the Lord Ordinary's findings
having been discarded.
[63] It is
appropriate for us to say a word or two concerning certain criticisms which
were made of the Lord Ordinary's reasoning in paragraph [78] of his
Opinion. The passage concerned is to be
found between page 92D and page 93C.
Having earlier found that he accepted the evidence of Mr Brown that the third
gritting run had in fact been carried out on route L3, the Lord Ordinary
observes that
"To make a finding that the
precipitation could not have washed away or diluted the effect of the salt,
therefore, I would require to infer that something had gone seriously wrong
with the spreading operation, to the extent that practically no salt was spread
on a 200 metre (and only a 200 metre)
stretch of road; whether it be that
an insufficient quantity of salt was loaded in the hopper; or that the gate at
the back was blocked; or that the salt was wet and became clogged; or that
there was a problem with the engine which drives the belt that pushes salt out
of the hopper; or that some other problem occurred. No case was pled along these lines and no
evidence was led to this effect. But I
cannot, simply because there has been no investigation of those matters, put
them out of mind entirely. It was always
open to the pursuer to plead a case raising the issue, as a matter of
inference, that there must have been some such problem and have sought to
recover documents relating thereto. The lack
of any information about this aspect is part of the overall picture that I have
to take into account in deciding whether the pursuer
has shown, albeit on a balance of
probabilities, that there was insufficient
rain to dissipate the salt; and that
therefore the only explanation is
that no salt, or only minimal
quantities, was spread. Of course, if
the expert evidence led by the pursuer was sufficiently compelling and capable
of being resolved in isolation with any degree of certainty, it could overcome
these concerns. But I do not consider
that it did lend itself to such an approach."
[64] We have to say
that we have had some difficulty in following the Lord Ordinary's reasoning in
this part of his Opinion. However,
leaving that point aside for a moment, the various circumstances referred to by
the Lord Ordinary, which might have interfered with the spreading of salt on
the road were not the subject of any specific averments. In that situation, in our view there was no
reason why the Lord Ordinary should have given consideration to these
particular issues. He was quite correct
in observing that it had been open to the pursuer to plead a case relating to
possible problems in the distribution of salt from the vehicles involved at the
material time, but, of course, that was not done. In that situation, we see no reason why the
Lord Ordinary should have given further consideration to those matters. However, having said that, we do not think
that anything contained in the passage concerned affects the overall view which
we have formed as to the Lord Ordinary's treatment of the facts of this case.
[65] In the whole
circumstances the reclaiming motion is refused.
We shall adhere to the Lord Ordinary's interlocutor of 3
November 2005.