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Technical Note (National Research Council of Canada. Division of Building Research), 1954-07-01
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Minimum Temperatures in Various Wind Speed Ranges
Boyd, D. W.
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DIVISION OF BUILDING RESEARCH
NATIONAL RESEARCH COUNCIL OF CANADA
'f
E
C
1HI N ][ CAlL
NOTE
No.
178
NOT FOR PUBLICATION FOR INTERNAL USE
PREPARED BY D. W. Boyd CHECKED BY APPROVED BY
PREPARED FOR Inquiry reply. MI§.. July
1954
SUBJECT Minimum temperatures in various wind speed ranges.
This Note contains information on certain minimum
tempera-エセ・ data obtained by the Meteorological Division, Department of
Transport, in answer to an inquiry from the ReAP. The following data
and comments are of special interest to the Division of Building
Research as they are closely related to building design in the North.
Records from the following stations were analysed: Watson
Lake, Yukon; Fort Nelson, B.C.; McMurray, Alta.; The Pas, Man.; Churchill, Man.; Trout Lake, Ont.; Armstrong, Ont.; Great Whale River, P.Q.; Knob Lake, P.Q.; Nitchequon, P.Q.; Goose Bay, Labrador; and Cape Harrison, Labrador.
The following table gives the minimum temperatures iD
degrees Fahrenheit for various wind speeds in m.p.h. TABLE I
MINIMUM TEMPERATURES
(in OF for various wind speeds in m.p.h.)
0-9
10-19
20-29
30-39
40
and upWatson Lake, Yukon
-60
-29-15
Fort Nelson, B.C.
-47
-38
-19
---McMurray, Alta.
-57
-35
-12
34-
---The Pas, Man.
-46
-42
-30
-21
Churchill, Man.
-46
:tti
-41
-40
-23
Trout Lake, ant.
-48
-28
セQYArmstrong, Ont.
-57
-41
-26
-21
16
Great Whale River, Que.
-50
-45
-36
-25
-9Knob Lake, Que.
-58
-43
-38
-25
-16
Nitchequon, セオ・N
-55
-42
-32
-25
8
Goose Bay, Lab.
-32
-31
-30
-17
-3
Cape Harrison, Lab.
-21
-23
-24
-25
-17
Nセ
For most of the stations the hourly reports for January,FebruarY', March, and December for five Y'ears
(1949-1953)
were2
-each of the ranges 0 to 9, 10 to 19, 20 to 29, 30 to 39, and 40
m.p.h. and up, was found. For a tew stations only six- or
three-hourly reports were available.
The minimwn temperatures are plotted in Fig. 1. In
general, the lowest temperatures occur with light winds. This is
most noticeable at Watson Lake, McMurray, Armstrong, Hitchequon, and
Knob Lake. At tour of the stations, Fort Nelson, The Pas, Trout
Lake, and Great Whale River there 1s less difterence between th..
minimum temperatures at 0 to 9 and 10 to 19 m.p.h. but much higher
minima occur with stronger winds. At Cape Ha:rrison, Goose Bay, and
Churchill the minima remain remarkably constant until quite strong
winds are reached. It must be remembered that the strong winds are
less trequent, and therefore there is a much smaller sample from
which to obtain a minLmum temperature at these high speeds. This
tact tends to cause a rapid increase in the slopes of the curves at
higher speeds. It may also account tor the steep slope between
10 to 19 and 20 to 29 m.p.h. at such stations as Fort Nelson and
Trout Lake.
Although the accuracy ot these curves may be questioned
because of the short period of records (tive winters), the coarse wind speed ranges, and the unequal sampling, nevertheless they show
that the wind velocity occurring at low temperatures can varY'
widely from one location to another in the North of Canada. This
is of considerable importance in establishing conditions for
calculation of heat losses from buildings. At Watson Lake, fo:r
example, the most severe condition tor heating may well be 60 below zero and calm, while at Churchill, where the minimum temperature is
only
46
below, one must also consider a 40 below zero temperatureI
I I I/
, 404 up 30-.39 M.P. H.----_
..- . 20-'29 RANGE.... IN 10- 19 \V I N C7 S PE.. E..D CAPE. ...-GMBMセセZZGセ⦅json .•,., " - " I gooセヲNN e.AY .. - - - : - - - 4 , / / セNNN J.. -'20o
-50 30 10 z - -TO :E-.30 :J セ 2 セ -40 u.. oFIG UR E.. 1 GRAPI-l S 1-10 \\1\ N G RE.-L AT \ 0 N S1-1\ P BE..T \'1 E.. E..N
_M_I_N_tM_U_M_ _T_E.._M_PE..RATU RE,... AND \V \ N 0 '5