This document analyzes possible evidence of climate change in the Sverdlovsk region of Russia. It examines trends in average annual temperature, which has shown a weak increase, as well as January temperatures, snow cover thickness, relative humidity, and river discharge levels over the past 80 years. One clear trend is that the duration of the heating period in Yekaterinburg has decreased by 12 days while average temperatures have increased by 1.1 degrees Celsius from 1962 to 2012. However, the document concludes that the wavy nature of the data does not allow for clear trends or predictions about the region's future climate to be made.
2. Climate of Sverdlovsk region
Latitude length of the region is
more than 600 km and
differences in relief are cause a
variety of climatic conditions.
Continental climate of the Ural
plains increases from Northwest
to Southeast.
Average January temperature
increases from -20°C in the
North to -16°C in the South.
Average July temperature varies
from +16°C in the North to
+19°C in the South.
The average annual
precipitation In the Southeast of
the region is 350 to 400 mm, in
the North is 500 mm, and
exceeds 500-600 mm in the
mountains of Southwest.
3. Information sources
Annual weather database
“Climate of Russian cities”
A Regional, Electronic,
Hydrographic Data Network For
the Arctic Region
http://atlas-
yakutia.ru/weather/climate_russia-
III.html
http://www.r-
arcticnet.sr.unh.edu/v4.0/
4. Average annual temperature
Weakly pronounced trend towards
increasing (see the “envelope”
curve – linear filtration based on 2
points).
There are no years with average
annual temperature below zero
after 1972. Before this date,
temperature sharply becomes
negative approximately ones per
ten-twelve years.
After the 1972 this effect
continuously neglected and curve
is smoothened.
-4
-2
0
2
4
6
8
1934
1938
1942
1946
1950
1954
1958
1962
1966
1970
1974
1978
1982
1986
1990
1994
1998
2002
2006
2010
T, OC
YEAR
5. Wavy dynamic of climatic values
Average January
temperature
68
70
72
74
76
78
80
1950
1954
1958
1962
1966
1970
1974
1978
1982
1986
1990
1994
1998
2002
2006
2010
HR, %
YEAR
Average monthly snow
cover thickness
0
20
40
60
80
100
120
1949
1953
1957
1961
1965
1969
1973
1977
1981
1985
1989
1993
1997
2001
2005
2009
H, CM
YEAR
Average annual relative
humidity of air
-28
-26
-24
-22
-20
-18
-16
-14
-12
-10
1934
1938
1942
1946
1950
1954
1958
1962
1966
1970
1974
1978
1982
1986
1990
1994
1998
2002
2006
2010
T, OC
YEAR
After 70s
After 70s After 70s
6. Average annual water discharge of rivers
0
0.2
0.4
0.6
0.8
1
1.2 1896
1901
1906
1911
1916
1921
1926
1931
1936
1941
1946
1951
1956
1961
1966
1971
1976
1981
1986
1991
1996
G/Gmax
YEAR
ISET SINARA SOSVA TURA
TAVDA PUSHMA TOBOL LOBVA
G, m3/s – average annual water discharge of river
Gmax, m3/s – maximum of average annual water discharge of river
7. Parameters of heating period in
Yekaterinburg
Year of
revision
Duration,
days
Average
temperature, oC
Reference
1962 233 -6.5 SNiP II-A.6-62 “Building climatology
and geophysics”
1972 228 -6.4 SNiP II-A.6-72 “Building climatology
and geophysics”
1982 228 -6.4 SNiP 2.01.01-82 “Building climatology
and geophysics”
1999 230 -6.0 SNiP 23-01-99 “Building climatology”
2012 221 -5.4 SP 131.13330.2012 “Building
climatology”
Duration of heating period decreases during 1962-2012 by 12 days and average
temperature increases by 1.1 oC.
8. Conclusions
All described data may be used to appreciate some evidentiary of climate
change in Sverdlovsk region.
These data may show relationship between climate change and water balance
of Sverdlovsk region.
However, wavy and sharp dynamic of described values during period of 80
years does not allow to show clear trends and to make predictions about
future of regional climate.
Sverdlovsk region probably will return into continental climate with cold
winters, and parameters of heating period in Yekaterinburg will follow this
trend.