changes in snow season in lapland from regional climate models john moore 1,2, and aslak grinsted 1...
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![Page 1: Changes in snow season in Lapland from regional climate models John Moore 1,2, and Aslak Grinsted 1 1 Arctic centre, University of Lapland Rovaneimi, Finland](https://reader037.vdocument.in/reader037/viewer/2022110304/551945c8550346990b8b459c/html5/thumbnails/1.jpg)
Changes in snow season in Lapland from regional climate
models
John Moore1,2, and Aslak Grinsted1
1 Arctic centre, University of Lapland
Rovaneimi, Finland 2 Thule Institute, University of Oulu,
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CO2 EMISSIONS PROFILESunder IPCC SRES scenarios
Source:IPCC
Used here
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GLOBAL TEMPERATURE RISEdue to four SRES emissions scenarios
Source: Hadley Centre
Used here
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GCM used for all regional models: HadAM3H
1961-1990 runs used control
2071-2100 with A2 forcing as scenarios
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Coarse resolution GCM model with Regional model nested inside at 25 km grid point spacing
Compared with 300 km grid points of GCM
50 km grid points
Still not enough to show much Mountainous topography – would need less than 10 km, we only have 25 km
12.5 km grid
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Christensen & Christensen, Nature (2003)
Sensitivity due to GCM and RCM resolution
ECHAM Hadley 50km Hadley 25km
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AGCM exp forcing
HadAM3H
ARPEGE ECHAM5 CCM3
HadCM3 SRES A2
3 ensemble members 150 km BDY 1
2 mem high res.
1 member T106
2 members T80 BDY4
HadCM3 SRES B2
1 member 150 km BDY 2
1 mem high res.
ECHAM4/OPYC3 SRES A2
1 member T106 BDY 3
ARPEGE/OPA SRES B2
1 mem high res.
RCM 50km Input
P5
P9
P1 P10 P6 P2/P12 P8 P7
BDY 1 3 mem 3 mem BDY 1 1 mem 1 mem 1 mem 1 mem 1 mem 1 mem BDY 1 ini cond.
1 mem
BDY 2 1 mem 1 mem 1 mem BDY 3 1 mem BDY 4 1 mem RCM 20 km Input
P5 P9 P1 P6 P8
BDY 1 1 mem 1 mem 1 mem 1 mem 1 mem
DMIHad Rossby Es ETH IPCC MPI GKSS
MeteoT42
100km
12 km
PRUDENCE http://prudence.dmi.dk/ set of models
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Regional climate models
• 9 for temperature– CNRM (France)– DMI (Denmark)– ETH (Switzerland)– HC (UK)– GKSS Germany)– KNMI (Netherlands)– MET NO (Norway)– MPI (Germany)– SMHI (Sweden)
•6 for snow season –DMI (Denmark)–ETH (Swiss)–GKSS (Germany)–KNMI (Netherlands)–MPI (Germany)–SMHI (Sweden)
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Simulated changes in winter (DJF) and summer (JJA) precipitation from the period 1961-1990 to 2071-2100. SMHI regional climate model with boundary conditions from the HadAM3H (left) and from the ECHAM4 (right).
A future warming that will be largest in winter in northern Europe and largest in summer in southern Europe.
Increased precipitation in northern Europe, especially during winter, and decreased precipitation in southern Europe during summer.
Europe view
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Simulated change in average summer temperature (upper panel) from the period 1961-1990 to the period 2071-2100.
Temperature changes in summer modest of Scandinavia compared with much of Europe
To make robust forcasts of changes we need to use the long term predictions and averages over at least 30 years.
This avoids to ”signal” of climate change becoming lost in the ”noise” of random weather
Europe view
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Comparison of 6 snow models
Lapland Snow Season - Control
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Comparison of 6 snow models
Lapland Snow Season - Forecast
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Changes in snow season
Lapland Snow Season - Change
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Ylläs Rovaniemi Pyhäend of season 0.20 0.23 0.22 days/yearstart of season 0.23 0.28 0.28 days/year
length of season 0.27 0.34 0.31 % per year
mean snow loss 0.45 0.55 0.52 % per yearmax snow thickness loss 0.29 0.39 0.36 % per year
Ylläs Rovaniemi Pyhäend of season 1 week in 34 31 32 yearsstart of season 1 week in 31 25 25 years
length of season 1 week in 16 14 14 years
Snow Season Change 1975-2085
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Chance of No Snow at Christmas Time (<10 kg/m2)
Models show winters will be wetter, but less snow cover
More iceMore rain
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Temperature annual cycle 2085 – 9 models Ylläs
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Temperature annual cycle 1975-2085 mean differences
Winters warmer by about 4-5C
Summers warmer by about 2-3C
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Reduced number of freezing days - Lapland
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Ylläs Rovaniemi Pyhäblower benefits 0.03 0.08 0.08 days/year
errors 0.05 0.05 0.06 days/year
Possible use of artificial snow making
Balance between rate of decrease in days below zero, and time of start of snow cover
Very large uncertaintity – little difference to benefit rate if -3C used instead of zero
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Tamperemean snow loss 0.72 % per year
max snow thickness loss 0.54 % per yearlength of season 0.62 % per year
Impact on snow season greater further South
Rovaniemi in 2085 like Tampere in 1975
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Conclusions
• 4-5°C/Century winter warming in Lapland• More rainfall, more ice, wet slushy snow• Much greater risk of dark Christmas, especially
in Rovaniemi• Rovaniemi 2085 like Tampere 1975• Snow season shorter by about 1 week every 15
years in Lapland• Reduced snow pack thickness due to less snow
and denser snow• Average snow affected more than peak snow• Bigger changes further South