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1 Climate change and the cryosphere. 2 Outline Background, climatology & variability Role of snow in the global climate system Contemporary observations.

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Presentation on theme: "1 Climate change and the cryosphere. 2 Outline Background, climatology & variability Role of snow in the global climate system Contemporary observations."— Presentation transcript:

1 1 Climate change and the cryosphere

2 2 Outline Background, climatology & variability Role of snow in the global climate system Contemporary observations of climate change Cryospheric indicators of climate change Future global & regional projections & implications of climate change

3 3 Background, climatology & variability

4 4 20 th Century Climatology Observed GFDL Ref: Masuda

5 5 Current snow coverage 1 April 2013

6 6 Departure from average 1 April 2013

7 7 Seasonal climatology

8 8 Observed & GFDL Northern Hemisphere Snow Extent (x10 6 km 2 ), 1973-2000 SeasonOBSGFDLMAERMSE Winter44422.40.55 Spring30354.81.00 Summer642.30.51 Fall19201.70.40 Annual25 0.90.22

9 9 Mean annual maximum monthly snow water equivalent (mm) in Canada, 1980- 1997 (Brown et al. 2003)

10 10 Current SWE in the Prairies

11 11 Monthly Eurasian standardized snow cover extent anomalies

12 12 Interannual variability Source: Karl et al. (1993).

13 13 Role of snow in the global climate system

14 14 Annual cycle of daily discharge in Skeena River (1955-2004) freshet

15 15 Contribution of snow to river runoff Source: Barnett et al. (2005).

16 16 Teleconnections Definition: Atmospheric interactions between widely separated regions that have been identified through statistical correlations (in space and time). For example, the El Niño teleconnection with the Southwest United States involves large-scale changes in climatic conditions that are linked to increased winter rainfall.

17 17

18 18 Correlation coefficient between annual Eurasian snow extent anomalies & discharge anomalies the following year in 64 rivers of northern Canada Source: Déry et al. (2005), JGR.

19 19 Observed 20 th century climate change

20 20 Warming air temperatures Climatic Research Unit, University of East Anglia, http://www.cru.uea.ac.uk/

21 21 20 th century climate & trends Reference: Déry and Wood (2005)

22 22 Trends in global surface air temperature

23 23 Trends in global surface precipitation

24 24 Cryospheric indicators of global change Snow depth, swe, density, albedo & temperature (heat content) Duration of snow cover & growing season Snowmelt/spring freshet date Soil moisture

25 25 Snow depth Source: Curtis et al. (1998), Int. J. Climatology

26 26

27 27 Annual cycle of daily snow accumulation (SWE) at Barkerville

28 28

29 29 Trend (%) in April 1 st swe, 1950- 1997 Source: Mote et al. (2005), BAMS

30 30 Albedo Source: Stone et al. (2002), JGR.

31 31 Trend (days/year) in snow cover duration, 1972-2000

32 32

33 33 Snowmelt Date Source: Stone et al. (2002), JGR.

34 34 Reference: Déry and Brown (2007)

35 35 Annual cycle of daily runoff for the Little Swift River near Barkerville

36 36 Trend in centre of volume in river discharge across western N. America Source: Stewart et al. (2005), J. Climate.

37 37 Future projections & implications of global change

38 38 Components of the climate system

39 39 IPCC 4th Assessment

40 40 IPCC 4th Assessment

41 41 Expected indicators of climate change IPCC 3 rd Assessment

42 42 IPCC 4th Assessment

43 43 IPCC 4th Assessment

44 44 IPCC 4 th Assessment Runs

45 45 Trends in Northern Hemisphere snow cover extent Source: Déry et al. (2006), JGR.

46 46 Projected change in seasonal snow cover frequency based on GFDL CM2 simulations (21 st - 20 th century) Projected change in frequency -0

47 47 Trends in Northern Hemisphere snow mass

48 48 Projected change in seasonal snow water equivalent (swe) based on GFDL CM2 simulations (21 st - 20 th century) Projected change in swe (mm)

49 49

50 50 Regional climate (baseline) Source: PCIC (http://www.pcic.uvic.ca)

51 51 Temperature Projections

52 52 Precipitation projections

53 53 Regional Projections for snow

54 54 Implications of global change Increase in planetary albedo (positive feedback on global warming) Decreasing water resources, including soil moisture Longer growing season Impacts on recreational activities Ecological implications

55 55 Further reading:

56 56 Points of Discussion: Which component of the cryosphere is most vulnerable to climate change? What are the possible environmental impacts of climate change in Prince George, B.C., Canada? Will there be any jobs for cryospheric scientists in the 21 st century?


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