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Whither Arctic Sea Ice? Walt Meier Climate Literacy and Energy Awareness Network May 9, 2011 http://nsidc.org Cooperative Institute for Research  in Environmental Sciences University of  Colorado
The Cryosphere Snow and ice spans the globe, from the equator to the poles. The cryosphere is found in over 100 countries. Sea ice forms by the freezing of the ocean. Can occur from pole to over halfway to the equator in the north. Integrated Global Observing Strategy (IGOS) Cryosphere Theme Report Countries affected by the cryosphere
Sea ice extent varies through the year Mar = 15,000,000 km 2 Sep = 7,000,000 km 2 Mar = 4,000,000 km 2 Sep = 19,000,000 km 2 Average extent for 1979-2000 from satellite data Adapted from NSIDC Sea Ice Index http://nsidc.org/data/seaice_index/
Summer Arctic sea ice is declining -11.6% per decade 1979-2000 Average 2007: 39% below average 2008: 34% below average 2009: 24% below average 2010: 30% below average 1979-2000 Median Thanks to Matt Savoie, NSIDC
Heading into summer 2011… NSIDC Arctic Sea Ice News & Analysis, http://nsidc.org/arcticseaicenews/ Sea Ice Extent, May 7, 2011
Ice is getting younger and thinner Based on satellite observations; from J. Maslanik, C. Fowler, Univ. Colorado Sea ice moves with winds and currents. Moves out of Arctic along Greenland coast, replenished by new ice. 1981-2007 Weekly sea ice motion
Ice is getting younger and thinner Based on satellite observations; from J. Maslanik, C. Fowler, Univ. Colorado Much of older, thicker ice north of Alaska melting away during summer Mar 2010 – Mar 2011 Mar 1985 – Mar 1986
IPCC 4 th  Assessment – Business as Usual Scenario Warming by the end of the 21 st  Century: Global mean = 2.8 º C (~5 º F); Arctic = ~7 º C (~13 º F) º C IPCC 4 th  Assessment, courtesy S. Solomon
Loss of summer sea ice decreases albedo 60% of energy reflected 40% of energy absorbed 10% of energy reflected 90% of energy absorbed The change from sea ice to ice-free ocean is the largest surface contrast on earth as far as solar energy is concerned With sea ice:  α   ≥ 60% Without sea ice:  α   ≤ 10% Ice Water
Sea Ice – Albedo Feedback Temperature  ↑ Ice melt  ↑ Albedo  ↓ Energy absorption  ↑ Heat  ↑ Amplification of warming
The sea ice-albedo feedback observed ,[object Object],[object Object],Solar heat input from D. Perovich (CRREL)
The sea ice-albedo feedback observed ,[object Object],August 2007 SST Anomaly ,[object Object],[object Object],SST from NOAA and M. Steele, Univ. of Washington
Arctic Amplification observed ,[object Object],[object Object],[object Object],From Serreze, et al., 2008; data from NOAA NCEP Autumn air temperature anomalies, (2003-2007) minus (1979-2007)
Observations faster than forecast by IPCC models  Updated from Stroeve et al., 2007 Observations Model Average Model Range (+/- 1 st. dev.) Arctic September Average Sea Ice Extent IPCC AR4 models,1900-2100 Observations, 1953-2010
Impacts of loss of summer sea ice Photo by Mike Webber, U.S. Fish & Wildlife Service
Biological impacts ,[object Object],[object Object]
Can polar bears be saved?? ,[object Object],“ Business as usual” to 2100 Stable GHG levels after 2020 10-year running average September sea ice extent Amstrup, S.C., et al.  Nature , vol . 468, 16 December 2010.
Summer sea ice returns if CO 2  levels drop (as function of time) * Arctic September Average Sea Ice Extent NCAR Community Sea Ice Model Thanks to Marika Holland, NCAR CO 2  increases to 700 ppm by 2100 (A1B), then drops to 2000 level by 2200    Summer sea ice extent disappears, but returns as CO 2  level drops Sea ice responds directly to CO 2  levels: CO 2  rises    sea ice decreases CO 2  drops    sea ice increases No tipping point? (as function of CO2)
Biological impacts ,[object Object],[object Object],Difference in primary production from 2006 to 2007 redrawn from  Arrigo et al., 2008
Coastal Erosion – Kivalina & Shishmaref, Alaska Erosion in Shishmaref, Oct. 2002 Storm 2 hours later AP/NY Times Shishmaref photos by Tony Weyiouanna Sr.
Sea ice loss opening up a new ocean New York Times, 10 Oct 2005 ,[object Object],[object Object],[object Object],[object Object],[object Object]
Already seeing impact of ice loss on climate ,[object Object],[object Object],[object Object],mm day -1 Precipitation change: Low ice years minus high ice years 1981-2007 J. Francis, Rutgers Univ.; Francis et al., Geophys. Res. Letters, 2009 U.S.
Can sea ice loss cause colder temperatures? ,[object Object],[object Object],[object Object],[object Object],[object Object]
Cold spilling out of the Arctic NCEP/NCAR Reanalyses, http://www.esrl.noaa.gov/psd/data/reanalysis/ 850 mb Geopotential Height Dec-Feb 1968-1996 Avg. Feb 2010 Dec 2010 Arctic air “lower”, in a bowl Cold stays in the Arctic Cold air spills out of the Arctic Winter 2009-2010 Winter 2010-2011 Thanks to J. Overland, NOAA PMEL
Whither Arctic Sea Ice? Using Sea Ice Data in the Classroom AccessData  Earth Exploration Toolbook chapter http://serc.carleton.edu/eet/seaice/ Developed by: Walt Meier  National Snow and Ice Data Center, Univ. Colorado Coop. Inst. for Research in Environmental Sciences Betsy Youngman Phoenix Country Day School Mark McCaffrey Coop. Inst. for Research in Environmental Sciences Anupma Prakash Geophysical Institute, University of Alaska Fairbanks Brian Rogan Boston Museum of Science
Whither Arctic Sea Ice? Using Sea Ice Data in the Classroom ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],http://serc.carleton.edu/eet/seaice/
Hudson Bay Case Study ,[object Object],[object Object],[object Object]
Resources on Arctic climate NOAA  Arctic Change, http://www.arctic.noaa.gov/
SnowTweets Project R. Kelly, Univ. Waterloo, http://snowcore.uwaterloo.ca/snowtweets/
NSIDC resources Atlas of the Cryosphere, http://nsidc.org/data/atlas/ WMS, OCG compliant web map server Several Arctic layers – sea ice snow, permafrost, snow, geographic locations http://nsidc.org/data/atlas/
NSIDC Arctic Sea Ice News and Analysis ,[object Object],[object Object],[object Object],http://nsidc.org/arcticseaicenews/
NSIDC “Icelights” ,[object Object],[object Object],http://nsidc.org/icelights/
NSIDC Education Center ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],http://nsidc.org/cryosphere/
NSIDC data on Google Earth ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],NSIDC Data on GoogleEarth http://nsidc.org/data/virtual_globes/
NSIDC data on Google Earth ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],NSIDC Data on GoogleEarth http://nsidc.org/data/virtual_globes/
For the Arctic, Climate Change is Already Here ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Funding and Support from Thank You!

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Meier clean presentation_ppt

  • 1. Whither Arctic Sea Ice? Walt Meier Climate Literacy and Energy Awareness Network May 9, 2011 http://nsidc.org Cooperative Institute for Research in Environmental Sciences University of Colorado
  • 2. The Cryosphere Snow and ice spans the globe, from the equator to the poles. The cryosphere is found in over 100 countries. Sea ice forms by the freezing of the ocean. Can occur from pole to over halfway to the equator in the north. Integrated Global Observing Strategy (IGOS) Cryosphere Theme Report Countries affected by the cryosphere
  • 3. Sea ice extent varies through the year Mar = 15,000,000 km 2 Sep = 7,000,000 km 2 Mar = 4,000,000 km 2 Sep = 19,000,000 km 2 Average extent for 1979-2000 from satellite data Adapted from NSIDC Sea Ice Index http://nsidc.org/data/seaice_index/
  • 4. Summer Arctic sea ice is declining -11.6% per decade 1979-2000 Average 2007: 39% below average 2008: 34% below average 2009: 24% below average 2010: 30% below average 1979-2000 Median Thanks to Matt Savoie, NSIDC
  • 5. Heading into summer 2011… NSIDC Arctic Sea Ice News & Analysis, http://nsidc.org/arcticseaicenews/ Sea Ice Extent, May 7, 2011
  • 6. Ice is getting younger and thinner Based on satellite observations; from J. Maslanik, C. Fowler, Univ. Colorado Sea ice moves with winds and currents. Moves out of Arctic along Greenland coast, replenished by new ice. 1981-2007 Weekly sea ice motion
  • 7. Ice is getting younger and thinner Based on satellite observations; from J. Maslanik, C. Fowler, Univ. Colorado Much of older, thicker ice north of Alaska melting away during summer Mar 2010 – Mar 2011 Mar 1985 – Mar 1986
  • 8. IPCC 4 th Assessment – Business as Usual Scenario Warming by the end of the 21 st Century: Global mean = 2.8 º C (~5 º F); Arctic = ~7 º C (~13 º F) º C IPCC 4 th Assessment, courtesy S. Solomon
  • 9. Loss of summer sea ice decreases albedo 60% of energy reflected 40% of energy absorbed 10% of energy reflected 90% of energy absorbed The change from sea ice to ice-free ocean is the largest surface contrast on earth as far as solar energy is concerned With sea ice: α ≥ 60% Without sea ice: α ≤ 10% Ice Water
  • 10. Sea Ice – Albedo Feedback Temperature ↑ Ice melt ↑ Albedo ↓ Energy absorption ↑ Heat ↑ Amplification of warming
  • 11.
  • 12.
  • 13.
  • 14. Observations faster than forecast by IPCC models Updated from Stroeve et al., 2007 Observations Model Average Model Range (+/- 1 st. dev.) Arctic September Average Sea Ice Extent IPCC AR4 models,1900-2100 Observations, 1953-2010
  • 15. Impacts of loss of summer sea ice Photo by Mike Webber, U.S. Fish & Wildlife Service
  • 16.
  • 17.
  • 18. Summer sea ice returns if CO 2 levels drop (as function of time) * Arctic September Average Sea Ice Extent NCAR Community Sea Ice Model Thanks to Marika Holland, NCAR CO 2 increases to 700 ppm by 2100 (A1B), then drops to 2000 level by 2200  Summer sea ice extent disappears, but returns as CO 2 level drops Sea ice responds directly to CO 2 levels: CO 2 rises  sea ice decreases CO 2 drops  sea ice increases No tipping point? (as function of CO2)
  • 19.
  • 20. Coastal Erosion – Kivalina & Shishmaref, Alaska Erosion in Shishmaref, Oct. 2002 Storm 2 hours later AP/NY Times Shishmaref photos by Tony Weyiouanna Sr.
  • 21.
  • 22.
  • 23.
  • 24. Cold spilling out of the Arctic NCEP/NCAR Reanalyses, http://www.esrl.noaa.gov/psd/data/reanalysis/ 850 mb Geopotential Height Dec-Feb 1968-1996 Avg. Feb 2010 Dec 2010 Arctic air “lower”, in a bowl Cold stays in the Arctic Cold air spills out of the Arctic Winter 2009-2010 Winter 2010-2011 Thanks to J. Overland, NOAA PMEL
  • 25. Whither Arctic Sea Ice? Using Sea Ice Data in the Classroom AccessData Earth Exploration Toolbook chapter http://serc.carleton.edu/eet/seaice/ Developed by: Walt Meier National Snow and Ice Data Center, Univ. Colorado Coop. Inst. for Research in Environmental Sciences Betsy Youngman Phoenix Country Day School Mark McCaffrey Coop. Inst. for Research in Environmental Sciences Anupma Prakash Geophysical Institute, University of Alaska Fairbanks Brian Rogan Boston Museum of Science
  • 26.
  • 27.
  • 28. Resources on Arctic climate NOAA Arctic Change, http://www.arctic.noaa.gov/
  • 29. SnowTweets Project R. Kelly, Univ. Waterloo, http://snowcore.uwaterloo.ca/snowtweets/
  • 30. NSIDC resources Atlas of the Cryosphere, http://nsidc.org/data/atlas/ WMS, OCG compliant web map server Several Arctic layers – sea ice snow, permafrost, snow, geographic locations http://nsidc.org/data/atlas/
  • 31.
  • 32.
  • 33.
  • 34.
  • 35.
  • 36.

Editor's Notes

  1. Shishmaref, on the far western shore of Alaska about 60 miles north of Nome. The permafrost that once reinforced Shishmaref’s waterfront is thawing. In earlier years, the sea was usually frozen during much of the stormy winter months. With warming, the wind-whipped ocean has eroded Shishmaref’s waterfront during many weeks when it once was frozen. The town’s residents have come to fear the full moon, with its unusually high tides.