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The role of clouds in the continuing decline of the Arctic sea ice

The role of clouds in the continuing decline of the Arctic sea ice. Irina Gorodetskaya , Bruno Tremblay and B. Liepert. Thanks to: J. Francis, K. Stramler, R. Cullather. AWI, Potsdam, 29 January 2008. arctic. Sea ice concentrations. Sea ice MAXIMUM: March. Sea ice MINIMUM: September.

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The role of clouds in the continuing decline of the Arctic sea ice

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  1. The role of clouds in the continuing decline of the Arctic sea ice Irina Gorodetskaya, Bruno Tremblay and B. Liepert Thanks to: J. Francis, K. Stramler, R. Cullather AWI, Potsdam, 29 January 2008

  2. arctic

  3. Sea ice concentrations Sea ice MAXIMUM: March Sea ice MINIMUM: September Data: HadSST1

  4. Beaufort sea in winter Beaufort sea

  5. frost smoke in winter Frost smoke from a freshly opened lead in winter

  6. land fast ponding ice ponding

  7. September 2005 September 2006 September 2007 Data Source: National Snow and Ice Data Center (NSIDC), Boulder, Colorado, USA

  8. x 2007

  9. Arctic Energy Budget Figure by N. Untersteiner.

  10. Ice-Albedo feedback

  11. TOA albedo vs NH sea ice winter surface albedo for ice summer surface albedo for ocean RE (sfc alb) ~ 0.5 Radiative effectiveness of ice wrt TOA albedo: RE = albedo (100% ice conc) - albedo (0% ice conc) RE (TOA albedo) << RE (surface albedo) due to the presence of clouds over open oceans Gorodetskaya et al, Atm-Ocean 2006

  12. Maps of sea ice and snow RE NH sea ice SH sea ice NH snow Gorodetskaya et al, Atm-Ocean 2006

  13. Reflected SW: total and due to sea ice Gorodetskaya and Tremblay, 2008, for AGU monograph “Arctic sea ice decline:...”, Eds. DeWeaver, Bitz, Tremblay

  14. Summer: cloud forcing offsets sea ice effects on the surface shortwave radiation % estimated from Wang and Key, Science 2003

  15. Cloud cover over the Arctic Ocean: - Spring: large positive trend - Summer: no trend … Schweiger, GRL 2004

  16. Change (days) from 1979-88 to 1989-2001 in melt onset: in freeze onset: in melt duration: Belchansky et al. 2004

  17. Arctic Oscillation recovered and sea ice did not… Overland and Wang, GRL 2005

  18. Total variance in the perennial ice edge attributable to anomalies in forcing parameters, 1980-2004 J. A. Francis and E Hunter

  19. Seasonal cyclesover Canadian Arctic sector TOVS data

  20. SHEBA

  21. Arctic clouds contain liquid the entire year (based on Intrieri et al., JGR 2002; SHEBA data) LIQUID ~ 10 ICE ~ 0.2 (Zuidema et al. J Atm Sci 2005) Mean optical depth in May:

  22. Lidar depolarization ratios: phase detection6 May 1998 (Intrieri et al., JGR 2002; Beaufort and Chukchi Seas)

  23. Cloud phase and long-wave: SPRING->SUMMER April May June

  24. Daily radiative fluxes and albedo Gorodetskaya, Tremblay, Liepert, to be submitted to GRL

  25. Daily downwelling LW and sfc temperature Gorodetskaya, Tremblay, Liepert, to be submitted to GRL

  26. Zoom on the melt onset: Gorodetskaya, Tremblay, Liepert, to be submitted to GRL

  27. Cloud base temperature Winter March and early May April and mid May Summer late August-early September Gorodetskaya, Tremblay, Liepert, to be submitted to GRL

  28.  = 1 - exp(-oLWP) (Stephens, 1978) FLW =   Te4 Te=CBT CBT Downwelling longwave flux depending on liquid water path and cloud base temperature Gorodetskaya, Tremblay, Liepert, to be submitted to GRL

  29. Changes between seasonal modes

  30. Conclusions from SHEBA study • The timing of the melt onset is determined by the increase in downwelling • LW rather than decreased surface albedo • Major contribution to the increase in the downwelling LW flux comes • from the increase in the cloud base temperatures at the end of spring and • the fact that clouds contain large amount of liquid • Longer melt period in the Arctic Pacific sector in the beginning of the • 21st century compared to the 1980-s is similarly associated with larger • downwelling LW flux at the end of summer/early fall due to increased • cloudiness and warmer cloud temperatures

  31. Sea ice thickness from NCAR CCSM3 21st century run Absorbed SW and ocean heat transport Holland, Bitz, Tremblay, GRL 2006

  32. CCSM3: temperature, clouds, and radiative fluxes in the 21st century Gorodetskaya and Tremblay, 2008, for AGU monograph “Arctic sea ice decline:...”, Eds. DeWeaver, Bitz, Tremblay

  33. Atmospheric changesresponsible for increased downwelling LW Gorodetskaya and Tremblay, 2008, for AGU monograph “Arctic sea ice decline:...”, Eds. DeWeaver, Bitz, Tremblay

  34. albedo clouds Seasonal changesin radiative fluxes LW down SW down Gorodetskaya et al. 2008, J. Climate

  35. Arctic Energy Budget Figure by N. Untersteiner.

  36. Conclusions Clouds are thought to provide the “umbrella” protecting the Arctic Ocean surface from increased solar flux absorption due to the sea ice melting However... • Sea ice has a robust effect on planetary albedo • despite the mitigating effect of clouds • Clouds actively contribute to the present sea ice decline • by increasing downwelling longwave radiation • Increase in cloud SW cooling is limited by LWP • Future increase in atmospheric and thus cloud base temperatures will allow cloud LW warming to increase even more

  37. 1-layer sea ice thermodynamic model: ice thickness and concentration Forced with: CCSM3 radiation, atm T, ocean heat flux Predicts: Ts, Ti, h, SIC

  38. simulated ice thicknessfor standard and perturbed forcing

  39. simulated ice albedo

  40. ice concentration

  41. increased LW down smaller sea ice area increased SW and LW absorbed by the ocean increased ice bottom melt

  42. Conclusions • NCAR CCSM3 model predicts seasonally ice-free Arctic by 2100 together with more cloud formation, more liquid water in clouds, increased cloud LW warming and cloud SW cooling • Experiments with a sea ice thermodynamic model show that increased LW cloud forcing can explain nearly 40% of the sea ice thinning in the NCAR CCSM3 model during 21st century • Strong SW cloud cooling during summer compensates but does not cancel the effect of increased LW forcing • The ice albedo feedback is initiated by the increased LW flux, while the oceanic heat flux is fixed at 2000-2010 level

  43. Thus we should not rely on cloudsto prevent disappearance of the Arctic sea ice …

  44. Temperature profile within the ice

  45. SHEBA expedition:Surface Heat Budget of the Arctic OceanOctober 1997-October 1998

  46. Changes annual mean sea ice extent at the end of the 21st century Arzel, Fichefet, Goosse, Ocean Modelling 2006

  47. paleoclimate theories M. Milankovitch, 1941: variations of the astronomical elements and the reflective power of the polar caps => strong oscillations of summer insolation => glacial cycles M. Budyko, 1969: small variations of atmospheric transparency => quaternary glaciations H. Gildor and E. Tziperman, 2000: sea ice is off => glaciers grow; sea ice is on => glaciers withdraw Dansgaard et al, 1989, Alley et al. 1993, Broecker 2000, Denton et al. 2005: displacements of sea ice edge + rapid atmospheric circulation changes => Dansgaard-Oeschger events

  48. modern warming Holland and Bitz 2003: the ice-albedo feedback is one of the major factors accelerating melting of the Arctic sea ice in response to the increase in the globally averaged temperature Groisman et al, 1994:spring snow retreat => enhances spring air temperature increase Hall, 2002:surface albedo feedback accounts for ~1/2 the high-latitude response to CO2 doubling Winton, 2005:Surface albedo feedback is a contributing, but not a dominating, factor in the coupled-models simulated Arctic amplification => Sea ice and atmosphere work together in changing the surface and TOA net shortwave flux

  49. Sea level pressure TOVS data

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