1. Climate Change: Action at the Poles W. Richard Peltier Department of Physics University of Toronto

2. Current, 2010, atmospheric CO2 concentration is 389 ppmv, which is to be compared to the pre- industrial level of ~280 ppmv, an increase of ~38% over the past ~160 years That global warming would be caused by increasing CO2 levels was predicted by the Nobel chemist Arhenious~1840 An early “hockey stick” A Chance Correlation??

3. Outline Motivation: Warming is amplified at high northern hemisphere latitudes where its impacts should be felt first. What about the southern hemisphere? Motivation: Warming is amplified at high northern hemisphere latitudes where its impacts should be felt first. What about the southern hemisphere? Land ice-sheets as polar “canaries” Land ice-sheets as polar “canaries” The Gravity Recovery And Climate Experiment (GRACE) satellites The Gravity Recovery And Climate Experiment (GRACE) satellites Meltback of the Greenland and Antarctic Ice-Sheets according to GRACE Meltback of the Greenland and Antarctic Ice-Sheets according to GRACE The Topex-Poseidon and Jason-1 altimetric satellites; global sea level rise The Topex-Poseidon and Jason-1 altimetric satellites; global sea level rise Inter-hemispheric sea level “teleconnections” Inter-hemispheric sea level “teleconnections” The West Antarctic Ice-Sheet (WAIS): A 5 million year history of collapse and reformation The West Antarctic Ice-Sheet (WAIS): A 5 million year history of collapse and reformation Which is the “most to be feared” polar ice-sheet? Which is the “most to be feared” polar ice-sheet? Summary Summary

4. Warming since the onset of NH industrialization Latest GISS analysis

5. Surface warming by decade: the phenomenon of polar amplification Surface warming is Most extreme in high Northern latitudes but Also on the Antarctic Peninsula

6. Temperature anomaly for July 2010 Russian wild fires Warming on the peninsula

7. Continental Ice-Sheets and Glaciers in the Modern Climate System: Polar “Canaries” AntarcticaGreenland Alaska

8. The Gravity Recovery And Climate Experiment--GRACE GRACE employs a K-band microwave link to measure the distance between the COM’s of the two platforms (10 microns in distance accuracy) GRACE employs a K-band microwave link to measure the distance between the COM’s of the two platforms (10 microns in distance accuracy) It delivers a new gravity field for each month of operation It delivers a new gravity field for each month of operation The time dependence of this global field is therefore measured directly The time dependence of this global field is therefore measured directly This time dependence may be interpreted in terms of the loss or gain of surface mass associated with both past and ongoing changes in surface ice cover This time dependence may be interpreted in terms of the loss or gain of surface mass associated with both past and ongoing changes in surface ice cover Interpretation of modern rates of change of surface ice cover require correction for ice-age influence Interpretation of modern rates of change of surface ice cover require correction for ice-age influence Orbit Orbit Altitude 485 km Altitude 485 km Inclination 89 degrees Inclination 89 degrees Eccentricity ~0.001 Eccentricity ~0.001 non-repeat ground track non-repeat ground track earth pointed, three axis stable earth pointed, three axis stable bus separation ~220 km bus separation ~220 km

9. Comparison of GRACE with GIA: North America and Greenland Latest version of the Model Raw GRACE data Corrected for hydrology

10. Northern Hemisphere LGM Ice Cover Summer and Winter Sea ice ~21 ka Continental Ice Sheets CSM 1.4

11. Sea level Impacts of Northern Hemisphere Land-Ice Melting

12. Estimating mass loss and global sea level rise: Alaska and Greenland Corrected for hydrology Corrected for GIA ~.15 mm/yr in Global sea level rise ~.62 mm/yr in Global sea level rise

13. What abut the southern hemisphere? What is observed is unexpected!

14. Estimating mass loss and global sea level rise: Antarctica CSR GFZ GIA CSR-GIA GFZ-GIA ~.32 mm/yr in global sea level rise ~.36 mm/yr in Global sea level rise

15. Stability of the WAIS over the past million years From Pollard and DeConto, Nature 2009 Lisieki and Raymo oceanographic forcing

16. WAIS has oscillated in the past between a glaciated and a deglaciated state The Ross sea Sector

17. Rise of sea level due to collapse of the Greenland and/or West Antarctic Ice Sheet (WAIS) Total melt from Greenland is equivalent to 7.6 m of global sea level rise, from West Antarctica is 6.3 m of global sea level rise Predictions with the mean sea level subtracted to as to reveal spatial non-uniformity Note that the greatest rise of sea level occurs in the opposite hemisphere from that in which the melting occurs—a consequence of gravitational influence

18. Sea level rise impact at the locations of individual coastal cities, in Canada and elsewhere

19. The modern budget of global sea level rise

20. Topex/Poseidon Jason 1 Satellite Sea Level Altimetry 11

21. Global sea level rise since the onset of industrialization and the modern record from tide gauges, ocean hydrography and satellite altimetry (Topex/Poseidon-and Jason 1) Globally averaged sea level based upon both modern tide gauge recordings and other archives : Note the acceleration 12 Note: The current rate of sea level rise based upon satellite altimetry is ~ 2.8 mm/year

22. Is GRACE observing the gain of ocean mass associated with land-ice melting?

23. Rate of mass addition to the oceans-unfiltered Global rate of SLR due to the addition of mass to the oceans based upon raw GRACE data = -0.28 mm/yr +/- 0.21 mm/yr Implying that the oceans are actually losing mass!!!

24. Models of Glaciation History---ICE-5G NOTE: these figures are from the recent paper by Peltier and Fairbanks that appeared in the December 2006 issue of QSR (25, 3322-3337). The new Barbados RSL curve has also appeared in the Working Group 1 Report of the IPCC AR4

25. Holocene relative sea level histories

26. Solutions of the sea Level Equation: Present-day rate of change of sea level Including rotational feedback Excluding rotational feedback (a)-(b) (a) + dU/dt =dG/dt

27. However- the GIA correction for the rate of mass addition to the oceans is VERY large and negative Gaussianhalf-widthsCoefficientsexcluded Max. Degree and order Mass rate over the oceans- mm/yr dGeoid over Oceans- mm/yr No filter none120-1.80-0.30 400 Km none120-1.65-0.29 No filter (2,1) rot feedback120-1.32-0.26 400 Km (2,1)120-1.17-0.26

28. A Question of (Mass) Balance, 2002-2008 Mass loss from the continents Greenland+Alaska+Antarctica = ~1.05 mm/yr (Peltier, 2009, QSR) Small ice sheets and glaciers = ~0.95 mm/yr (Meier et al, 2007, Science) Continental drying = ~0.17 mm/yr (GLDAS) TOTAL = 2.17 mm/yr +/- 0.37 mm/yr Mass gain by the oceans Raw GRACE signal =~-0.28 mm/yr Correction due to spectral leakage =~-0.43 mm/yr Correction due to GIA (ICE-5G(VM2)) =~-1.80 mm/yr TOTAL = 1.95 mm/yr +/- 0.16 mm/yr It will be clear that mass balance is achieved only because of the magnitude of the GIA correction for the rate of gain of mass by the oceans

29. Ice Melting Rising Seas Rising Seas Massive Greenland and West Antarctic ice sheets are melting at accelerating rates Massive Greenland and West Antarctic ice sheets are melting at accelerating rates Together hold enough water to raise sea level 12 meters (39 feet) Together hold enough water to raise sea level 12 meters (39 feet) A 10 meter rise in sea level today would inundate coastal areas home to more than 600 million people A 10 meter rise in sea level today would inundate coastal areas home to more than 600 million people The risk is that climate change could spiral out of control, making it impossible to arrest trends such as rising temperatures, ice melting, and rising seas, threatening food security and creating hundreds of millions of climate refugees. Photo Credit: Yann Arthus-Bertrand

30. Summary The impacts of global warming are exacerbated at the poles: in the northern hemisphere due to the direct of air temperature; in the southern hemisphere due to ocean warming The impacts of global warming are exacerbated at the poles: in the northern hemisphere due to the direct of air temperature; in the southern hemisphere due to ocean warming Land ice melting in both hemispheres is making a significant contribution to global sea level rise Land ice melting in both hemispheres is making a significant contribution to global sea level rise The GRACE satellites are able to directly constrain the rate of loss of land ice in the major ice catchments but NOT for the smaller ice sheets and glaciers The GRACE satellites are able to directly constrain the rate of loss of land ice in the major ice catchments but NOT for the smaller ice sheets and glaciers Because of the “opposite hemisphere effect”, northern hemisphere communities would be most strongly impacted by a collapse of the WAIS Because of the “opposite hemisphere effect”, northern hemisphere communities would be most strongly impacted by a collapse of the WAIS