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Large-Scale Surface Mass Balance of Ice Sheets from a Comprehensive Atmospheric Model

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Abstract

The surface mass balance for Greenland and Antarctica has been calculated using model data from an AMIP-type experiment for the period 1979–2001 using the ECHAM5 spectral transform model at different triangular truncations. There is a significant reduction in the calculated ablation for the highest model resolution, T319 with an equivalent grid distance of ca 40 km. As a consequence the T319 model has a positive surface mass balance for both ice sheets during the period. For Greenland, the models at lower resolution, T106 and T63, on the other hand, have a much stronger ablation leading to a negative surface mass balance. Calculations have also been undertaken for a climate change experiment using the IPCC scenario A1B, with a T213 resolution (corresponding to a grid distance of some 60 km) and comparing two 30-year periods from the end of the twentieth century and the end of the twenty-first century, respectively. For Greenland there is change of 495 km3/year, going from a positive to a negative surface mass balance corresponding to a sea level rise of 1.4 mm/year. For Antarctica there is an increase in the positive surface mass balance of 285 km3/year corresponding to a sea level fall by 0.8 mm/year. The surface mass balance changes of the two ice sheets lead to a sea level rise of 7 cm at the end of this century compared to end of the twentieth century. Other possible mass losses such as due to changes in the calving of icebergs are not considered. It appears that such changes must increase significantly, and several times more than the surface mass balance changes, if the ice sheets are to make a major contribution to sea level rise this century. The model calculations indicate large inter-annual variations in all relevant parameters making it impossible to identify robust trends from the examined periods at the end of the twentieth century. The calculated inter-annual variations are similar in magnitude to observations. The 30-year trend in SMB at the end of the twenty-first century is significant. The increase in precipitation on the ice sheets follows closely the Clausius-Clapeyron relation and is the main reason for the increase in the surface mass balance of Antarctica. On Greenland precipitation in the form of snow is gradually starting to decrease and cannot compensate for the increase in ablation. Another factor is the proportionally higher temperature increase on Greenland leading to a larger ablation. It follows that a modest increase in temperature will not be sufficient to compensate for the increase in accumulation, but this will change when temperature increases go beyond any critical limit. Calculations show that such a limit for Greenland might well be passed during this century. For Antarctica this will take much longer and probably well into following centuries.

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References

  • Allerup P, Madsen H, Vejen F (2000) Correction of precipitation based on off-site weather information. Atmos Res 53(4):231–250

    Article  Google Scholar 

  • AMIP Project Office (1996) AMIP II Guidelines, AMIP newsletter, No. 8. Available online at http://www-pcmdi.llnl.gov/projects/amip/NEWS/amipnl8.php#2.%20AMIP%20II%20Experimental

  • Bengtsson L, Hodges KI, Roeckner E (2006) Storm tracks and climate change. J Climate 19(15):3518–3543

    Article  Google Scholar 

  • Bengtsson L, Hodges KI, Esch M, Keenlyside N, Kornblueh L, Luo J, Yamagata T (2007a) How may tropical cyclones change in a warmer climate? Tellus 59(4):539–561

    Article  Google Scholar 

  • Bengtsson L et al (2007b) The need for a dynamical climate reanalysis. Bull Amer Meteor Soc 88:495–501

    Article  Google Scholar 

  • Bengtsson L, Hodges KI, Keenlyside N (2009) Will extra-tropical storms intensify in a warmer climate? J Climate 2276–2301:2009

    Google Scholar 

  • Bengtsson L, Hodges KI, Koumoutsaris S, Zahn M, Keenlyside N (2011) On the atmospheric water balance of the Polar Regions. Tellus, under review

  • Box JE, Bromwich DH, Veenhuis BA, Bai LS, Stroeve JC, Rogers JC, Steffen K, Haran T, Wang SH (2006) Greenland ice sheet surface mass balance variability (1988–2004) from calibrated Polar MM5 output. J Climate 19(12):2783–2800

    Article  Google Scholar 

  • Box JE, Yang L, Bromwich D, Bai L-S (2009) Greenland ice sheet surface air temperature variability: 1840–2007. J Climate 22(14):4029

    Article  Google Scholar 

  • Bromwich DH, Guo Z, Bai L, Chen Q-S (2004) Modeled Antarctic precipitation. Part I: spatial and temporal variability. J Climate 17:427–447

    Article  Google Scholar 

  • De Angelis H, Skvarca P (2003) Glacier surge after ice shelf collapse. Science 299(5612):1560–1562

    Article  Google Scholar 

  • Dee DP, Uppala S (2009) Variational bias correction of satellite radiance data in the era-interim reanalysis. Q J R Meteorol Soc 135(644):1830–1841

    Article  Google Scholar 

  • DiMarzio J, Brenner A, Schutz R, Shuman CA, Zwally HJ (2007) GLAS/ICESat 1 km laser altimetry digital elevation model of Greenland. National Snow and Ice Data Center. Digital media, Boulder, Colorado

    Google Scholar 

  • Fettweis X (2007) Reconstruction of the 1979–2006 Greenland ice sheet surface mass balance using the regional climate model MAR. Cryosphere 1(1):21–40

    Article  Google Scholar 

  • Gregory JM, Huybrechts P (2006) Ice-sheet contributions to future sea-level change. Philos Trans R Soc A-Math Phys Eng Sci 364(1844):1709–1731

    Article  Google Scholar 

  • Groisman PY, Peck EL, Quayle RG (1999) Intercomparison of recording and standard nonrecording US Gauges. J Atm Ocean Tech 16(5):602–609

    Article  Google Scholar 

  • Hagemann S, Arpe K, Roeckner E (2006) Evaluation of the hydrological cycle in the ECHAM5 model. J Climate 19(16):3810–3827

    Article  Google Scholar 

  • Hanna E, Huybrechts P, Steffen K, Cappelen J, Huff R, Shuman C, Irvine-Fynn T, Wise S, Griffiths M (2008) Increased runoff from melt from the Greenland ice sheet: a response to global warming. J Climate 21(2):331–341

    Article  Google Scholar 

  • Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Climate 19(21):5686–5699

    Article  Google Scholar 

  • Huybrechts P, Goelzer H, Janssens I, Driesschaert E, Fichefet T, Goosse H, Loutre M-F (2011) Response of the Greenland and Antarctic ice sheets to multi-millennial greenhouse warming in the Earth system model of intermediate complexity LOVECLIM. Surv Geophys (this issue)

  • Intergovernmental Panel on Climate Change (IPCC) (2007) Climate change 2007: the scientific basis. Cambridge University Press, Cambridge

    Google Scholar 

  • Jakobson E, Vihma T (2009) Atmospheric moisture budget in the Arctic based on the ERA-40 reanalysis Int J Climatol. doi:10.1002/joc.2039

  • Johannessen OM, Khvorostovsky K, Miles MW, Bobylev LP (2005) Recent ice-sheet growth in the interior of Greenland. Science 310(5750):1013–1016

    Article  Google Scholar 

  • Krinner G, Magand O, Simmonds I, Genthon C, Dufrense J-L (2007) Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries. Clim Dyn 28:215–230. doi:10.1007/s00382-006-0177-x

    Article  Google Scholar 

  • Lemke P, Ren J, Alley RB, Allison I, Carrasco J, Flato G, Fujii Y, Kaser G, Mote P, Thomas RH, Zhang T (2007) Observations: changes in snow, ice and frozen ground. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate change 2007: the physical science basis. Contribution of Working Group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge, UK and New York

    Google Scholar 

  • Mernild SH, Liston GE, Hiemstra CA, Steffen K, Hanna E, Christensen JH (2009) Greenland ice sheet surface mass-balance modelling and freshwater flux for 2007, and in a 1995–2007 perspective. Hydrol Process 23(17):2470–2484

    Article  Google Scholar 

  • Mernild SH, Liston GE, Hiemstra CA, Christensen JH (2010) Greenland ice sheet surface mass-balance modeling in a 131-yr perspective, 1950–2080. J Hydrometeorol 11(1):3–25

    Article  Google Scholar 

  • Mote TL (2007) Greenland surface melt trends 1973–2007: evidence of a large increase in 2007, Geophys Res Lett 34. doi:10.1029/2007GL031976

  • Oerlemans J (1990) A model for the surface balance of glaciers. Part 1: Alpine glaciers. Z Gletscherk Glazialgeol 27:63–83

    Google Scholar 

  • Ohmura A (2001) Physical basis for the temperature-based melt-index method. J Appl Meteorol 40(4):753–761

    Article  Google Scholar 

  • Ohmura A (2006) Changes in mountain glaciers and ice caps during the twentieth century. Ann Glaciol 43:361–368

    Article  Google Scholar 

  • Ohmura A, Wild M, Bengtsson L (1996) A possible change in mass balance of Greenland and antarctic ice sheets in the coming century. J Climate 9(9):2124–2135

    Article  Google Scholar 

  • Ohmura A, Calanca P, Wild M, Anklin M (1999) Precipitation, accumulation and mass balance of Greenland ice sheet (1999). Z Gletscherk Glazialgeol 35:1–20

    Google Scholar 

  • Pierrehumbert RT, Brogniez H, Roca R (2007) On the relative humidity of the Earth’s atmosphere. In: Schneider T, Sobel AH (eds) The global circulation of the atmosphere. Princeton University Press, Princeton, NJ, pp 143–185

    Google Scholar 

  • Ridley JK, Huybrechts P, Gregory JM, Lowe JA (2005) Elimination of the Greenland ice sheet in a high CO2 climate. J Climate 18(17):3409–3427

    Article  Google Scholar 

  • Roeckner E, Bauml G, Bonaventura L, Brokopf R, Esch M, Giorgetta M, Hagemann S, Kirchner I, Kornblueh L, Manzini E, Rhodin A, Schlese U, Schulzweida U, Tompkins A (2003) The atmospheric general circulation model ECHM5: Part 1, Tech Rep 349, Max Planck Institute for Meteorology, Hamburg

  • Roeckner E, Stier P, Feichter J, Kloster S, Esch M, Fischer-Bruns I (2006) Im-pact of carbonaceous aerosol emissions on regional climate change. Clim Dyn 27(6):553–571

    Article  Google Scholar 

  • Serreze MC, Barrett AP, Slater AG, Woodgate RA, Aagaard K, Lammers RB, Steele M, Moritz R, Meredith M, Lee CM (2006) The large-scale freshwater cycle of the arctic. J Geophys Res-Oceans 111(C11). doi:10.1029/2005JC003424

  • Tedesco M (2007) Snowmelt detection over the Greenland ice sheet from SSM/I brightness temperature daily variations. Geophys Res Lett 34. doi:10.1029/2006GL028466

  • Wild M, Calanca P, Scherrer SC, Ohmura A (2003) Effects of polar ice sheets on global sea level in high-resolution greenhouse scenarios. J Geophys Res-Atmos 108(D5). doi:10.1029/2002JD002451

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Acknowledgments

The authors are most grateful to Noel Keenlyside of the Leibniz Institute of Marine Sciences at Kiel University for providing the ECHAM5 C20 and C21 climate simulation data.

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Correspondence to Lennart Bengtsson.

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Bengtsson, L., Koumoutsaris, S. & Hodges, K. Large-Scale Surface Mass Balance of Ice Sheets from a Comprehensive Atmospheric Model. Surv Geophys 32, 459–474 (2011). https://doi.org/10.1007/s10712-011-9120-8

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