Simulated Antarctic precipitation and surface mass balance at the end of the twentieth and twenty-first centuries

• Published in: Climate dynamics Vol. 28; no. 2-3; pp. 215 - 230
• Main Authors: KRINNER, G, MAGAND, O, SIMMONDS, I, GENTHON, C, DUFRESNE, J.-L
• Format: Journal Article
• Language: English
• Published: Heidelberg Springer 01.02.2007; Berlin Springer Nature B.V
• Subjects: Atmospheric circulation; Climatology. Bioclimatology. Climate change; Earth, ocean, space; Exact sciences and technology; External geophysics; Marine; Meteorology; Oceanography; Sea level; Snow. Ice. Glaciers; Snowmelt; Antarctica; PS, Antarctica; Century 21st; mass balance; Atmosphere model; General circulation models; atmospheric precipitation; Atmosphere cryosphere interaction; Climate models; Forecast model; Dynamical climatology; Century 20th; Polar Cap; ice sheets; climate modification; global change; sea ice; warming; polar regions; ice caps; Polar region; Forcing; sea level
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-006-0177-x

The aim of this work is to assess potential future Antarctic surface mass balance changes, the underlying mechanisms, and the impact of these changes on global sea level. To this end, this paper presents simulations of the Antarctic climate for the end of the twentieth and twenty-first centuries. The simulations were carried out with a stretched-grid atmospheric general circulation model, allowing for high horizontal resolution (60 km) over Antarctica. It is found that the simulated present-day surface mass balance is skilful on continental scales. Errors on regional scales are moderate when observed sea surface conditions are used; more significant regional biases appear when sea surface conditions from a coupled model run are prescribed. The simulated Antarctic surface mass balance increases by 32 mm water equivalent per year in the next century, corresponding to a sea level decrease of 1.2 mm year^sup -1^ by the end of the twenty-first century. This surface mass balance increase is largely due to precipitation changes, while changes in snow melt and turbulent latent surface fluxes are weak. The temperature increase leads to an increased moisture transport towards the interior of the continent because of the higher moisture holding capacity of warmer air, but changes in atmospheric dynamics, in particular off the Antarctic coast, regionally modulate this signal.[PUBLICATION ABSTRACT]