Abstract

On average, the models in the Fifth Climate Model Intercomparison Project archive predict an increase in Antarctic precipitation from 5.5 to 24.5 % between 1986–2005 and 2080–2099, depending on greenhouse gas emissions scenarios. This translates into a moderation of future sea level rise ranging from −19 to −71 mm between 2006 and 2099. However, comparison with CloudSat and ERA-Interim data show that almost all the models overestimate current Antarctic precipitation, some by more than 100 %. If only the models that agree with CloudSat data within 20 % of error are considered, larger precipitation changes (from 7.4 to 29.3 %) and impact on sea level (from −25 to −85 mm) are predicted. A common practice of averaging all models to evaluate climate projections thus leads to a significant underestimation of the contribution of Antarctic precipitation to future sea level. Models simulate, on average, a 7.4 %/°C precipitation change with surface temperature warming. The models in better agreement with CloudSat observations for Antarctic snowfall predict, on average, larger temperature and Antarctic sea ice cover changes, which could explain the larger changes in Antarctic precipitation simulated by these models. The agreement between the models, CloudSat data and ERA-Interim is generally less in the interior of Antarctica than at the peripheries, but the interior is also where climate change will induce the smallest absolute change in precipitation. About three-quarters of the impact on sea level will result from precipitation change over the half most peripheral and lowest elevation part of the surface of Antarctica.

Highlights

  • Predicting the evolution of the Antarctic ice sheet is a major challenge with relevance to sea level rise

  • Climate models participating in the Coupled Model Intercomparison Project Phase 5 (CMIP5) consistently predict Antarctic precipitation to increase in a warming climate (Church et al 2013)

  • These 5 CMIP5 models are representative of the range of models in the Historical scenario (Table 1)

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Summary

Introduction

Predicting the evolution of the Antarctic ice sheet is a major challenge with relevance to sea level rise. Climate models participating in the Coupled Model Intercomparison Project Phase 5 (CMIP5) consistently predict Antarctic precipitation to increase in a warming climate (Church et al 2013) Due to this change in precipitation, snow accumulation (the sum of precipitation, sublimation/evaporation, meltwater run-off, and blowing snow) should increase in Antarctica (Church et al 2013). The ability of CMIP5 climate models to reproduce present-day Antarctic snowfall is assessed against this new satellite climatology. After this model assessment, an intercomparison and analysis of CMIP5 model projections for the twenty-first century is presented. The sensitivities of Antarctic precipitation to near-surface air temperature and sea ice area changes are investigated

Data and methods
Mean annual snowfall rate
Seasonal variability
Trends in Antarctic precipitation during the period 1956–2005
Precipitation changes and consequences on sea level
Precipitation and temperature changes
Precipitation and sea ice cover changes
Discussion and conclusions
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