Abstract

Abstract. We evaluate modelled Antarctic ice sheet (AIS) near-surface climate, surface mass balance (SMB) and surface energy balance (SEB) from the updated polar version of the regional atmospheric climate model, RACMO2 (1979–2016). The updated model, referred to as RACMO2.3p2, incorporates upper-air relaxation, a revised topography, tuned parameters in the cloud scheme to generate more precipitation towards the AIS interior and modified snow properties reducing drifting snow sublimation and increasing surface snowmelt. Comparisons of RACMO2 model output with several independent observational data show that the existing biases in AIS temperature, radiative fluxes and SMB components are further reduced with respect to the previous model version. The model-integrated annual average SMB for the ice sheet including ice shelves (minus the Antarctic Peninsula, AP) now amounts to 2229 Gt y−1, with an interannual variability of 109 Gt y−1. The largest improvement is found in modelled surface snowmelt, which now compares well with satellite and weather station observations. For the high-resolution (∼ 5.5 km) AP simulation, results remain comparable to earlier studies. The updated model provides a new, high-resolution data set of the contemporary near-surface climate and SMB of the AIS; this model version will be used for future climate scenario projections in a forthcoming study.

Highlights

  • Before being able to accurately predict future changes in the climate and surface mass balance (SMB) of the Antarctic ice sheet (AIS), it is required that its contemporary climate and SMB are realistically modelled

  • In this study we evaluated the modelled Antarctic ice sheet (AIS) climate, surface mass balance (SMB) and surface energy balance (SEB) in RACMO2.3p2, the latest polar version of the regional atmospheric climate model RACMO2 (1979–2016)

  • This model version is applied at 27 km horizontal resolution to the full AIS and at 5.5 km resolution to the Antarctic Peninsula (AP)

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Summary

Introduction

Before being able to accurately predict future changes in the climate and surface mass balance (SMB) of the Antarctic ice sheet (AIS), it is required that its contemporary climate and SMB are realistically modelled. Biases in SMB and SEB are caused by too-thin clouds simulated over the AIS, resulting in too little snowfall, too much downwelling shortwave radiation and too little downwelling longwave radiation (Van Wessem et al, 2014a; King et al, 2015). These biases are potentially related to an unrealistic fractionation of ice and water content in these clouds, which significantly affects the sensitivity of the (cloud) radiative fluxes to changes in cloud content (King et al, 2015). This paper is part of a tandem model evaluation over the Greenland (part 1) and Antarctic (this study) ice sheets

The Regional Atmospheric Climate Model RACMO2
Surface energy budget and surface mass balance
Model updates
10 Filchner
Initialisation and set-up
Observational data
Automatic weather stations
In situ SMB and temperature observations
Accumulation radar
Drifting snow in Adélie Land
QuikSCAT melt fluxes
CloudSat–CALIPSO
Upper-air profiles
Discharge estimates
Changes in modelled SEB
Changes in modelled SMB
Changes in integrated SMB
Kohnen Station radiosondes
In situ observations
Snow accumulation radar
Drifting snow transport
Surface melt
Changes in modelled SMB and SEB
Clouds
Summary and conclusions
Full Text
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