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Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part?2: Antarctica (1979–2016)

机译:使用RACMO2对极地冰盖的气候和表面质量平衡进行建模–第2部分:南极洲(1979–2016)

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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 sup?1/sup , with an interannual variability of 109?Gt?y sup?1/sup . 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.
机译:我们根据区域大气气候模型RACMO2(1979-2016)的最新极地版本评估了建模的南极冰盖(AIS)近地表气候,地表质量平衡(SMB)和表面能平衡(SEB)。更新后的模型称为RACMO2.3p2,它结合了高空弛豫,修正的地形,云方案中的调整参数,可向AIS内部产生更多的降水,并具有改良的降雪性能,从而减少了飘雪升华和表面融雪的增加。 RACMO2模型输出与几个独立观测数据的比较表明,相对于先前的模型版本,AIS温度,辐射通量和SMB组件中的现有偏差得到了进一步降低。包括冰架(减去南极半岛,AP)的冰盖的模型集成年平均SMB现在为2229?Gt?y ?1 ,年际变化为109?Gt?y ?1 。在模拟的表面融雪中发现的最大改进,现在可以与卫星和气象站的观测结果很好地比较。对于高分辨率(约5.5?km)的AP模拟,结果仍可与早期研究相媲美。更新后的模型提供了有关现代近地表气候和AIS的SMB的新的高分辨率数据集;在即将进行的研究中,该模型版本将用于未来的气候情景预测。

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