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A new, high-resolution surface mass balance map of Antarctica (1979-2010) based on regional atmospheric climate modeling

机译:基于区域大气气候模型的新的高分辨率南极洲表面质量平衡图(1979-2010年)

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摘要

A new, high resolution (27 km) surface mass balance (SMB) map of the Antarctic ice sheet is presented, based on output of a regional atmospheric climate model that includes snowdrift physics and is forced by the most recent reanalysis data from the European Centre for Medium-Range Weather Forecasts (ECMWF), ERA-Interim (1979-2010). The SMB map confirms high accumulation zones in the western Antarctic Peninsula (>1500 mm y ~(-1)) and coastal West Antarctica (>1000 mm y ~(-1)), and shows low SMB values in large parts of the interior ice sheet (<25 mm y ~(-1)). The location and extent of ablation areas are modeled realistically. The modeled SMB is in good agreement with ±750 in-situ SMB measurements (R = 0.88), without a need for post-calibration. The average ice sheet-integrated SMB (including ice shelves) is estimated at 2418 ± 181 Gt y ~(-1). Snowfall shows modest interannual variability (σ = 114 Gt y ~(-1)), but a pronounced seasonal cycle (σ = 30 Gt mo ~(-1)), with a winter maximum. The main ablation process is drifting snow sublimation, which also peaks in winter but with little interannual variability (σ = 9 Gt y ~(-1)).
机译:根据区域大气气候模型的输出(包括随风飘移的物理现象),并根据欧洲中心的最新再分析数据,得出了南极冰盖的新的高分辨率(27公里)表面质量平衡(SMB)地图ERA-Interim(1979-2010)中距离天气预报(ECMWF)。 SMB图确认了南极半岛西部(> 1500 mm y〜(-1))和南极西部沿海地区(> 1000 mm y〜(-1))的高堆积带,并在内部大部分区域显示了较低的SMB值冰盖(<25毫米y〜(-1))。消融区域的位置和范围是实际建模的。建模的SMB与±750原位SMB测量(R = 0.88)非常吻合,无需进行后校准。冰盖整合的SMB(包括冰架)的平均估计值为2418±181 Gt y〜(-1)。降雪显示出适度的年际变化(σ= 114 Gt y〜(-1)),但有明显的季节性周期(σ= 30 Gt mo〜(-1)),且冬季最大。主要的消融过程是漂移雪升华,它在冬天也达到顶峰,但年际变化很小(σ= 9 Gt y〜(-1))。

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