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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmospheric climate model
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Reassessment of the Antarctic surface mass balance using calibrated output of a regional atmospheric climate model

机译:使用区域大气气候模型的校准输出重新评估南极表面质量平衡

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摘要

A detailed comparison of model-simulated and observed Antarctic surface mass balance (SMB) is presented, using output of a regional atmospheric climate model (RACMO2/ANT) for the period 1980 to 2004. All available SMB observations from Antarctica (N = 1900) are used for the comparison, except clearly erroneous observations and data which are in areas where dominant SMB patterns occur on scales smaller than the model resolution. A high correlation is found (r = 0.82), while the regression slope (1.2) indicates that the model slightly overemphasizes SMB gradients. Comparing the model SMB with the latest SMB compilation, a similarly high correlation is found (r = 0.79), but the regression slope is much too steep because model-simulated SMB agrees less with the compilation in data-sparse regions. Model-simulated SMB resembles the observed SMB as a function of elevation very well. This is used to calibrate model-simulated SMB to reassess the contemporary Antarctic SMB. Compared to the latest SMB compilation, calibrated model-simulated SMB is up to 1 m yr~-1 higher in the coastal zones of East and West Antarctica, which are without exception in areas with few observations. As a result, the SMB integrated over the grounded ice sheet (171 ± 3 mm yr~-1) exceeds previous estimates by as much as 15%. Support or falsification of this model result can only be found in new SMB observations from high accumulation regions.
机译:使用1980年至2004年期间的区域大气气候模型(RACMO2 / ANT)的输出,对模型模拟和观测的南极表面质量平衡(SMB)进行了详细的比较。所有南极洲可用的SMB观测(N = 1900)除了明显错误的观测值和数据位于主要SMB模式以小于模型分辨率的尺度发生的区域外,这些值用于比较。发现高度相关(r = 0.82),而回归斜率(1.2)表明该模型稍微过分强调了SMB梯度。将模型SMB与最新的SMB编译进行比较,发现具有相似的高相关性(r = 0.79),但是回归斜率过于陡峭,因为模型仿真的SMB与数据稀疏区域中的编译不太一致。模型模拟的SMB非常类似于观察到的SMB,它是海拔的函数。这用于校准模型仿真的SMB,以重新评估当代的南极SMB。与最新的SMB汇编相比,经过校准的模型模拟SMB在南极东部和西部的沿海地区要高出1 m yr〜-1,而在观测很少的地区也不例外。结果,集成在接地冰原上的SMB(171±3 mm yr〜-1)比以前的估计高出15%。该模型结果的支持或伪造只能在来自高聚积地区的新的SMB观测中找到。

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