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Applying the Energy- and Water Balance Model for Incorporation of the Cryospheric Component into a Climate Model. Part Ⅲ. Modeling Mass Balance on the Surface of the Antarctic Ice Sheet

机译:应用能量和水平衡模型将低温组分掺入气候模型中。第三部分。南极冰盖表面上的质量平衡

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摘要

The Earth system models have been actively developed during recent decades. They integrate the blocks describing the dynamics of the atmosphere, the ocean and the cryosphere. The Antarctic ice sheet (AIS) is one of the most important components of the Earth's cryosphere. Therefore, the incorporation of the AIS model into the Earth system model will significantly improve the accuracy of reconstructions of climate parameters for paleoclimate studies and for climate predictions. This paper presents a description of the energy balance block of the AIS model. This is a continuation of our recent work on integration of the cryosphere block to the climate model. The testing of the block (the EWBM-A buffer model) was carried out using the climate data generated by the INMCM model developed in the Institute of Numerical Mathematics of RAS. The results of the calculations of the surface mass balance components of the Antarctic ice sheet are presented for the 30-year pre-industrial period and are compared with the recent results obtained in the literature.
机译:近几十年来,地球系统模型已经积极开发。它们整合了描述大气,海洋和冰屋动态的块。南极冰盖(AIS)是地球冰屋最重要的组成部分之一。因此,将AIS模型纳入地球系统模型将显着提高气候参数重建的准确性,用于古古典研究和气候预测。本文介绍了AIS模型的能量平衡块的描述。这是我们最近关于将冷冻圈块整合到气候模型的工作的延续。使用在RAS的数学数学研究所开发的INMCM模型产生的气候数据进行块(EWBM-A缓冲模型)的测试。南极冰盖的表面质量平衡组分的计算结果介绍了30年前工业期间,并与文献中获得的最近结果进行比较。

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