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Lapse Rate Peculiarities in the Arctic from Reanalysis Data and Model Simulations

机译:从再分析数据和模型模拟得出北极的流失率特征

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Monthly mean data of the ERA-Interim reanalysis (1979-2014) are used to estimate the lapse rate in the Northern Hemisphere high-latitude troposphere. The relationship between the lapse rate and surface air temperature T-s is analyzed in terms of interannual variability for different seasons. The study analyzes the ability of the HIRHAM5 regional climate model to simulate the features of lapse rate distribution in the Arctic troposphere and the parameter of its sensitivity to the variation in surface air temperature d/dT(s) that were derived from reanalysis data. The regional features of the link between the vertical stratification of tropospheric temperature and the Arctic Oscillation are revealed. The estimates obtained from reanalysis data and model simulations are especially significant as the Arctic climate has higher variability and sensitivity under global changes that is characterized by so called Arctic amplification.
机译:ERA-临时分析的每月平均数据(1979-2014年)用于估算北半球高纬对流层的消失率。根据不同季节的年际变化分析了流失率与地面气温T-s之间的关系。这项研究分析了HIRHAM5区域气候模型模拟北极对流层流逝速率分布特征的能力,以及对重新分析数据得出的其对地面气温d / dT(s)的敏感性参数。揭示了对流层温度的垂直分层与北极涛动之间联系的区域特征。从再分析数据和模型模拟获得的估计值尤其重要,因为在以所谓的北极放大为特征的全球变化下,北极气候具有更高的变异性和敏感性。

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