Variability of Extreme Temperature in the Arctic Observation and RCM

H. Matthes, A. Rinke, K. Dethloff
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引用次数: 9

Abstract

This paper discusses results of a simulation with the regional climate model HIRHAM for 1958-2001, driven by the ECMWF reanalysis (ERA40) data over the Arctic domain. The aim is to analyze the ability of the model to capture certain features of climate extremes derived from daily mean, maximum and minimum temperatures. For this purpose, a range of climate indices (frost days, cold and warm spell days, growing degree days and growing season length) was calculated from the model output as well as from ERA40 data and region-specific station data for Eastern and Western Russian Arctic for comparison. It is demonstrated that the model captures the main features in the spatial distribution and temporal development of most indices well. Though systematic deviations in the seasonal means occur in various indices (frost days, growing degree days), variability and trends are well reproduced. Seasonal mean patterns in frost days are reproduced best, though the model persistently calculates too many frost days. Seasonal means of cold and warm spell days are reproduced without systematic biases, though deviations occur in summer for cold spells and in spring and summer for warm spells due to an early spring warming in the regional climate model and a low variability of the daily maximum temperature over sea ice.
北极观测和RCM中极端温度的变率
本文讨论了区域气候模式HIRHAM 1958-2001年在ECMWF再分析(ERA40)数据驱动下对北极地区的模拟结果。目的是分析该模式捕捉由日平均、最高和最低温度得出的极端气候的某些特征的能力。为此,从模式输出以及ERA40数据和俄罗斯北极东部和西部的区域特定站数据中计算了一系列气候指数(霜冻日数、寒暖日数、生长期日数和生长期长度)以进行比较。结果表明,该模型较好地反映了大多数指数的空间分布和时间发展的主要特征。虽然不同指数(霜冻日数、生长期日数)的季节平均值存在系统偏差,但变异性和趋势得到了很好的再现。尽管该模式持续地计算了过多的霜冻日数,但霜冻日数的季节平均模式的再现效果最好。由于区域气候模式的早春变暖以及海冰上的日最高温度的低变率,冷期和暖期的季节平均值在夏季和春季和夏季会出现偏差,但再现冷期和暖期的季节平均值没有系统偏差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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