波罗的海表面极端温度的变化

B. W. An, J. Haapala
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引用次数: 2

摘要

未来波罗的海发生极端海表温度(SST)的可能性似乎更加明显,因此其预测和推断是必不可少的。本研究分析了波罗的海海温的平均变化,并利用21世纪的极值分布计算了回归期。为了说明极值理论的应用,分析了基于NEMO-LIM3[1]的波罗的海区域气候模式的年海温最大值。这些变化是根据20世纪(1971-2000年)的控制模拟估算的,并在IPCC SRES A2排放情景的强迫下对2011-2040、2041-2070和2071-2099预估期进行了评估。结果表明,在此情景下,极端暖事件(如30年回复值)的发生频率将高于当前情景,且呈现不同的空间格局。此外,到21世纪末,波罗的海的空间变率强度将逐渐减弱。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in Baltic Sea surface temperature extremes
The probability of extreme sea surface temperature (SST) occurring seems more apparent for future in the Baltic Sea therefore its prediction and inferences are essential. This study analyzed the mean change of the SST in the Baltic Sea and calculated return periods using extreme value distributions of the 21st century. To illustrate the application of extreme value theory, annual SST maxima from the Baltic Sea regional climate model based on NEMO-LIM3 [1] were analyzed. The changes were estimated from the control simulation of the 20th century (1971-2000) and were assessed for the following projected periods 2011-2040, 2041-2070, and 2071-2099 forced by the IPCC SRES A2 emission scenario. Under that scenario, results indicate that the warm extremes (e.g. 30-year return values) will occur more frequently than those of the current condition and also show different spatial patterns. In addition, the strength of the spatial variability in the Baltic Sea will be reduced gradually towards the end of the 21st century.
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