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Changes in Baltic Sea surface temperature extremes

机译:波罗的海地表极端温度的变化

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摘要

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.
机译:对于波罗的海的未来,出现极端海表温度(SST)的可能性似乎更加明显,因此其预测和推断至关重要。这项研究分析了波罗的海海表温度的平均变化,并使用21世纪的极值分布计算了返回期。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型的年度SST最大值。这些变化是根据20世纪(1971–2000年)的控制模拟进行估算的,并根据IPCC SRES A2排放情景对以下预计的2011-2040年,2041-2070年和2071-2099年进行了评估。在这种情况下,结果表明,温暖的极端天气(例如30年的返回值)比当前状况更频繁地出现,并且显示出不同的空间格局。此外,到21世纪末,波罗的海空间变异的强度将逐渐降低。

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