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Summertime inter-annual temperature variability in an ensemble of regional model simulations: analysis of the surface energy budget.

机译:区域模型模拟中的夏季年际温度变化:对表面能收支的分析。

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The inter-annual variability in monthly mean summer temperatures derived from nine different regional climate model (RCM) integrations is investigated for both the control climate (1961-1990) and a future climate (2071-2100) based on A2 emissions. All regional model integrations, carried out in the PRUDENCE project, use the same boundaries of the HadAM3H global atmospheric model. Compared to the CRU TS 2.0 observational data set most RCMs (but not all) overpredict the temperature variability significantly in their control simulation. The behaviour of the different regional climate models is analysed in terms of the surface energy budget, and the contributions of the different terms in the surface energy budget to the temperature variability are estimated. This analysis shows a clear relation in the model ensemble between temperature variability and the combined effects of downward long wave, net short wave radiation and evaporation (defined as F). However, it appears that the overestimation of the temperature variability has no unique cause. The effect of short-wave radiation dominates in some RCMs, whereas in others the effect of evaporation dominates. In all models the temperature variability and F increase when imposing future climate boundary conditions, with particularly high values in central Europe..
机译:根据A2排放量,对控制气候(1961-1990)和未来气候(2071-2100)都研究了从九种不同的区域气候模型(RCM)积分得出的夏季平均每月温度的年际变化。在PRUDENCE项目中进行的所有区域模型集成都使用HadAM3H全球大气模型的相同边界。与CRU TS 2.0观测数据集相比,大多数RCM(但不是全部)在其控制仿真中会过高地预测温度变化。根据地表能量预算分析了不同区域气候模型的行为,并估算了地表能量预算中不同术语对温度变化的贡献。该分析表明,模型集合中温度变化与向下长波,净短波辐射和蒸发(定义为F)的综合影响之间存在明确的关系。但是,似乎高估了温度变化并没有唯一的原因。在某些RCM中,短波辐射的影响起主要作用,而在另一些RCM中,蒸发的作用起主要作用。在所有模型中,当施加未来的气候边界条件时,温度变异性和F都会增加,在中欧特别高。

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