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Climate change impacts on wind speeds and wind energy density in northern Europe: empirical downscaling of multiple AOGCMs

机译:气候变化对北欧的风速和风能密度的影响:多个AOGCM的经验缩减

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ABSTRACT: We present empirical downscaling of 5 state-of-the-art AOGCMs (Atmosphere-Ocean General Circulation Models) to investigate potential changes in wind speeds and energy density in northern Europe. The approach is based on downscaling the Weibull parameters of wind speed probability distributions from AOGCM-derived 500 hPa relative vorticity and sea-level pressure gradients, and is demonstrated to generate accurate depictions of the wind climate during the transfer function conditioning period. Bootstrapping is used to develop 100 realizations for each downscaling period and these are used to assess the uncertainty in the results due to stochastic effects in the AOGCM-derived downscaling predictors. Projected changes in the wind speed probability distribution vary with the AOGCMs from which the predictors are derived, but generally it is shown that mean wind speeds, 90th percentile wind speeds and energy density are slightly lower in the 2081–2100 climate projection period than during 1961–1990 at the majority of the 46 stations studied. Conversely it is found that there is no significant difference between conditions during 2046–2065 and 1961–1990 based on the ensemble of downscaling results. Equally, the winter time of 2046–2065 is largely indistinguishable from 1961–1990 for the majority of stations, while the winters of 2081–2100 appear to be associated with lower mean and 90th percentile wind speeds and energy density.
机译:摘要:我们提出了5种最先进的AOGCM(大气-海洋总循环模型)的经验降尺度,以研究北欧风速和能量密度的潜在变化。该方法基于根据AOGCM得出的500 hPa相对涡度和海平面压力梯度缩小风速概率分布的Weibull参数,并被证明可以在传递函数调节期间生成准确的风气候描述。自举用于每个降尺度周期开发100个实现,并且用于评估AOGCM降尺度预测器中的随机效应导致的结果不确定性。风速概率分布的预计变化随预测变量所基于的AOGCM的不同而不同,但通常表明,在2081–2100年的气候预测期内,平均风速,第90个百分位风速和能量密度比1961年略低–1990年研究的46个台站中的大多数。相反,基于缩小结果的集合,发现2046-2065年和1961-1990年之间的条件之间没有显着差异。同样,对于大多数站来说,2046-2065年的冬季时间与1961-1990年的时间基本没有区别,而2081-2100年的冬季似乎与较低的平均风速和90%的风速和能量密度有关。

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