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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Changes in European drought characteristics projected by the PRUDENCE regional climate models
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Changes in European drought characteristics projected by the PRUDENCE regional climate models

机译:PRUDENCE区域气候模型预测的欧洲干旱特征变化

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One of the key features of global climate change will be perturbations to the hydrological regime across Europe. To date, assessments of the impacts of future change have generally used results from only one climate model, thus underestimating the range of possible change projected by different climate models. Here, the skill of six regional climate models (RCMs) in reproducing the mean precipitation for the 1961 - 1990 period for six catchments across Europe is compared and their projections of changes in future precipitation are assessed. A simple drought index based on monthly precipitation anomalies is also described and used to assess the models. Considerable variation in model skill in reproducing monthly mean precipitation and drought statistics is observed, with model errors in the reproduction of drought events independent of those for the mean, suggesting that the models have difficulties in reproducing the observed persistence of low monthly rainfall totals. In broad terms, the models indicate decreases in summer and increases in winter precipitation across Europe. On the regional scales required for impacts analysis, considerable model uncertainty is demonstrated for future projections, particularly for drought frequency. Although increases in the frequency of long-duration droughts are identified for catchments in southern Europe, the magnitude of this change is not certain. In contrast, for a catchment in northern England, such events are likely to become less frequent. For shorter-duration droughts, future changes encompass the direction of change. For stakeholders in each of the regions, these changes and uncertainties pose different challenges for the management of water resources. For the scientific community, the challenge raised is how to incorporate this uncertainty in climate change projections in a way that allows those groups to make informed decisions based on model projections. It is suggested that probabilistic scenarios for specific hydrological impacts offer considerable potential to achieve this. Copyright (C) 2007 Royal Meteorological Society
机译:全球气候变化的主要特征之一将是对整个欧洲的水文制度的干扰。迄今为止,对未来变化影响的评估通常仅使用一种气候模型的结果,因此低估了不同气候模型预测的可能变化范围。在此,比较了六个区域气候模型(RCM)再现整个欧洲六个流域1961-1990年期间的平均降水的技巧,并评估了它们对未来降水变化的预测。还描述了基于月降水异常的简单干旱指数,并将其用于评估模型。观测到的再现月均降水量和干旱统计数据的模型技巧差异很大,而干旱事件的再现模型误差与均值无关,这表明该模型难以再现观测到的低月降雨量总量的持续性。从广义上讲,这些模型表明整个欧洲夏季减少,冬季降水增加。在影响分析所需的区域尺度上,对于未来的预测,尤其是干旱频率,证明了相当大的模型不确定性。尽管确定了南欧流域长期干旱的频率增加,但这种变化的程度尚不确定。相比之下,对于英格兰北部的一个流域,此类事件的发生频率可能​​会降低。对于持续时间较短的干旱,未来的变化包括变化的方向。对于每个地区的利益相关者而言,这些变化和不确定性给水资源管理带来了不同的挑战。对于科学界而言,所面临的挑战是如何将这种不确定性纳入气候变化预测中,从而使这些群体能够基于模型预测做出明智的决策。建议针对特定水文影响的概率方案提供了实现此目标的巨大潜力。皇家气象学会(C)2007

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