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荷兰新的气候变化情景。

New climate change scenarios for the Netherlands.

作者信息

van den Hurk B, Tank A K, Lenderink G, Ulden A van, Oldenborgh G J van, Katsman C, Brink H van den, Keller F, Bessembinder J, Burgers G, Komen G, Hazeleger W, Drijfhout S

机构信息

KNMI, Postbox 201, 3730 AE De Bilt, The Netherlands.

出版信息

Water Sci Technol. 2007;56(4):27-33. doi: 10.2166/wst.2007.533.

Abstract

A new set of climate change scenarios for 2050 for the Netherlands was produced recently. The scenarios span a wide range of possible future climate conditions, and include climate variables that are of interest to a broad user community. The scenario values are constructed by combining output from an ensemble of recent General Climate Model (GCM) simulations, Regional Climate Model (RCM) output, meteorological observations and a touch of expert judgment. For temperature, precipitation, potential evaporation and wind four scenarios are constructed, encompassing ranges of both global mean temperature rise in 2050 and the strength of the response of the dominant atmospheric circulation in the area of interest to global warming. For this particular area, wintertime precipitation is seen to increase between 3.5 and 7% per degree global warming, but mean summertime precipitation shows opposite signs depending on the assumed response of the circulation regime. Annual maximum daily mean wind speed shows small changes compared to the observed (natural) variability of this variable. Sea level rise in the North Sea in 2100 ranges between 35 and 85 cm. Preliminary assessment of the impact of the new scenarios on water management and coastal defence policies indicate that particularly dry summer scenarios and increased intensity of extreme daily precipitation deserves additional attention in the near future.

摘要

荷兰最近生成了一套新的2050年气候变化情景。这些情景涵盖了未来广泛的可能气候状况,并且包括广大用户群体感兴趣的气候变量。情景值是通过综合近期通用气候模型(GCM)模拟集合的输出、区域气候模型(RCM)输出、气象观测数据以及一些专家判断构建而成的。针对温度、降水、潜在蒸发和风速构建了四种情景,涵盖了2050年全球平均气温上升幅度以及感兴趣区域内主导大气环流对全球变暖响应强度的范围。对于该特定区域,每升温1摄氏度,冬季降水预计增加3.5%至7%,但夏季平均降水根据假定的环流模式响应呈现相反趋势。与该变量观测到的(自然)变率相比,年最大日平均风速变化较小。2100年北海海平面上升幅度在35厘米至85厘米之间。对新情景对水资源管理和海岸防御政策影响的初步评估表明,在不久的将来,特别干旱的夏季情景以及极端日降水强度增加尤其值得关注。

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