瑞士气候变化下的复合干旱

Christoph Nathanael von Matt, Regula Muelchi, L. Gudmundsson, Olivia Martius
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摘要

摘要由于在低流量时期从河流中取水受到限制,而同时灌溉需求又很高,因此瑞士在生长季节同时出现气象、农业和水文干旱(多变量复合干旱)是一个问题。我们使用瑞士的瞬态气候和水文情景(CH2018 和 Hydro-CH2018)分析了瑞士 52 个集水区在延长的夏季(5 月至 10 月)的复合干旱情况,包括有减缓措施的情景(代表性浓度路径 2.6 (RCP2.6),8 个模型链)和无减缓措施的情景(RCP8.5,20 个模型链)。在 RCP8.5 情景下,预计到本世纪中叶,瑞士所有大区的复合干旱日数将显著增加。频率增加的主要原因是干旱事件更频繁(显著),而不是事件持续时间更长(不显著)。模型对变化符号的看法基本一致。到 2085 年,预计阿尔卑斯山以北地区每个集水区在夏季延长季节发生复合干旱事件的中位数为 1 次,阿尔卑斯山以南地区为每 1-2 年发生 1 次。此外,复合干旱日数的增加主要发生在 5 月至 10 月间,导致主要农业生产季节的转移和更明显的季节性,最高发生概率出现在 7 月中旬至 10 月初。加上日数和事件的增加,预计将有更多的流域同时受到复合干旱的影响。在 RCP2.6(减缓)情景下,到 21 世纪末,复合干旱天数和事件的增加并不显著。与 RCP8.5 相比,到本世纪末,阿尔卑斯山以北的复合干旱日数减少了 50%-55%,阿尔卑斯山以南则减少了 75%。这强调了协调适应与早期采取的减缓措施相结合的必要性。
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Compound droughts under climate change in Switzerland
Abstract. The co-occurrence of meteorological, agricultural, and hydrological droughts (multivariate compound droughts) in Switzerland during growing season is problematic due to limitations in water abstractions from rivers during low-flow periods, while at the same time the need for irrigation is high. We analyse compound droughts for 52 catchments in Switzerland during the extended summer season (May–October) using the transient climate and hydrological scenarios for Switzerland (CH2018 and Hydro-CH2018) for both a scenario with mitigation (representative concentration pathway 2.6 (RCP2.6), 8 model chains) and a scenario without mitigation (RCP8.5, 20 model chains). In the RCP8.5 scenario the number of compound drought days is projected to significantly increase by mid-century across all greater regions of Switzerland. The increased frequency is mainly a result of more frequent events (significant) rather than longer event durations (non-significant). Models generally agree on the sign of change. By 2085, compound drought events are projected to occur in median once per catchment per extended summer season north of the Alps and every 1–2 years south of the Alps. Further, the increases in compound drought days mainly occur between May–October, leading to a shift in the main agricultural production season and a more pronounced seasonality with the highest occurrence probabilities between mid-July and the beginning of October. Coupled to the increase in days and events, significantly more catchments are projected to be affected by compound droughts at the same time. In the RCP2.6 (mitigation) scenario, the increase in the number of compound drought days and events is not significant by the end of the 21st century. In comparison with RCP8.5, the number of compound drought days is reduced by 50 %–55 % north of the Alps and by up to 75 % south of the Alps by the end of the century. This emphasizes the need for coordinated adaptation in combination with mitigation measures taken at an early stage.
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