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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Projected changes in precipitation intensity and frequency in Switzerland: a multi-model perspective
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Projected changes in precipitation intensity and frequency in Switzerland: a multi-model perspective

机译:瑞士降水强度和频率的预计变化:多模型视角

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摘要

Fundamental changes in the hydrological cycle are to be expected in a future warmer climate. For Switzerland, recent climate change assessments based on the ENSEMBLES regional climate models project for the A1B emission scenario summer mean precipitation to significantly decrease by the end of this century, whereas winter mean precipitation tend to rise in Southern Switzerland. From an end-user perspective, projected changes in seasonal means are often insufficient to adequately address the multifaceted challenges of climate change adaptation. In this study, we investigate the projected changes in seasonal precipitation by considering changes in frequency and intensity, precipitation type (convective vs stratiform) and temporal structure (wet and dry spells) over Switzerland. As proxies for rain-type changes, we rely on the parameterized convective and large-scale precipitation components simulated by the models. The study reveals that the projected summer drying over Switzerland at the end of the century is mainly driven by a widespread reduction in the number of precipitation days. Thereby, the drying evolves altitude-specific: over low-land regions it is associated with a decrease in both convective and large-scale precipitation. Over elevated regions it is primarily associated with a decline in large-scale precipitation only, whereas convective precipitation remains at current levels. As a consequence, almost all the models project an increase in convective fraction at elevated altitudes. The decrease in the number of wet days during summer is accompanied by decreases (increases) in the number of multi-day wet (dry) spells. This future shift in multi-day episodes also lowers down the likelihood of short dry spell occurrence in all of the models. The models further project a higher mean precipitation intensity in spring and autumn north of the Alps, whereas a similar tendency is expected for the winter season over most of Switzerland.
机译:在未来的温暖气候中,预计水文循环将发生根本变化。对于瑞士而言,基于ENSEMBLES区域气候模型项目的最新气候变化评估显示,到本世纪末,A1B排放情景的夏季平均降水量将显着减少,而瑞士南部的冬季平均降水量则趋于上升。从最终用户的角度来看,季节性手段的预期变化通常不足以充分应对气候变化适应的多方面挑战。在这项研究中,我们通过考虑瑞士上空的频率和强度,降水类型(对流与层状)和时间结构(湿法和干法)的变化来调查季节性降水的预计变化。作为降雨类型变化的代理,我们依靠模型模拟的参数化对流和大规模降水分量。研究表明,到本世纪末,瑞士夏季预计将出现干燥,这主要是由于降水天数的广泛减少所致。因此,干燥过程会随着海拔高度的变化而变化:在低地地区,对流降水和大规模降水都会减少。在高海拔地区,它主要仅与大规模降水的减少有关,而对流降水仍保持在当前水平。结果,几乎所有的模型都预测在高海拔地区对流分数将增加。夏季潮湿天数的减少伴随着多天潮湿(干)法术次数的减少(增加)。多日情节中这种未来的变化也降低了所有模型中短期干旱发生的可能性。这些模型进一步预测了阿尔卑斯山北部春季和秋季的平均降水强度较高,而在瑞士大部分地区的冬季,预计会有类似的趋势。

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