Evaluation of convection-permitting extreme precipitation simulations for the south of France

Linh N. Luu, R. Vautard, P. Yiou, J. Soubeyroux
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引用次数: 8

Abstract

Abstract. In the autumn, the French Mediterranean area is frequently exposed to heavy precipitation events whose daily accumulation can exceed 300 mm. One of the key processes contributing to these precipitation amounts is deep convection, which can be explicitly resolved by state-of-the-art convection-permitting models to reproduce heavy rainfall events that are comparable to observations. This approach has been tested and performed at climate scale in several studies in recent decades for different areas. In this research, we investigate the added value of using an ensemble of three climate simulations at convection-permitting resolution (approx. 3 km) to replicate extreme precipitation events at both daily and shorter timescales over the south of France. These three convection-permitting simulations are performed with the Weather Research and Forecasting (WRF) Model. They are forced by three EURO-CORDEX simulations, which are also run with WRF at the resolution of 0.11∘ (approx. 12 km). We found that a convection-permitting approach provides a more realistic representation of extreme daily and 3-hourly rainfall in comparison with EURO-CORDEX simulations. Their similarity to observations allows use for climate change studies and its impacts.
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法国南部允许对流的极端降水模拟的评估
摘要在秋季,法属地中海地区经常遭受日累积可超过300毫米的强降水事件。造成这些降水量的关键过程之一是深对流,这可以通过最先进的对流允许模型来明确地解决,以重现与观测相媲美的强降雨事件。近几十年来,在不同地区的几项研究中,这种方法已经在气候尺度上得到了测试和实施。在这项研究中,我们研究了在允许对流的分辨率下使用三个气候模拟集合的附加价值。(3公里)来复制法国南部每日和更短时间尺度的极端降水事件。这三个允许对流的模拟是用天气研究与预报(WRF)模式进行的。它们是由三个euro - cordex模拟得出的,这些模拟也在WRF下以0.11°(约)的分辨率运行。12公里)。我们发现,与EURO-CORDEX模拟相比,允许对流的方法提供了更真实的极端日和3小时降雨量。它们与观测结果的相似性允许用于气候变化研究及其影响。
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