Future Changes in Day-to-Day Precipitation Variability in Europe

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Hydrometeorology Pub Date : 2024-06-11 DOI:10.1175/jhm-d-23-0206.1
Ondřej Lhotka, E. Plavcová, R. Beranová
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Abstract

We analyzed regional patterns of day-to-day precipitation variability across Europe and assessed their future changes using CORDEX regional climate models. A discrete Markov chain process was employed to calculate transition probabilities from wet and dry states and the precipitation variability was quantified using the proposed Variability index (IVAR; sum of wet-to-dry and dry-to-wet transitions divided by total number of transitions). IVAR is, in general, lowest in Southern Europe and gradually increases northward in the observed data. Performance of the regional climate models is season dependent: they capture IVAR reasonably well in summer but higher simulated variability was found for the winter season. IVAR trends computed for the 2006–2095 period suggest decreasing day-to-day precipitation variability over Southern Europe, especially in summer under the high-concentration RCP8.5 pathway. By contrast, increased variability is projected in Northern Europe. Between these two regions, future IVAR trends are less clear, because they strongly depend on the selection of driving global model, hinting of an uncertain future hydroclimate in the Central European region.
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欧洲逐日降水变异性的未来变化
我们利用 CORDEX 区域气候模式分析了欧洲地区降水日变化模式并评估了其未来变化。我们采用离散马尔可夫链过程来计算从干湿状态过渡的概率,并利用提出的变率指数(IVAR;从湿到干和从干到湿过渡的总和除以过渡总数)来量化降水变率。一般来说,IVAR 在南欧最低,在观测数据中向北逐渐增加。区域气候模式的性能与季节有关:它们对夏季 IVAR 的捕捉相当好,但发现冬季的模拟变率较高。计算出的 2006-2095 年 IVAR 趋势表明,南欧降水的逐日变率在下降,尤其是在高浓度 RCP8.5 路径下的夏季。相比之下,北欧的变率预计会增加。在这两个地区之间,未来的 IVAR 趋势并不明显,因为它们在很大程度上取决于驱动全球模式的选择,这表明中欧地区未来的水文气候并不确定。
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来源期刊
Journal of Hydrometeorology
Journal of Hydrometeorology 地学-气象与大气科学
CiteScore
7.40
自引率
5.30%
发文量
116
审稿时长
4-8 weeks
期刊介绍: The Journal of Hydrometeorology (JHM) (ISSN: 1525-755X; eISSN: 1525-7541) publishes research on modeling, observing, and forecasting processes related to fluxes and storage of water and energy, including interactions with the boundary layer and lower atmosphere, and processes related to precipitation, radiation, and other meteorological inputs.
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