Hydrology and earth system sciences· 2026Q1
Climatology and trends of observed daily and hourly extreme precipitation in the French Alps
- 3citations
- Q1SCImago
- 2026year
Short summary
Extreme precipitation events in the French Alps show significant regional and seasonal trends, with daily extremes increasing in the south and decreasing in the north, while hourly extremes exhibit an east-west divide.
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Key points
- Daily extreme precipitation shows strong positive trends in the southern French Alps and negative trends in the north, particularly influenced by autumn.
- Hourly extreme precipitation trends are mostly non-significant but indicate an east-west division, with positive trends in the high Alps and negative trends in the pre-Alps.
- The study provides an updated climatology and trend analysis of daily and hourly precipitation extremes, defined as 20-year return levels.
- Differences in precipitation extremes and trends are strongly influenced by complex topography, seasons, and weather patterns across the northern and southern Alps.
AI-generated from the title and abstract; the full text is not read.
Abstract
Abstract. The French Alps are characterized by complex topography, which influences precipitation regimes and associated risks in various ways. Extreme precipitation, especially when it happens on very short timescales, can lead to flash floods and landslides with important social and economic impacts. Local stakeholders, working on prevention and protection from such events, report a perceived recent increase in sub-daily extreme precipitation intensities in the French Alps. However, to our knowledge, this has not yet been confirmed statistically. In this paper, we apply a statistical approach based on extreme value theory on long time series of in situ observations. By comparing daily and hourly observations and analysing both months and seasons, we are able to present a climatology as well as trends of precipitation extremes in unprecedented detail. Here we define 'extreme' as 20-year return levels of precipitation intensity, focusing thus on very rare events. In a first part, we use a stationary framework to provide an updated climatology of daily and hourly extremes. We make use of an existing weather pattern classification to show the dynamic influences on precipitation maxima, highlighting the strong differences between the northern and the southern French Alps as well as between seasons. In a second part, we compute trends of these extremes, for which we also find partially large differences between regions and seasons. For annual extremes of daily precipitation, we find strong positive trends in the south and negative trends in the north, mostly driven by changes in autumn. Annual trends of hourly extremes are mostly non-significant and show more of an east-west division, with positive trends in the high Alps and negative ones in the pre-Alps.
The authors' abstract, as published at the source. Hydrology and earth system sciences, 2026 · DOI ↗
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