Abstract
The causes of recent hydrological droughts and their future evolution under a changing climate are still poorly
understood. Banking on a 216-year river flow time series at the Po River outlet, we show that the 2022 hydrological
drought is the worst event (30% lower than the second worst, with a six-century return period), part of an
increasing trend in severe drought occurrence. The decline in summer river flows (−4.14 cubic meters per
second per year), which is more relevant than the precipitation decline, is attributed to a combination of
changes in the precipitation regime, resulting in a decline of snow fraction (−0.6% per year) and snowmelt
(−0.18 millimeters per day per year), and to increasing evaporation rate (+0.013 cubic kilometers per year)
and irrigated areas (100% increment from 1900). Our study presents a compelling case where the hydrological
impact of climate change is exacerbated by local changes in hydrologic seasonality and water use.
Lingua originale | Inglese |
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pagine (da-a) | eadg8304 |
Rivista | Science advances |
Volume | 9 |
Numero di pubblicazione | 32 |
DOI | |
Stato di pubblicazione | Pubblicato - 2023 |