Climatic features of the Adige river basin (Italian Alps) were analyzed for a one-century-and-half period. A monthly water balance model was applied to a dense grid and then aggregated as a single series, representative of the whole basin. Time trends, climate variability, presence of cyclicity and links with external forcings were assessed. Precipitation regimes showed a prevailing trend of decreasing variability, but temperature showed long-term opposite trends. Not always was climate variability directly attributable to a climate change forcing.
Meteorological data in Eccel & Ranzi, A Multi‐century Meteo‐hydrological Analysis for the Adige River Basin (Central Alps). Part I: Climate Variability (1862–2011) at Different Time Scales
Roberto Ranzi
Data Curation
2025-01-01
Abstract
Climatic features of the Adige river basin (Italian Alps) were analyzed for a one-century-and-half period. A monthly water balance model was applied to a dense grid and then aggregated as a single series, representative of the whole basin. Time trends, climate variability, presence of cyclicity and links with external forcings were assessed. Precipitation regimes showed a prevailing trend of decreasing variability, but temperature showed long-term opposite trends. Not always was climate variability directly attributable to a climate change forcing. File in questo prodotto:
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Meteorological data in Eccel&Ranzi_2025.zip
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