Assessing the Impact of Climate Change on Soil Moisture and Temperature Regimes in Northern Algeria
DOI:
https://doi.org/10.54386/jam.v28i2.3263Keywords:
Soil moisture regime, Climate change, Java Newhall simulation model, Soil classification, Algeria , Soil temperature regimeAbstract
This study analyzes the evolution of hydric and thermal regimes in the main soils of the Algiers region, including the Sahel and the Mitidja Plain, using climatic data from several representative stations. The results show significant spatial and temporal variability linked to recent climatic fluctuations. Most stations exhibit a xeric moisture regime typical of Mediterranean climates, with alternating wet and dry periods. Since the 2000s, the Mitidja Plain has shown a gradual trend toward wetter conditions, marked by more wet days and fewer dry days. Temperature data indicate an increase of about 0.8 °C since 1984, from 17.3 °C to 18.1 °C on average, with all stations classified within the thermic regime (mean annual temperature > 8 °C). These changes illustrate the effects of regional climate change—greater rainfall variability and general warming—which affect soil classification and pedogenesis through changes in water availability, leaching, and oxidation. The study underscores the importance of sustainable land management to mitigate soil degradation and erosion.
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