Year-to-year fluctuations in fog-water collection in central Mediterranean Iberian Peninsula and the influential large-scale tropospheric circulation patterns

被引:0
作者
Agosta, Eduardo Andres [1 ]
Corell, David [2 ]
Estrela, Maria Jose [2 ]
机构
[1] Spanish Catholic Bishops Conf, Dept Integral Ecol, Calle Anastro 1, Madrid 28033, Spain
[2] Univ Valencia, Fac Geog & Hist, Dept Geog, Ave Blasco Ibanez 28, Valencia 46010, Spain
关键词
Fog-water collection/harvesting; NAO; Teleconnection patterns; Interannual variability; Global warming; VARIABILITY; PRECIPITATION; RAINFALL; OSCILLATION; SEASONALITY; RESOURCES; REGION;
D O I
10.1016/j.atmosres.2025.108210
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study examines the mean annual cycles of monthly cumulated fog-water amounts (CFW) in the central Mediterranean Iberian Peninsula (MIP), highlighting the interplay between meteorological conditions, topography, and geographic location. Seasonal asymmetry in fog-water collection is evident, with summer exhibiting higher fog collection frequency but lower water volumes. In contrast, non-summer seasons feature lower frequency but higher intensity fog events. Tropospheric circulation anomalies at mid-and low-tropospheric levels reveal that fog-water collection is influenced by moisture transport from the Mediterranean, particularly during high fog-collection months. Positive specific humidity anomalies near coastal areas, driven by southeasterly wind anomalies, are crucial for frequent fog formation, while broader, less concentrated anomalies characterize higher-intensity fog events. These findings align with prior research emphasizing the role of cyclonic conditions and maritime moisture advection in enhancing fog-water collection yields. Additionally, seasonal variations in tropospheric circulation anomalies are linked to large-scale teleconnection patterns such as the North Atlantic Oscillation (NAO), Arctic Oscillation (AO), and Eastern Atlantic-Western Russia (EAWR) patterns. These modulate moisture advection, precipitation anomalies, and low-level winds that drive fog formation and collection. In summer, subtropical high-pressure weakening contributes to increased fog-water cumulates, while winter anomalies highlight the impact of quasi-stationary cyclonic circulations and autumn anomalies, positive NAO/AO phases. These results underscore the climatic importance of fog-water collection for water resource management in drought-prone regions and provide a foundation for future climate monitoring and prediction under anthropogenic radiative forcing. The study's insights have practical implications for enhancing water availability through fog collection in Mediterranean ecosystems.
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页数:18
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