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Titlebook: Recent Research on Hydrogeology, Geoecology and Atmospheric Sciences; Proceedings of the 1 Haroun Chenchouni,Helder I. Chaminé,Mingjie Chen

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樓主: 海市蜃樓
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發(fā)表于 2025-3-23 10:30:46 | 只看該作者
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發(fā)表于 2025-3-23 14:29:01 | 只看該作者
Recent Research on Hydrogeology, Geoecology and Atmospheric SciencesProceedings of the 1
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發(fā)表于 2025-3-23 21:58:26 | 只看該作者
Impact of Potential Evapotranspiration Estimation on River Discharge in the Casamance Basin (Southerlibrated and validated with Nash–Sutcliffe efficiencies of 70.4% and 69.0%, respectively, at the outlet Kolda. The signals of the flow regimes were well reproduced even though the magnitudes were sometimes underestimated. The variations in the simulated flows as a function of those observed displaye
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發(fā)表于 2025-3-23 22:21:21 | 只看該作者
Hydrochemical Attributes and Their Spatial Variation in the Rainwater of Kuwaite samples identified that crustal, marine, and anthropogenic sources of the neutralizing ions have influenced the rainwater chemistry. The principal component analysis (PCA)?revealed that the anthropogenic influence is more significant from oil refineries, apart from other industrial activities, and
15#
發(fā)表于 2025-3-24 04:06:41 | 只看該作者
A Tool in R for Easy Hydroclimatic Calculationsl Process 25:1924–1933, 2011; Rau et al. in Spatio-temporal analysis of monthly temperature in the mountainous regions of Peru. An approach for NCEP NCAR Reanalysis data correction, 2013); (c) Estimation of a monthly runoff index for ungauged watersheds through the GR2M model (Rau et al. in Hydrol P
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發(fā)表于 2025-3-24 07:00:54 | 只看該作者
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發(fā)表于 2025-3-24 10:41:49 | 只看該作者
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發(fā)表于 2025-3-24 15:34:32 | 只看該作者
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發(fā)表于 2025-3-24 19:00:47 | 只看該作者
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發(fā)表于 2025-3-25 03:08:51 | 只看該作者
Hydrological Flows and Flood Protection: Case Study of the Mexa Dam (Mafragh River Basin, North-Eastafety but are a factor in the aggravation of floods on houses and agricultural lands downstream. Moreover, the period of flood discharges can extend over several months (159 successive days following the floods observed in December 2003–January 2004 and 143?days during the February–March 2012 floods
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