Simulating the impact of varying vegetation on West African monsoon surface fluxes using a regional convection-permitting model. [PDF]
Comparison between the use of varying vegetation fraction and fix vegetation fraction in regional climate models over West Africa: Case study of the Unified Model with focus on three different climatic zones. Abstract This study assessed the sensitivity of the West African climate to varying vegetation fractions.
Bamba A +8 more
europepmc +2 more sources
Modeling the impact of measured and projected climate and management systems on agricultural fields: Surface runoff, soil moisture, and soil erosion. [PDF]
Abstract As global climate change poses a challenge to crop production, it is imperative to prioritize effective adaptation of agricultural systems based on a scientific understanding of likely impacts. In this study, we applied an integrated watershed modeling framework to examine the impacts of projected climate on runoff, soil moisture, and soil ...
Lee S +7 more
europepmc +2 more sources
Station hydrologique cotière d'Abidjan de 1966 à 1980 [PDF]
In this document the monthly T-S diagrams and the regression lines of the temperature and salinity two weeks mean values have been drawn for 0, 5, 10, 15, 20 and 25 meters of depth. The annual variations of the dynamic height anomaly are represented for every coastal station from 1966 to 1980.
Cissoko, S.
openaire +4 more sources
Stations cotieres et station hydrologique cotiere d'Abidjan: annees 1980-1981 [PDF]
Beach surface temperature is recorded every morning between 7h30 and 8h00 at each coastal station. On figure 2, 3, 4 and 5 it has been plotted daily variation and mean variation computed on 7, 15 and 30 days basis of sea surface temperature. However it seems that variations of dynamic height anomaly are reflecting more accurately the stages of the ...
Cissoko, S.
openaire +4 more sources
Calage et validation de SWAT sur le bassin versant du Bafing (Fleuve Sénégal) en amont de BAFING MAKANA : vers une application à la gestion du barrage de Manantali [PDF]
En matière de Gestion des Ressources En Eau, il devient de plus en plus nécessaire de remonter à l'information pluviométrique. La modélisation est devenue ainsi un outil incontournable. Les modèles hydrologiques reposent sur le cycle hydrologique.
S. Sambou +5 more
doaj +1 more source
OSSEC Rhône : outil opérationnel de suivi des étiages en temps réel sur le Rhône
L’Outil de Suivi et de Surveillance des Étiages en Cohérence sur le Rhône (OSSEC Rhône) est un outil permettant de caractériser en temps réel les événements d’étiage sur le Rhône et ses principaux affluents.
Blaise Calmel +3 more
doaj +1 more source
Variabilité hydroclimatique en Basse-Casamance : tendances et perceptions communautaires [PDF]
En zone soudanienne, les épisodes climatiques dégradantes des quatre dernières décennies continuent d’engendrer des contraintes socioéconomiques et environnementales dans les territoires.
Bouly SANE; Yancoba SANE
doaj
The soil and water assessment tool (SWAT) model is used to assess the effects of land‐use change on the hydrological processes of the Lake Tana basin. According to the findings, the SWAT model is essential for effective modeling of the impact of land‐use change on water quality and quantity. Abstract Human activities impact hydrology through changes in
Birhan Getachew +1 more
wiley +1 more source
Abstract Hard rock aquifers (HRAs) in West Africa (WA) are located within a thick regolith layer. The representation of thick tropical regolith in integrated hydrological models lacks consensus on aquifer geometries and parameter ranges. Our main objective was to determine the knowledge requirements on saturated hydraulic conductivity (Ks) to model the
Amelie Herzog +6 more
wiley +1 more source
Le présent travail a pour objectif d'améliorer notre connaissance du cycle de l'eau et en particulier de l'apport du manteau neigeux dans le bilan hydrologique au niveau du bassin versant montagneux du Rheraya au Sud de la ville de Marrakech.
Abdelghani Boudhar +4 more
doaj +1 more source

