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in Modeling Earth Systems (JAMES)Journal of Geophysical Research All units are mm. Any queries (other than missing content) should be directed to the corresponding author for the article.Please check your email for instructions on resetting your password. Thus the transition (equinox) seasons bring most rainfall to East Africa (Figure right panel). Here the potential impact of the stratospheric aerosol geoengineering on the West African Summer Monsoon precipitation and the associated mechanisms are investigated, using climate model simulations from the Geoengineering Large Ensemble project that used stratospheric sulfate aerosols injection to stabilize global mean surface temperature and, also, the interhemispheric and equator‐to‐pole temperature gradients at their 2020 values under RCP8.5 scenario. This method is identified as a possible means to reduce the climate impacts of global warming. Authors; Authors and affiliations; A. Journal of Geomagnetism and AeronomyNonlinear If you do not receive an email within 10 minutes, your email address may not be registered,

We found that simulated rainfall in GLENS reasonably reproduces the observed spatial patterns of WASM precipitation, including its characteristic northward jump over the season.We focused our study on three specific regions which are the NSA, the SSA, and the WAR. Composition and StructureInformation First Online: 08 May 2018.

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NASA and University of Maryland scientists have found that the African monsoon consists of two distinct seasons.
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and Chemical OceanographySolar In this latter region, if the objective were to restore the Western African monsoon precipitation, this work suggests that the deployment of SAG should be limited to offset 1/3 of RCP8.5 warming.In this study, we identified the physical mechanisms behind changes in WASM precipitation under RCP8.5 and GLENS, by applying the decomposition method developed in Chadwick et al. Results indicate that under Representative Concentration Pathway 8.5, during the monsoon period, precipitation increases by 44.76%, 19.74%, and 5.14% compared to the present‐day climate in the Northern Sahel, Southern Sahel, and Western Africa region, respectively.

Using simulations from the Geoengineering Large Ensemble project that employed stratospheric sulfate aerosols injection to keep global mean surface temperature and also the interhemispheric and equator‐to‐pole temperature gradients at their 2020 values (present‐day climate) under Representative Concentration Pathway 8.5 scenario, we investigate the potential impact of SAG on the West African Summer Monsoon (WASM) precipitation and the involved physical processes.

Here the potential impact of the stratospheric aerosol geoengineering on the West African Summer Monsoon precipitation and the associated mechanisms are investigated, using climate model simulations from the Geoengineering Large Ensemble project that used stratospheric sulfate aerosols injection to stabilize global mean surface temperature and, also, the interhemispheric and equator‐to‐pole temperature gradients at their 2020 values under RCP8.5 …
An increase in Sahel precipitation has been associated with a summer intensification and northward shift of the West African monsoon system as a response to amplified warming over the Sahara. and you may need to create a new Wiley Online Library account.Enter your email address below and we will send you your usernameIf the address matches an existing account you will receive an email with instructions to retrieve your username



Spatial pattern of mean monthly JASO (July to October) precipitation computed for 1990–2009 in the West Africa from (a) model, (b) GPCP, and (c) CMAP.