6533b851fe1ef96bd12a8f54
RESEARCH PRODUCT
Role of Indian fluxes in the intraseasonal 10-30 days variability of the African monsoon.
Djiby SarrAichetou DiaChristophe DuroureAbou Karim FarotaAbdoulaye SyAbdoulaye Bouya DiopBenjamin PohlBouya Diopsubject
Monsoon of South AsiaConvectionMonsoonFluxIndianRossby waveMonsoonWest africanWater-vapor[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/ClimatologyFlux (metallurgy)13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyActive phaseSahelEnvironmental scienceIntra-seasonaldescription
12 pages; International audience; This study focused on the influence of Indian monsoon on the 10-30 days variability of the West African monsoon. One relies on the 500-300 hPa moisture fluxes calculated from specific wind and moisture fields from the ERAInterim reanalysis over the 1998-2008 period. These fluxes carry a signal of a spatio-temporal Rossby wave structure propagating westward from India. In the active phase of high convection of this wave, 500-300 hPa fluxes are Easterly. This high-tropospheric Rossby wave signal from the Indian monsoon area would modulate the dynamics over the Sahel.
year | journal | country | edition | language |
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2018-10-29 |