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Impact of vegetation and soil moisture seasonal dynamics on dust emissions over the Sahel
Author(s) -
Pierre C.,
Bergametti G.,
Marticorena B.,
Mougin E.,
Bouet C.,
Schmechtig C.
Publication year - 2012
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd016950
Subject(s) - environmental science , vegetation (pathology) , atmospheric sciences , mineral dust , arid , forcing (mathematics) , range (aeronautics) , satellite , water content , climatology , annual cycle , aerosol , meteorology , geology , geography , medicine , paleontology , materials science , geotechnical engineering , pathology , aerospace engineering , engineering , composite material
To address the challenging issue of estimating mineral dust emissions from the semi‐arid Sahel, a modeling approach is developed by combining two specific models: one dedicated to the simulation of the seasonal herbaceous layer in the Sahel (STEP) and the other to the estimation of dust emissions (MB). The area of interest is the Sahelian belt (12°N–20°N, 20°W–35°E) and the simulations were performed at a 0.25° spatial resolution over a 4‐year period (2004–2007). The rainfall forcing is provided by a TRMM (Tropical Rainfall Measuring Mission) satellite‐derived product; the other meteorological data are ECMWF products. An empirical parameterization is used to estimate the surface roughness and its temporal dynamics according to the characteristics of the simulated vegetation in terms of surface cover and height. Where no vegetation grows, the surface properties are considered as constant in time and are derived from the POLDER‐1 satellite measurements. Simulations are constrained step by step by comparisons with observations. Simulated annual dust fluxes emitted from the whole area range from approximately 100 Mt to 400 Mt depending on the year, in good agreement with previous works dealing with Saharan dust emissions. For the fringe where herbaceous vegetation can affect dust emissions, the annual dust emission fluxes range between 0.5 Mt and 20 Mt depending on the year. Inhibition of dust emissions due to the seasonal dynamics of vegetation and surface soil moisture over this fringe varies between 20% and 35%.

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