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  Impact of vegetation and preferential source areas on global dust aerosol: Results from a model study

Tegen, I., Harrison, S. P., Kohfeld, K. E., Prentice, I. C., Coe, M., & Heimann, M. (2002). Impact of vegetation and preferential source areas on global dust aerosol: Results from a model study. Journal of Geophysical Research-Atmospheres, 107(D21): 4576. doi:10.1029/2001JD000963.

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BGC0553.pdf (Verlagsversion), 8MB
 
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 Urheber:
Tegen, I.1, Autor           
Harrison, S. P.2, Autor           
Kohfeld, K. E.2, Autor           
Prentice, I. C.1, Autor           
Coe, M., Autor
Heimann, M.3, Autor           
Affiliations:
1Department Biogeochemical Synthesis, Prof. C. Prentice, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497753              
2Research Group Paleo-Climatology, Dr. S. P. Harrison, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497765              
3Department Biogeochemical Systems, Prof. M. Heimann, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497755              

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Schlagwörter: aerosols; mineral dust; tracer modeling; global modeling General-circulation model; last glacial maximum; north-atlantic ocean; deep arabian sea; particle fluxes; sediment trap; atmospheric dust; pacific-ocean; saharan dust; mineral dust
 Zusammenfassung: We present a model of the dust cycle that successfully predicts dust emissions as determined by land surface properties, monthly vegetation and snow cover, and 6-hourly surface wind speeds for the years 1982-1993. The model takes account of the role of dry lake beds as preferential source areas for dust emission. The occurrence of these preferential sources is determined by a water routing and storage model. The dust source scheme also explicitly takes into account the role of vegetation type as well as monthly vegetation cover. Dust transport is computed using assimilated winds for the years 1987-1990. Deposition of dust occurs through dry and wet deposition, where subcloud scavenging is calculated using assimilated precipitation fields. Comparison of simulated patterns of atmospheric dust loading with the Total Ozone Mapping Spectrometer satellite absorbing aerosol index shows that the model produces realistic results from daily to interannual timescales. The magnitude of dust deposition agrees well with sediment flux data from marine sites. Emission of submicron dust from preferential source areas are required for the computation of a realistic dust optical thickness. Sensitivity studies show that Asian dust source strengths are particularly sensitive to the seasonality of vegetation cover.

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 Datum: 2002-02-042002-11-092002
 Publikationsstatus: Erschienen
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 Identifikatoren: DOI: 10.1029/2001JD000963
Anderer: BGC0553
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Titel: Journal of Geophysical Research-Atmospheres
Genre der Quelle: Zeitschrift
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Ort, Verlag, Ausgabe: Washington, D.C. : American Geophysical Union
Seiten: - Band / Heft: 107 (D21) Artikelnummer: 4576 Start- / Endseite: - Identifikator: ISSN: 0148-0227
CoNE: https://pure.mpg.de/cone/journals/resource/991042728714264_1