A new process-based and scale-aware desert dust emission scheme for global climate models – Part I: Description and evaluation against inverse modeling emissions
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Published:2023-06-14
Issue:11
Volume:23
Page:6487-6523
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Leung Danny M.ORCID, Kok Jasper F.ORCID, Li LongleiORCID, Okin Gregory S.ORCID, Prigent Catherine, Klose MartinaORCID, Pérez García-Pando CarlosORCID, Menut LaurentORCID, Mahowald Natalie M.ORCID, Lawrence David M.ORCID, Chamecki Marcelo
Abstract
Abstract. Desert dust accounts for most of the atmosphere's aerosol burden by mass and
produces numerous important impacts on the Earth system. However, current
global climate models (GCMs) and land-surface models (LSMs) struggle to
accurately represent key dust emission processes, in part because of
inadequate representations of soil particle sizes that affect the dust
emission threshold, surface roughness elements that absorb wind momentum,
and boundary-layer characteristics that control wind fluctuations.
Furthermore, because dust emission is driven by small-scale (∼ 1 km or smaller) processes, simulating the global cycle of desert dust in
GCMs with coarse horizontal resolutions (∼ 100 km) presents a
fundamental challenge. This representation problem is exacerbated by dust
emission fluxes scaling nonlinearly with wind speed above a threshold wind
speed that is sensitive to land-surface characteristics. Here, we address
these fundamental problems underlying the simulation of dust emissions in
GCMs and LSMs by developing improved descriptions of (1) the effect of soil
texture on the dust emission threshold, (2) the effects of nonerodible
roughness elements (both rocks and green vegetation) on the surface wind
stress, and (3) the effects of boundary-layer turbulence on driving
intermittent dust emissions. We then use the resulting revised dust emission
parameterization to simulate global dust emissions in a standalone model
forced by reanalysis meteorology and land-surface fields. We further propose
(4) a simple methodology to rescale lower-resolution dust emission
simulations to match the spatial variability of higher-resolution emission
simulations in GCMs. The resulting dust emission simulation shows
substantially improved agreement against regional dust emissions
observationally constrained by inverse modeling. We thus find that our
revised dust emission parameterization can substantially improve dust
emission simulations in GCMs and LSMs.
Funder
Directorate for Geosciences Army Research Office Helmholtz Association Horizon 2020
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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