Atmospheric Dynamics and Numerical Simulations of Six Frontal Dust Storms in the Middle East Region

dc.bibliographicCitation.firstPage125eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.volume12eng
dc.contributor.authorHamzeh, Nasim Hossein
dc.contributor.authorKarami, Sara
dc.contributor.authorKaskaoutis, Dimitris G.
dc.contributor.authorTegen, Ina
dc.contributor.authorMoradi, Mohamad
dc.contributor.authorOpp, Christian
dc.date.accessioned2022-03-03T10:18:43Z
dc.date.available2022-03-03T10:18:43Z
dc.date.issued2021
dc.description.abstractThis study analyzes six frontal dust storms in the Middle East during the cold period (October–March), aiming to examine the atmospheric circulation patterns and force dynamics that triggered the fronts and the associated (pre-or post-frontal) dust storms. Cold troughs mostly located over Turkey, Syria and north Iraq played a major role in the front propagation at the surface, while cyclonic conditions and strong winds facilitated the dust storms. The presence of an upper-atmosphere (300 hPa) sub-tropical jet stream traversing from Egypt to Iran constitutes also a dynamic force accompanying the frontal dust storms. Moderate-Resolution Imaging Spectroradiometer (MODIS) and Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) observations are used to monitor the spatial and vertical extent of the dust storms, while model (Weather Research and Forecasting model coupled with Chemistry (WRF-Chem), Copernicus Atmospheric Monitoring Service (CAMS), Regional Climate Model-4 (RegCM4)) simulations are also analyzed. The WRF-Chem outputs were in better agreement with the MODIS observations compared to those of CAMS and RegCM4. The fronts were identified by WRF-Chem simulations via gradients in the potential temperature and sudden changes of wind direction in vertical cross-sections. Overall, the uncertainties in the simulations and the remarkable differences between the model outputs indicate that modelling of dust storms in the Middle East is really challenging due to the complex terrain, incorrect representation of the dust sources and soil/surface characteristics, and uncertainties in simulating the wind speed/direction and meteorological dynamics. Given the potential threat by dust storms, more attention should be directed to the dust model development in this region. © 2021 by the authors. Licensee MDPI, Basel, Switzerland.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8119
dc.identifier.urihttps://doi.org/10.34657/7159
dc.language.isoengeng
dc.publisherBasel : MDPIeng
dc.relation.doihttps://doi.org/10.3390/atmos12010125
dc.relation.essn2073-4433
dc.relation.ispartofseriesAtmosphere 12 (2021), Nr. 1eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectAODeng
dc.subjectFrontal dust stormeng
dc.subjectMiddle Easteng
dc.subjectMODISeng
dc.subjectNumerical prediction modelseng
dc.subjectSynoptic meteorologyeng
dc.subject.ddc550eng
dc.titleAtmospheric Dynamics and Numerical Simulations of Six Frontal Dust Storms in the Middle East Regioneng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleAtmosphereeng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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