Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019

The living conditions in the Urmia Basin (northwestern Iran) face significant challenges due to dust events. This study investigates the spatial and temporal characteristics of dust phenomena in the Urmia Basin using MERRA-2 data and observational data from Tabriz, Urmia, Sarab, and Mahabad over a 3...

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Main Authors: Elham Mobarak Hassan, Ebrahim Fattahi, Maral Habibi
Format: Article
Language:English
Published: MDPI AG 2023-11-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/12/1761
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author Elham Mobarak Hassan
Ebrahim Fattahi
Maral Habibi
author_facet Elham Mobarak Hassan
Ebrahim Fattahi
Maral Habibi
author_sort Elham Mobarak Hassan
collection DOAJ
description The living conditions in the Urmia Basin (northwestern Iran) face significant challenges due to dust events. This study investigates the spatial and temporal characteristics of dust phenomena in the Urmia Basin using MERRA-2 data and observational data from Tabriz, Urmia, Sarab, and Mahabad over a 30-year period (1990–2019). The findings reveal that despite several fluctuations, the annual number of dusty days increased from the 1990s to the 2010s in the Urmia Basin. The maximum number of dusty days was found to predominantly occur in May (spring) and October (autumn), driven by two distinct mechanisms. In early autumn, developing synoptic systems associated with increased wind speeds can cause dust emission from dry land sources. Consequently, an increase in dust wet deposition, precipitation, dust surface concentration, and the number of dusty days occurs in October. In contrast, a sharp decrease in precipitation from April to May leads to drying soil and dust emission in May. Among the studied cities, Tabriz experienced the highest number of dusty days (728) due to the combined effects of cross-border and local dust sources. The highest dust column density and dust dry deposition in the south and east of Urmia Lake indicate the impact of declining water levels, which resulted in a dry lakebed as the primary local dust source. The MERRA-2 spatial distribution reveals that dust surface concentration, and the number of dusty days decrease similarly from the southwest to the northeast of the Urmia Basin as the distance from cross-border dust sources increases. A positive correlation is observed between the number of dusty days and MEERA-2 data, including dust surface concentration, dust dry deposition, column mass dust, and total aerosol extinction, with coefficients of 0.74, 0.71, 0.69, and 0.68, respectively.
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spelling doaj.art-beabf350973e41f587447d000ea7bcf82023-12-22T13:52:47ZengMDPI AGAtmosphere2073-44332023-11-011412176110.3390/atmos14121761Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019Elham Mobarak Hassan0Ebrahim Fattahi1Maral Habibi2Department of Environment, Ahvaz Branch, Islamic Azad University, Ahvaz 61349-37333, IranDepartment of Hydrometeorology, Atmospheric Science and Meteorological Research Center, Tehran 14118-13389, IranDepartment of Geography and Regional Science, University of Graz, 8010 Graz, AustriaThe living conditions in the Urmia Basin (northwestern Iran) face significant challenges due to dust events. This study investigates the spatial and temporal characteristics of dust phenomena in the Urmia Basin using MERRA-2 data and observational data from Tabriz, Urmia, Sarab, and Mahabad over a 30-year period (1990–2019). The findings reveal that despite several fluctuations, the annual number of dusty days increased from the 1990s to the 2010s in the Urmia Basin. The maximum number of dusty days was found to predominantly occur in May (spring) and October (autumn), driven by two distinct mechanisms. In early autumn, developing synoptic systems associated with increased wind speeds can cause dust emission from dry land sources. Consequently, an increase in dust wet deposition, precipitation, dust surface concentration, and the number of dusty days occurs in October. In contrast, a sharp decrease in precipitation from April to May leads to drying soil and dust emission in May. Among the studied cities, Tabriz experienced the highest number of dusty days (728) due to the combined effects of cross-border and local dust sources. The highest dust column density and dust dry deposition in the south and east of Urmia Lake indicate the impact of declining water levels, which resulted in a dry lakebed as the primary local dust source. The MERRA-2 spatial distribution reveals that dust surface concentration, and the number of dusty days decrease similarly from the southwest to the northeast of the Urmia Basin as the distance from cross-border dust sources increases. A positive correlation is observed between the number of dusty days and MEERA-2 data, including dust surface concentration, dust dry deposition, column mass dust, and total aerosol extinction, with coefficients of 0.74, 0.71, 0.69, and 0.68, respectively.https://www.mdpi.com/2073-4433/14/12/1761Urmia BasinMERRA-2dust surface mass concentrationdust dry depositiondusty days
spellingShingle Elham Mobarak Hassan
Ebrahim Fattahi
Maral Habibi
Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
Atmosphere
Urmia Basin
MERRA-2
dust surface mass concentration
dust dry deposition
dusty days
title Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
title_full Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
title_fullStr Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
title_full_unstemmed Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
title_short Temporal and Spatial Variability of Dust in the Urmia Basin, 1990–2019
title_sort temporal and spatial variability of dust in the urmia basin 1990 2019
topic Urmia Basin
MERRA-2
dust surface mass concentration
dust dry deposition
dusty days
url https://www.mdpi.com/2073-4433/14/12/1761
work_keys_str_mv AT elhammobarakhassan temporalandspatialvariabilityofdustintheurmiabasin19902019
AT ebrahimfattahi temporalandspatialvariabilityofdustintheurmiabasin19902019
AT maralhabibi temporalandspatialvariabilityofdustintheurmiabasin19902019