Sand and dust storm trajectories from Iraq Mesopotamian flood plain to Kuwait

Although Kuwait is greatly impacted by sand and dust storms (SDS) from Southern Iraq, to date little is known about the nature of these storms. Kuwait is vulnerable to SDS trajectories from the middle Euphrates region, specifically, from two “hot spot” areas (Al-Batha and Mamlahat Al-Samawah) of 455...

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Veröffentlicht in:The Science of the total environment 2020-03, Vol.710, p.136291-136291, Article 136291
Hauptverfasser: Al-Hemoud, Ali, Al-Dousari, Ali, Al-Dashti, Hassan, Petrov, Peter, Al-Saleh, Abeer, Al-Khafaji, Sarhan, Behbehani, Weam, Li, Jing, Koutrakis, Petros
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container_title The Science of the total environment
container_volume 710
creator Al-Hemoud, Ali
Al-Dousari, Ali
Al-Dashti, Hassan
Petrov, Peter
Al-Saleh, Abeer
Al-Khafaji, Sarhan
Behbehani, Weam
Li, Jing
Koutrakis, Petros
description Although Kuwait is greatly impacted by sand and dust storms (SDS) from Southern Iraq, to date little is known about the nature of these storms. Kuwait is vulnerable to SDS trajectories from the middle Euphrates region, specifically, from two “hot spot” areas (Al-Batha and Mamlahat Al-Samawah) of 4550 km2 located 250 km from its northern border. This study explores the transboundary SDS jets originating from Southern Iraq using Moderate Resolution Imaging Spectroradiometer (MODIS) images obtained from Aqua and Terra satellites over a twelve-year period (2007–2018). Furthermore, an analysis of a 5-day diurnal variation (two days prior, the day of the SDS occurrence, and two days after) explored the hourly patterns of visibility and wind speed, as well as grain size distribution of soil samples to better understand grain size compositions and sediment transport mechanisms. Satellite images confirmed that dust storm jets originated from the “hot spot” in southern Iraq and spread over Kuwait and extended to neighboring Arab Gulf countries as far as Bahrain (900 km) and Qatar (1200 km). In general, the highest wind speed and lowest visibility values were recorded in Northern of Kuwait, with suspended dust sustained for two days following the dust storm. The largest silt and clay fractions (grains ≤63 μm) were identified at the center and west Sabkha region of the “hot spot” area. Very fine sand particles (63–250 μm) were identified within the crescent sand dunes (Barchans) and artificial sand dunes (Al-Fajr). It is recommended that sustainable rehabilitation and land restoration of the “hot spot” area will result in the elimination of the long-range transport of SDS jet streams affecting the downwind Gulf countries. [Display omitted] •Severe sand and dust storm (SDS) trajectories traveled from the source and crossed over three countries.•The use of high spatial resolution MODIS Aqua and Terra satellite images is important to delineate the SDS sources.•Suspended dust was sustained for two days following the severe dust storms.•Understanding the genesis of the dust storms is critical to mitigation efforts.
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Kuwait is vulnerable to SDS trajectories from the middle Euphrates region, specifically, from two “hot spot” areas (Al-Batha and Mamlahat Al-Samawah) of 4550 km2 located 250 km from its northern border. This study explores the transboundary SDS jets originating from Southern Iraq using Moderate Resolution Imaging Spectroradiometer (MODIS) images obtained from Aqua and Terra satellites over a twelve-year period (2007–2018). Furthermore, an analysis of a 5-day diurnal variation (two days prior, the day of the SDS occurrence, and two days after) explored the hourly patterns of visibility and wind speed, as well as grain size distribution of soil samples to better understand grain size compositions and sediment transport mechanisms. Satellite images confirmed that dust storm jets originated from the “hot spot” in southern Iraq and spread over Kuwait and extended to neighboring Arab Gulf countries as far as Bahrain (900 km) and Qatar (1200 km). In general, the highest wind speed and lowest visibility values were recorded in Northern of Kuwait, with suspended dust sustained for two days following the dust storm. The largest silt and clay fractions (grains ≤63 μm) were identified at the center and west Sabkha region of the “hot spot” area. Very fine sand particles (63–250 μm) were identified within the crescent sand dunes (Barchans) and artificial sand dunes (Al-Fajr). It is recommended that sustainable rehabilitation and land restoration of the “hot spot” area will result in the elimination of the long-range transport of SDS jet streams affecting the downwind Gulf countries. 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In general, the highest wind speed and lowest visibility values were recorded in Northern of Kuwait, with suspended dust sustained for two days following the dust storm. The largest silt and clay fractions (grains ≤63 μm) were identified at the center and west Sabkha region of the “hot spot” area. Very fine sand particles (63–250 μm) were identified within the crescent sand dunes (Barchans) and artificial sand dunes (Al-Fajr). It is recommended that sustainable rehabilitation and land restoration of the “hot spot” area will result in the elimination of the long-range transport of SDS jet streams affecting the downwind Gulf countries. 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subjects Dust storms
Iraq
Kuwait
Mesopotamia
Sand dunes
title Sand and dust storm trajectories from Iraq Mesopotamian flood plain to Kuwait
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