Spatiotemporal variability of dust storm source susceptibility during wet and dry periods: The Tigris-Euphrates River Basin

被引:4
|
作者
Naghibi, Amir [1 ,2 ]
Hashemi, Hossein [1 ,2 ]
Zhao, Pengxiang [1 ,3 ]
Brogaard, Sara [1 ,4 ]
Eklund, Lina [1 ,3 ]
Hassan, Hussein Hamid [5 ]
Mansourian, Ali [1 ,3 ,6 ]
机构
[1] Lund Univ, Fac Social Sci, Ctr Adv Middle Eastern Studies, Lund, Sweden
[2] Lund Univ, Div Water Resources Engn, Fac Engn, Lund, Sweden
[3] Lund Univ, Fac Sci, GIS Ctr, Dept Phys Geog & Ecosyst Sci, Lund, Sweden
[4] Lund Univ, Fac Social Sci, Ctr Sustainabil Studies, Lund, Sweden
[5] Univ Duhok, Coll Spatial Planning, Dept Spatial Planning, Duhok, Iraq
[6] Lund Univ, Nat Based Future Solut Profile Area, Lund, Sweden
关键词
Dust storm source; Middle east; Climate; Random forests; Spatiotemporal modeling; WIND-TUNNEL; TEMPORAL VARIATIONS; RANDOM FORESTS; SAND; CLASSIFICATION; IDENTIFICATION; ERODIBILITY; FREQUENCY; EMISSIONS; EXPOSURE;
D O I
10.1016/j.apr.2023.101953
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study develops a framework for spatiotemporal modeling of dust storm source susceptibility in a critical case study, the Tigris-Euphrates River Basin, as a significant source of dust storms in the Middle East. The study period was divided into four periods, 2000-2004 (hydrological dry year), 2005-2007 (hydrological wet year), 2008-2012 (hydrological dry year), and 2013-2021 (hydrological wet year) representing hydrological condi-tions in the study area. Initially, visual interpretations of true color composites of the MODIS satellite images were conducted to spot dust storm sources in the studied periods. Topographical, hydrological, soil texture, and vegetation health datasets were prepared to model dust storm source susceptibility in each period. The random forest algorithm was implemented on the four study periods' datasets. For each period, 70% of dust and non-dust storm sources and conditioning factors were used for training the models. The models were then validated using the validation datasets (remaining 30%), and the importance of the variables was determined for each study period. In the 2008-2012 period, experiencing an extensive drought in the region, a higher number of dust storm sources were detected, and 383 locations (pixels) in the area were considered highly susceptible to dust storm sources. In all study periods, as well as in the ensemble model (integrating the results of four study periods into one overall model), high susceptibility to dust storms was detected in areas where lakes and marshlands had dried up due to climate factors, inappropriate water management strategies, and land use policies. The results also depicted that elevation, wind speed, precipitation, vegetation coverage, slope degree, distance from rivers, and soil texture had high impacts on the susceptibility of land to be a dust storm source.
引用
收藏
页数:11
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