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Water household changes, climate change, and human impact – reasons for the dusty side of the Aral Sea Syndrome

Christian OppUniversity of Marburg, Department of Geography, 35037 Marburg, GermanyMichael GrollUniversity of Marburg, Department of Geography, 35037 Marburg, GermanyOleg SemenovLyudmila ShardakovaHydrometeorological Research Institute (HRMI), 100052 Tashkent, UzbekistanYulia A. KovalevskayaHydrometeorological Research Institute (HRMI), 100052 Tashkent, UzbekistanRashid KulmatovNational University of Uzbekistan, 100174 Tashkent, UzbekistanI. Sh. NormatovInstitute of Water Problems, Hydropower and Ecology, Academy of Science, Republic of Tajikistan, 734002 Dushanbe, TajikistanIlhom AslanovNational Research University, Tashkent Institute of Irrigation and Agricultural Mechanization Engineers, Tashkent, Uzbekistan
E3S Web of Conferencesjournal2024en
ABI

Аннотация

The reduced water input into lakes and riverbeds is an initial reason for desiccated water bodies and their lacustrine and fluvial sediments. Under arid and semi-arid and even continental climate these dry sediments are a very important source of sand and dust storms (SDS) besides sources from deserts. These natural prerequisites, the ongoing climate change and predominately the land use caused water withdrawal from the main tributaries Amudarya and Syrdarya are the main reasons for the acceleration of SDS in the Aral Sea region. Long-term dust analyses between 2003 and 2012 have identified the deserts Karakum, Kyzylkum and the new desert Aralkum as the main source areas for SDS in the Turan Lowlands. Among the atmospheric dust and dusty depositions salty aerosols respectively sediments were identified. The Aral Sea Syndrome and its effects affect ecosystems, animals, plants and people. A case study from Kazakhstan showed that children are more affected by near-surface sand and dust storms than adults.

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