Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan

Global climate change can have a significant impact on the development and sustainability of agricultural production. Climate scenarios indicate that an expected increase in air temperature in semiarid Uzbekistan can lead to an increase in evapotranspiration from agricultural fields, an increase in...

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Main Authors: Ahmad Hamidov, Javlonbek Ishchanov, Mukhamadkhan Khamidov
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Agronomy
Subjects:
Online Access:https://www.mdpi.com/2073-4395/10/8/1173
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spelling doaj-ee4b10891458416484da44b661a948fe2021-04-02T14:23:44ZengMDPI AGAgronomy2073-43952020-08-01101173117310.3390/agronomy10081173Impact of Climate Change on Groundwater Management in the Northwestern Part of UzbekistanAhmad Hamidov0Javlonbek Ishchanov1Mukhamadkhan Khamidov2Leibniz Centre for Agricultural Landscape Research (ZALF), Eberswalder Straße 84, 15374 Müncheberg, GermanyTashkent Institute of Irrigation and Agricultural Mechanization Engineers (TIIAME), Kary-Niyaziy 39, Tashkent 100000, UzbekistanTashkent Institute of Irrigation and Agricultural Mechanization Engineers (TIIAME), Kary-Niyaziy 39, Tashkent 100000, UzbekistanGlobal climate change can have a significant impact on the development and sustainability of agricultural production. Climate scenarios indicate that an expected increase in air temperature in semiarid Uzbekistan can lead to an increase in evapotranspiration from agricultural fields, an increase in irrigation water requirements, and a deterioration in the ameliorative status of irrigated lands. The long-term mismanagement of irrigation practices and poor conditions of drainage infrastructure have led to an increase in the water table and its salinization level in the northwestern part of Uzbekistan. This article presents the results of an analysis of the amelioration of irrigated lands in the Khorezm region of Uzbekistan as well as the modeling of the dynamics of water table depths and salinity levels using the Mann–Kendall trend test and linear regression model. The study estimated the water table depths and salinity dynamics under the impact of climate change during 2020–2050 and 2050–2100. The results show that the water table depths in the region would generally decrease (from 1.72 m in 2050 to 1.77 m by 2100 based on the Mann–Kendall trend test; from 1.75 m in 2050 to 1.79 m by 2100 according to the linear regression model), but its salinity level would increase (from 1.72 g·L<sup>−1</sup> in 2050 to 1.85 g·L<sup>−1</sup> by 2100 based on the Mann–Kendall trend test; from 1.97 g·L<sup>−1</sup> in 2050 to 2.1 g·L<sup>−1</sup> by 2100 according to the linear regression model). The results of the study provide insights into the groundwater response to climate change and assist authorities in better planning management strategies for the region.https://www.mdpi.com/2073-4395/10/8/1173groundwatermineralizationMann–Kendall trend testlinear regressionirrigated agricultureKhorezm
collection DOAJ
language English
format Article
sources DOAJ
author Ahmad Hamidov
Javlonbek Ishchanov
Mukhamadkhan Khamidov
spellingShingle Ahmad Hamidov
Javlonbek Ishchanov
Mukhamadkhan Khamidov
Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
Agronomy
groundwater
mineralization
Mann–Kendall trend test
linear regression
irrigated agriculture
Khorezm
author_facet Ahmad Hamidov
Javlonbek Ishchanov
Mukhamadkhan Khamidov
author_sort Ahmad Hamidov
title Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
title_short Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
title_full Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
title_fullStr Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
title_full_unstemmed Impact of Climate Change on Groundwater Management in the Northwestern Part of Uzbekistan
title_sort impact of climate change on groundwater management in the northwestern part of uzbekistan
publisher MDPI AG
series Agronomy
issn 2073-4395
publishDate 2020-08-01
description Global climate change can have a significant impact on the development and sustainability of agricultural production. Climate scenarios indicate that an expected increase in air temperature in semiarid Uzbekistan can lead to an increase in evapotranspiration from agricultural fields, an increase in irrigation water requirements, and a deterioration in the ameliorative status of irrigated lands. The long-term mismanagement of irrigation practices and poor conditions of drainage infrastructure have led to an increase in the water table and its salinization level in the northwestern part of Uzbekistan. This article presents the results of an analysis of the amelioration of irrigated lands in the Khorezm region of Uzbekistan as well as the modeling of the dynamics of water table depths and salinity levels using the Mann–Kendall trend test and linear regression model. The study estimated the water table depths and salinity dynamics under the impact of climate change during 2020–2050 and 2050–2100. The results show that the water table depths in the region would generally decrease (from 1.72 m in 2050 to 1.77 m by 2100 based on the Mann–Kendall trend test; from 1.75 m in 2050 to 1.79 m by 2100 according to the linear regression model), but its salinity level would increase (from 1.72 g·L<sup>−1</sup> in 2050 to 1.85 g·L<sup>−1</sup> by 2100 based on the Mann–Kendall trend test; from 1.97 g·L<sup>−1</sup> in 2050 to 2.1 g·L<sup>−1</sup> by 2100 according to the linear regression model). The results of the study provide insights into the groundwater response to climate change and assist authorities in better planning management strategies for the region.
topic groundwater
mineralization
Mann–Kendall trend test
linear regression
irrigated agriculture
Khorezm
url https://www.mdpi.com/2073-4395/10/8/1173
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