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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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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