Articles | Volume 24, issue 21
https://doi.org/10.5194/acp-24-12203-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-12203-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Nov 2024
Research article |
| 04 Nov 2024
| 04 Nov 2024
Precipitation in the mountains of Central Asia: isotopic composition and source regions
Zarina Saidaliyeva
CORRESPONDING AUTHOR
Department of Geography and Environmental Science, University of Reading, Reading, RG6 6AB, UK
Maria Shahgedanova
Department of Geography and Environmental Science, University of Reading, Reading, RG6 6AB, UK
Vadim Yapiyev
Department of Geography and Environmental Science, University of Reading, Reading, RG6 6AB, UK
School of Mining and Geosciences, Nazarbayev University, Astana, 010000, Kazakhstan
Andrew John Wade
Department of Geography and Environmental Science, University of Reading, Reading, RG6 6AB, UK
Fakhriddin Akbarov
Centre of Glacial Geology, Institute of Geology and Geophysics, Tashkent, 100164, Uzbekistan
Mukhammed Esenaman uulu
Central Asian Institute for Applied Geosciences, Bishkek, 720027, Kyrgyzstan
Olga Kalashnikova
Central Asian Institute for Applied Geosciences, Bishkek, 720027, Kyrgyzstan
Vassiliy Kapitsa
Central Asian Regional Glaciological Centre under the auspices of UNESCO, Almaty, 050010, Kazakhstan
Nikolay Kasatkin
Central Asian Regional Glaciological Centre under the auspices of UNESCO, Almaty, 050010, Kazakhstan
Ilkhomiddin Rakhimov
Institute of Water Problems, Hydropower and Ecology, Dushanbe, 734025, Tajikistan
Rysbek Satylkanov
Tien Shan High Mountain Research Center, Bishkek, 720033, Kyrgyzstan
Daniiar Sayakbaev
Tien Shan High Mountain Research Center, Bishkek, 720033, Kyrgyzstan
Eleonora Semakova
Ulugh Beg Astronomical Institute, Academy of Sciences of Uzbekistan, Tashkent, 100052, Uzbekistan
Igor Severskiy
Central Asian Regional Glaciological Centre under the auspices of UNESCO, Almaty, 050010, Kazakhstan
Maxim Petrov
Centre of Glacial Geology, Institute of Geology and Geophysics, Tashkent, 100164, Uzbekistan
Gulomjon Umirzakov
National University of Uzbekistan, Tashkent, 100174, Uzbekistan
Hydrometeorological Research Institute, Tashkent, 100052, Uzbekistan
Ryskul Usubaliev
Central Asian Institute for Applied Geosciences, Bishkek, 720027, Kyrgyzstan
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The Cryosphere, 19, 6591–6628, https://doi.org/10.5194/tc-19-6591-2025, https://doi.org/10.5194/tc-19-6591-2025, 2025
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This study provides a comprehensive geophysical dataset on permafrost in the data-scarce Tien Shan and Pamir mountain regions of Central Asia. It also introduces a novel modeling method to quantify ground ice content across different landforms. The findings indicate that this approach is well suited for characterizing ice-rich permafrost, which is crucial for evaluating future water availability and assessing risks associated with thawing permafrost.
Horst Machguth, Anja Eichler, Margit Schwikowski, Sabina Brütsch, Enrico Mattea, Stanislav Kutuzov, Martin Heule, Ryskul Usubaliev, Sultan Belekov, Vladimir N. Mikhalenko, Martin Hoelzle, and Marlene Kronenberg
The Cryosphere, 18, 1633–1646, https://doi.org/10.5194/tc-18-1633-2024, https://doi.org/10.5194/tc-18-1633-2024, 2024
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In 2018 we drilled an 18 m ice core on the summit of Grigoriev ice cap, located in the Tien Shan mountains of Kyrgyzstan. The core analysis reveals strong melting since the early 2000s. Regardless of this, we find that the structure and temperature of the ice have changed little since the 1980s. The probable cause of this apparent stability is (i) an increase in snowfall and (ii) the fact that meltwater nowadays leaves the glacier and thereby removes so-called latent heat.
Youping Chen, Magdalena Opała-Owczarek, Feng Chen, Piotr Owczarek, Heli Zhang, Shijie Wang, Mao Hu, Rysbek Satylkanov, Bakytbek Ermenbaev, Bakhtiyorov Zulfiyor, Huaming Shang, and Ruibo Zhang
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2022-329, https://doi.org/10.5194/hess-2022-329, 2022
Preprint withdrawn
Short summary
Short summary
Mountain precipitation is an important force driving the cycles of the cryosphere, biosphere and hydrosphere in arid Central Asia. This driving force has broad coherence in spatiotemporal variation, with periodic cycles and decadal shifts caused by the North Atlantic Oscillation and the El Niño-Southern Oscillation. In the future, the increase of precipitation will delay the impact of the sharp rise in temperature on the melting of glacier mass balance.
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Short summary
Ratios of stable isotopes of oxygen and hydrogen in precipitation are used to trace source regions and pathways of atmospheric moisture. A database of these measurements was developed for the mountains of Central Asia and analysed in the context of atmospheric trajectories. Over 50 % of precipitation was formed from moisture re-evaporated from regional terrestrial sources including the irrigated land in the Aral Sea basin, highlighting its support of the water tower function of the mountains.
Ratios of stable isotopes of oxygen and hydrogen in precipitation are used to trace source...
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