Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Gafurov, Abror"'
Autor:
Gafurov, Abror, Selyuzhenok, Valeria, Latinovic, Milena, Apel, Heiko, Mamaraimov, Adkham, Salokhiddinov, Abdulkhakim, Boergens, Eva, Güntner, Andreas
Publikováno v:
In Journal of Hydrology: Regional Studies December 2024 56
Autor:
Akbari, Mahdi, Mirchi, Ali, Roozbahani, Amin, Gafurov, Abror, Kløve, Bjørn, Haghighi, Ali Torabi
Publikováno v:
In Journal of Great Lakes Research August 2022 48(4):876-889
Autor:
Umirbekov, Atabek, Peña-Guerrero, Mayra Daniela, Didovets, Iulii, Apel, Heiko, Gafurov, Abror, Müller, Daniel
Publikováno v:
Hydrology & Earth System Sciences Discussions; 7/26/2024, p1-19, 19p
Publikováno v:
In Water Security August 2020 10
Autor:
He, Zhihua, Unger-Shayesteh, Katy, Vorogushyn, Sergiy, Weise, Stephan M., Kalashnikova, Olga, Gafurov, Abror, Duethmann, Doris, Barandun, Martina, Merz, Bruno
Publikováno v:
In Journal of Hydrology April 2019 571:332-348
Autor:
Gafurov, Abror, Mamaraimov, Adkham
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Snow is an important hydrological component in Central Asia. The snowmelt contributes to more than 50 % of total water formation in the region. Many hydro-meteorological phenomena such as floods or droughts can be triggered by snowmelt amounts in Cen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b9f9bd199c4831e75fcaf8cf1c1939b
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020658
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020658
Akademický článek
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Autor:
Unger-Shayesteh, Katy, Vorogushyn, Sergiy, Farinotti, Daniel, Gafurov, Abror, Duethmann, Doris, Mandychev, Alexander, Merz, Bruno
Publikováno v:
In Global and Planetary Change November 2013 110 Part A:4-25
Autor:
Kriegel, David, Mayer, Christoph, Hagg, Wilfried, Vorogushyn, Sergiy, Duethmann, Doris, Gafurov, Abror, Farinotti, Daniel
Publikováno v:
In Global and Planetary Change November 2013 110 Part A:51-61
Discharge as an integrated representation of all hydrological processes is the most common response variable used in sensitivity analyses. However, due to overlaying effects of all hydrological processes, the sensitivity signal of certain parameters
Externí odkaz:
http://hdl.handle.net/10150/622888
http://arizona.openrepository.com/arizona/handle/10150/622888
http://arizona.openrepository.com/arizona/handle/10150/622888