Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Changliang Yin"'
Publikováno v:
Hydrological Processes. 22:3386-3392
The use of stable isotopes is a practical tool in the study of the lake water budget. This is an one way to study the hydrological cycle in the large numbers of inland lakes on the Tibetan Plateau, in which the isotope record of the sediment is belie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e99d2c4140bdd2f8a398852cff01234
https://doi.org/10.1002/hyp.6919
https://doi.org/10.1002/hyp.6919
Autor:
Yu Wang, ZhongPing Zhao, LingLong Ma, Zhongfang Liu, Changliang Yin, Lide Tian, Wusheng Yu, Wei Tang
Publikováno v:
Science in China Series D: Earth Sciences. 51:1121-1128
Precipitation δ 18O at Yushu, eastern Tibetan Plateau, shows strong fluctuation and lack of clear seasonality. The seasonal pattern of precipitation stable isotope at Yushu is apparently different from either that of the southwest monsoon region to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66d5c8244b000658404eedda81e8a9c0
https://doi.org/10.1007/s11430-008-0089-1
https://doi.org/10.1007/s11430-008-0089-1
Publikováno v:
Science in China Series D: Earth Sciences. 51:966-975
Oxygen stable isotope of atmospheric water vapor is widely used to study the modern process of climate. Atmospheric water vapor samples were collected at Dlingha, northeast of Tibetan Plateau during the period from July 2005 to February 2006. The var
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5669ad5ab772a145f7f0216f23851a30
https://doi.org/10.1007/s11430-008-0076-6
https://doi.org/10.1007/s11430-008-0076-6
Publikováno v:
Frontiers of Earth Science in China. 2:49-57
The relationship between the variation of δ 18O in precipitation in Yarlungzangbo River basin and the moisture flux was analyzed with NCEP/NCAR reanalysis grid data and δ 18O in precipitation at four stations (Lazi, Nugesha, Yangcun and Nuxia) of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f39cd8797b7f2325b54254ded618f856
https://doi.org/10.1007/s11707-008-0012-2
https://doi.org/10.1007/s11707-008-0012-2
Publikováno v:
Hydrological Processes; 8/15/2008, Vol. 22 Issue 17, p3386-3392, 7p, 5 Charts, 5 Graphs, 1 Map