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| Content Provider | Springer Nature Link |
|---|---|
| Author | Li, Zhen Yao, Tandong Tian, Lide Xu, Baiqing Wu, Guangjian |
| Copyright Year | 2006 |
| Abstract | Expeditions to Muztagata (in the eastern Pamirs) during the summer seasons of 2002 and 2003 collected precipitation samples and measured their oxygen isotopes. The δ $^{18}$O in precipitation displays a wide range, varying from −17.40‰ to +1.33‰ in June-September 2002 and from −22.31‰ to +4.59‰ in May-August 2003. The δ $^{18}$O in precipitation correlates with the initial temperature of precipitation during the observing periods. The positive correlation between δ $^{18}$O and temperature suggests that δ $^{18}$O can be used as an indicator of temperature in this region. The δ $^{18}$O values in fresh-snow samples collected from two snow events at different elevations on the Muztagata Glacier show a strong “altitude effect”, with a ratio of nearly −0.40% per 100 m from 5500 m to 7450 m. |
| Starting Page | 36 |
| Ending Page | 42 |
| Page Count | 7 |
| File Format | |
| ISSN | 10069313 |
| Journal | Science in China Series D: Earth Sciences |
| Volume Number | 49 |
| Issue Number | 1 |
| Language | English |
| Publisher | Science in China Press |
| Publisher Date | 2006-01-01 |
| Publisher Place | Beijing |
| Access Restriction | Subscribed |
| Subject Keyword | Muztagata δ $^{18}$O temperature altitude effect Geosciences |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences |
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