Relationship between the 0 ℃ Layer Height and the Streamflow of the Urumqi River in the Period of Spring Snowmelt-Reference-Cited by-同舟云学术

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Relationship between the 0 ℃ Layer Height and the Streamflow of the Urumqi River in the Period of Spring Snowmelt

Published:2010-03-18 Issue:1 Volume:27 Page:69-74
ISSN:1001-4675
Container-title:Arid Zone Research
language:en
Short-container-title:Arid Zone Research

Author:

GONG Heng-rui,SHI Yu,FENG Zhi-min

Publisher

China Science Publishing & Media Ltd.

Subject

Atmospheric Science,Geology,Environmental Science (miscellaneous),Water Science and Technology,Ecology

Cited by 4 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Climate change and runoff response based on isotope analysis in an arid mountain watershed of the western Kunlun Mountains;Hydrological Sciences Journal;2016-10-03

2. Spatio-temporal changes in free-air freezing level heights in Northwest China, 1960–2012;Quaternary International;2013-11

3. Characteristics of melt water discharge in the Glacier No. 1 basin, headwater of Urumqi River;Journal of Hydrology;2013-05

4. Response of runoff to change of atmospheric 0°C level height in summer in arid region of Northwest China;Science China Earth Sciences;2012-07-17

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