Dew formation and its long-term trend in a desert riparian forest ecosystem on the eastern edge of the taklimakan desert in China

Journal of Hydrology

Volumn 472-473, Issue , 2012, Pages 90-98

  Hao, Xing Ming ^a   Li, Cong ^b   Guo, Bin ^a   Ma, Jian Xin ^a   Ayup, Mubarek ^a   Chen, Zhong Sheng ^a  

^a XINJIANG INSTITUTE OF ECOLOGY AND GEOGRAPHY   (China)

^b Xinjiang Climate Center   (China)

Author keywords

Canopy condensation; Dewfall; Eddy covariance; Long term trend; Meteorological factors

Indexed keywords

ANNUAL RAINFALL; DESERT ECOSYSTEM; DEW FORMATION; DEWFALL; DIFFERENT TIME SCALE; EASTERN EDGE; EDDY COVARIANCE; EDDY COVARIANCE SYSTEMS; LONG-TERM TREND; METEOROLOGICAL FACTORS; OBSERVATION PERIOD; OBSERVATIONAL DATA; POPULUS; QUANTITATIVE CHARACTERISTICS; RIPARIAN FORESTS; SOIL SURFACES; SOIL WATER CONTENT; TAKLIMAKAN DESERT; TOP SOILS; WATER BALANCE; WEATHER STATIONS;

ARID REGIONS; FORESTRY; RAIN; SOIL MOISTURE; WATER RESOURCES;

LANDFORMS;

CONDENSATION; DESERT; DEW; EDDY COVARIANCE; FOREST CANOPY; FOREST ECOSYSTEM; LONG-TERM CHANGE; METEOROLOGY; RAINFALL; REGIONAL CLIMATE; RIPARIAN FOREST; WATER BUDGET; WATER RESOURCE; WEATHER STATION;

CHINA; DESERTS; FOREST CANOPY; METEOROLOGY; MOISTURE CONTENT; RAIN; SOIL; WATER RESOURCES;

CHINA; TAKLIMAKAN DESERT; XINJIANG UYGUR;

POPULUS;

EID: 84868301264     PISSN: 00221694     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jhydrol.2012.09.015     Document Type: Article

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