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Influences of relative humidity and Indian monsoon precipitation on leaf water stable isotopes from the southeastern Tibetan Plateau
Author(s) -
Yu Wusheng,
Xu Baiqing,
Lai ChunTa,
Ma Yaoming,
Tian Lide,
Qu Dongmei,
Zhu Zhiyong
Publication year - 2014
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2014gl062004
Subject(s) - precipitation , relative humidity , plateau (mathematics) , monsoon , environmental science , wet season , east asian monsoon , humidity , stable isotope ratio , dry season , atmospheric sciences , hydrology (agriculture) , climatology , geology , geography , biology , ecology , mathematical analysis , physics , mathematics , geotechnical engineering , quantum mechanics , meteorology
This project report results of the first leaf water δ 18 O and δD time series of the woody plant Quercus aquifolioides undertaken on the southeastern Tibetan Plateau (STP). The data show that δD of leaf water underwent less enrichment than δ 18 O relative to precipitation and soil water, and could “inherit” the δD value characteristics of precipitation far better than δ 18 O. The leaf water δD values were strongly modified by evaporative enrichment in response to lower and more drastically changing relative humidity observed outside of the rainy season. In comparison, leaf water δD values more closely tracked those observed in the monsoon precipitation (acted as source water) in the rainy season. Our findings suggest that leaf water δD values from the STP were sensitive to the Indian monsoon activities, and the effects of relative humidity and the Indian monsoon precipitation should be considered for stable isotopes in tree ring cellulose or other biomarkers studies on the STP.