Atmospheric water vapor and soil moisture jointly determine the spatiotemporal variations of CO2 fluxes and evapotranspiration across the Qinghai-Tibetan Plateau grasslands
- 1 October 2021
- journal article
- research article
- Published by Elsevier in Science of The Total Environment
- Vol. 791, 148379
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Energy flux partitioning and evapotranspiration in a sub‐alpine spruce forest ecosystemHydrological Processes, 2013
- Energy and surface moisture seasonally limit evaporation and sublimation from snow-free alpine tundraAgricultural and Forest Meteorology, 2012
- Soil Respiration in Tibetan Alpine Grasslands: Belowground Biomass and Soil Moisture, but Not Soil Temperature, Best Explain the Large-Scale PatternsPLOS ONE, 2012
- CO2 fluxes and their driving factors over alpine meadow grassland ecosystems in the northern shore of Qinghai Lake, ChinaChinese Journal of Plant Ecology, 2012
- Nonlinear controls on evapotranspiration in arctic coastal wetlandsBiogeosciences, 2011
- Partitioning of evapotranspiration and its controls in four grassland ecosystems: Application of a two-source modelAgricultural and Forest Meteorology, 2009
- A working guide to boosted regression treesJournal of Animal Ecology, 2008
- Leaf area controls on energy partitioning of a temperate mountain grasslandBiogeosciences, 2008
- Temperature and biomass influences on interannual changes in CO2 exchange in an alpine meadow on the Qinghai‐Tibetan PlateauGlobal Change Biology, 2006
- Comparative study of the net exchange of CO2 in 3 types of vegetation ecosystems on the Qinghai-Tibetan PlateauChinese Science Bulletin, 2005