scholarly journals Disentangling Climate and LAI Effects on Seasonal Variability in Water Use Efficiency Across Terrestrial Ecosystems in China

2018 ◽  
Vol 123 (8) ◽  
pp. 2429-2443 ◽  
Author(s):  
Yue Li ◽  
Hao Shi ◽  
Lei Zhou ◽  
Derek Eamus ◽  
Alfredo Huete ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Seasonal Variability ◽  
Terrestrial Ecosystems ◽  
Use Efficiency

scholarly journals How is water-use efficiency of terrestrial ecosystems distributed and changing on Earth?

2014 ◽  
Vol 4 (1) ◽  
Author(s):  
Xuguang Tang ◽  
Hengpeng Li ◽  
Ankur R. Desai ◽  
Zoltan Nagy ◽  
Juhua Luo ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Terrestrial Ecosystems ◽  
Use Efficiency

Characteristics of water use efficiency in terrestrial ecosystems and its influence factors in Ningxia Province

2019 ◽  
Vol 39 (24) ◽  
Author(s):  
宫菲 GONG Fei ◽  
杜灵通 DU Lingtong ◽  
孟晨 MENG Chen ◽  
丹杨 DAN Yang ◽  
王乐 WANG Le ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Influence Factors ◽  
Terrestrial Ecosystems ◽  
Use Efficiency

scholarly journals Responses of Water Use Efficiency to Drought in Southwest China

2020 ◽  
Vol 12 (1) ◽  
pp. 199 ◽  
Author(s):  
Jingxue Zhao ◽  
Tongren Xu ◽  
Jingfeng Xiao ◽  
Shaomin Liu ◽  
Kebiao Mao ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Southwest China ◽  
Vegetation Type ◽  
Terrestrial Ecosystems ◽  
Temporal Variations ◽  
Drought Severity ◽  
Enhancement Effect ◽  
Severe Drought ◽  
Use Efficiency

Water use efficiency (WUE) measures the tradeoff between carbon uptake and water consumption in terrestrial ecosystems. It remains unclear how the responses of WUE to drought vary with drought severity. We assessed the spatio-temporal variations of ecosystem WUE and its responses to drought for terrestrial ecosystems in Southwest China over the period 2000–2017. The annual WUE values varied with vegetation type in the region: Forests (3.25 gC kg−1H2O) > shrublands (2.00 gC kg−1H2O) > croplands (1.76 gC kg−1H2O) > grasslands (1.04 gC kg−1H2O). During the period 2000–2017, frequent droughts occurred in Southwest China, and overall, drought had an enhancement effect on WUE. However, the effects of drought on WUE varied with vegetation type and drought severity. Croplands were the most sensitive to drought, and slight water deficiency led to the decline of cropland WUE. Over grasslands, mild drought increased its WUE while moderate and severe drought reduced its WUE. For forests and shrublands, mild and moderate drought increased their WUE, and only severe drought reduce their WUE, indicating that these ecosystems had stronger resistance to drought. Assessing the patterns and trends of ecosystem WUE and its responses to drought are essential for understanding plant water use strategy and informing ecosystem water management.

Enhanced water use efficiency in global terrestrial ecosystems under increasing aerosol loadings

2017 ◽  
Vol 237-238 ◽  
pp. 39-49 ◽  
Author(s):  
Xiaoliang Lu ◽  
Min Chen ◽  
Yaling Liu ◽  
Diego G. Miralles ◽  
Faming Wang
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Terrestrial Ecosystems ◽  
Use Efficiency

scholarly journals Contrasting responses of water use efficiency to drought across global terrestrial ecosystems

2016 ◽  
Vol 6 (1) ◽  
Author(s):  
Yuting Yang ◽  
Huade Guan ◽  
Okke Batelaan ◽  
Tim R. McVicar ◽  
Di Long ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Terrestrial Ecosystems ◽  
Use Efficiency

scholarly journals Quantifying Soil Moisture Impacts on Water Use Efficiency in Terrestrial Ecosystems of China

2021 ◽  
Vol 13 (21) ◽  
pp. 4257
Author(s):  
Xingming Hao ◽  
Jingjing Zhang ◽  
Xue Fan ◽  
Haichao Hao ◽  
Yuanhang Li
Keyword(s):  
Soil Moisture ◽  
Water Use Efficiency ◽  
Water Use ◽  
Land Surface ◽  
Net Primary Production ◽  
Terrestrial Ecosystems ◽  
Sensitivity Coefficient ◽  
Analytical Framework ◽  
Average Value ◽  
Use Efficiency

Soil moisture (SM) significantly affects the exchange of land surface energy and the stability of terrestrial ecosystems. Although some conclusions have been drawn about the effects of SM on the ecosystem water use efficiency (WUE), the influence mechanism and the quantitative assessment framework of SM on WUE are still unclear. This study provides an analysis framework for the feedback relationship between SM and WUE based on the dependence of the evaporation fraction on SM and output datasets from remote sensing and the Global Land Data Assimilation System. The results show that the range of WUE of terrestrial ecosystems of China was0.02–19.26 g C/kg H2O in the growing season with an average value of 1.05 g C/kg H2O. They also show a downward trend in43.99% of the total area. In the evapotranspiration (ET) pathway, SM negatively affected WUE, and the sensitivity coefficient ranged from −18.49 to −0.04. In the net primary production (NPP) pathway, the sensitivity coefficient ranged from −68.66 to 43.19. Under the dual effects of the ET and NPP pathways, the influence of SM on WUE was negative in 84.62% of the area. Variation in SM led to significant WUE variability. Generally, the percentage change in WUE (ΔWUE) ranged from 0% to 190.86%, with an average value of 28.02%. The maximum ΔWUE ranged from 0% to 758.78%, with an average value of 109.29%. The WUE of forest ecosystems showed strong resistance to SM variation, whereas that of non-forest vegetation was more sensitive to SM variation. This analytical framework provides a new perspective on the feedback relationship between WUE and SM in terrestrial ecosystems.

AmazonFACE – Assessing the response of Amazon rainforest functioning to elevated atmospheric carbon dioxide concentrations

2020 ◽  
Author(s):  
Anja Rammig ◽  
Katrin Fleischer ◽  
Sabrina Garcia ◽  
Nathielly Martins ◽  
Juliane Menezes ◽  
...  
Keyword(s):  
Water Use Efficiency ◽  
Water Use ◽  
Carbon Sink ◽  
Global Climate ◽  
Terrestrial Ecosystems ◽  
Amazon Rainforest ◽  
Past Century ◽  
Sink Strength ◽  
Climate Conditions ◽  
Use Efficiency

<p>The rapid rise in atmospheric CO<sub>2</sub> concentration over the past century is unprecedented. It has unambiguously influenced Earth’s climate system and terrestrial ecosystems. Elevated atmospheric CO<sub>2</sub> concentrations (eCO<sub>2</sub>) have induced an increase in biomass and thus, a carbon sink in forests worldwide. It is assumed that eCO<sub>2</sub> stimulates photosynthesis and plant productivity and enhances water-use efficiency – the so-called CO<sub>2</sub>-fertilization effect, which may provide an important buffering effect for plants during adverse climate conditions. For these reasons, current global climate simulations consistently predict that tropical forests will continue to sequester more carbon in aboveground biomass, partially compensating human emissions and decelerating climate change by acting as a carbon sink. In contrast to model simulations, several lines of evidence point towards a decreasing carbon sink strength of the Amazon rainforest. Reliable predictions of eCO<sub>2</sub> effects in the Amazon rainforest are hindered by a lack of process-based information gained from ecosystem scale eCO<sub>2</sub> experiments. Here we report on baseline measurements from the Amazon Free Air CO<sub>2</sub> Enrichment (AmazonFACE) experiment and preliminary results from open-top chamber (OTC) experiments with eCO<sub>2</sub>. After three months of eCO<sub>2</sub>, we find that understory saplings increased carbon assimilation by 17% (under light saturated conditions) and water use efficiency by 39% in the OTC experiment. We present our main hypotheses for the FACE experiment, and discuss our expectations on the potential driving processes for limiting or stimulating the Amazon rainforest carbon sink under eCO<sub>2</sub>. We focus on possible effects of eCO<sub>2</sub> on carbon uptake and allocation, nutrient cycling, water-use and plant-herbivore interactions, which need to be implemented in dynamic vegetation models to estimate future changes of the Amazon carbon sink.</p>

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