Response of Ecosystem Productivity to High Vapor Pressure Deficit and Low Soil Moisture: Lessons Learned From the Global Eddy‐Covariance Observations

Author:

Xu Shiqin123ORCID,Gentine Pierre4ORCID,Li Lingcheng5ORCID,Wang Lixin6ORCID,Yu Zhongbo78ORCID,Dong Ningpeng9ORCID,Ju Qin78,Zhang Yuliang10

Affiliation:

1. Now at Hydrology, Agriculture and Land Observation (HALO) Laboratory, Division of Biological and Environmental Science and Engineering King Abdullah University of Science and Technology Thuwal Saudi Arabia

2. College of Geography and Environmental Science Northwest Normal University Lanzhou PR China

3. Key Laboratory of Resource Environment and Sustainable Development of Oasis Lanzhou PR China

4. Department of Earth and Environmental Engineering Columbia University NY New York USA

5. Atmosphere Sciences and Global Change Division Pacific Northwest National Laboratory WA Seattle USA

6. Department of Earth Science Indiana University‐Purdue University Indianapolis IN Indianapolis USA

7. National Key Laboratory of Water Disaster Prevention Hohai University Nanjing PR China

8. College of Hydrology and Water Resources Hohai University Nanjing PR China

9. State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin China Institute of Water Resources and Hydropower Research Beijing PR China

10. School of Civil Engineering Hefei University of Technology Hefei PR China

Abstract

AbstractAlthough there is mounting concern about how high vapor pressure deficit (VPD) and low soil moisture (SM) affect ecosystem productivity, their relative importance is still under debate. Here, we comprehensively quantified the relative impacts of these two factors on ecosystem gross primary production (GPP) using observations from a global network of eddy‐covariance towers and two approaches (sensitivity analysis and linear regression model). Both approaches agree that a higher percentage of sites experience GPP reduction from high VPD than from low SM over the growing season. However, the constraint of high VPD and low SM on GPP reduction is tightly linked with climates and plant functional types. Humid and mesic ecosystems including forests and grasslands are dominated by VPD, while the semi‐arid and arid ecosystems including shrublands and savannas are dominated by SM. The varying dominant role of these two factors on GPP is closely related to plant stomatal behavior, as predicted by a stomatal conductance model. Additionally, we highlight the non‐linear impact of SM on GPP during droughts and the possible underestimation of the SM effects for deep‐rooted plants when only using surface‐layer SM. Our results shed light on a better understanding of the impacts of VPD and SM on vegetation productivity, with important implications for modeling the response and feedback of ecosystem dynamics to current and future climates.

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),General Environmental Science

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