Soil moisture dominates dryness stress on ecosystem production globally

Laibao Liu,Dahe Qin,Mathias Hauser,Lukas Gudmundsson,Sonia I Seneviratne,Shuangcheng Li

doi:10.1038/s41467-020-18631-1

Laibao Liu, Dahe Qin + Show 4 more

Open Access

https://doi.org/10.1038/s41467-020-18631-1

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Journal: Nature Communications	Publication Date: Sep 29, 2020
Citations: 353	License type: open-access

Affiliation: ETH Zurich, Peking University

Abstract

Dryness stress can limit vegetation growth and is often characterized by low soil moisture (SM) and high atmospheric water demand (vapor pressure deficit, VPD). However, the relative role of SM and VPD in limiting ecosystem production remains debated and is difficult to disentangle, as SM and VPD are coupled through land-atmosphere interactions, hindering the ability to predict ecosystem responses to dryness. Here, we combine satellite observations of solar-induced fluorescence with estimates of SM and VPD and show that SM is the dominant driver of dryness stress on ecosystem production across more than 70% of vegetated land areas with valid data. Moreover, after accounting for SM-VPD coupling, VPD effects on ecosystem production are much smaller across large areas. We also find that SM stress is strongest in semi-arid ecosystems. Our results clarify a longstanding question and open new avenues for improving models to allow a better management of drought risk.

Highlights

Dryness stress can limit vegetation growth and is often characterized by low soil moisture (SM) and high atmospheric water demand
The difficulty to disentangle the respective effects of SM and VPD stems from the fact that SM and VPD are strongly coupled through land–atmosphere interactions[7,20]
Given the strong SM-VPD coupling (Fig. 1c), e.g., on the yearly scale, both lower SM and higher VPD are associated with lower ecosystem gross primary production (GPP), indicated by solar-induced chlorophyll fluorescence (SIF) (Fig. 1a, b)

Summary

Introduction

Dryness stress can limit vegetation growth and is often characterized by low soil moisture (SM) and high atmospheric water demand (vapor pressure deficit, VPD). The relative role of low SM and high VPD in limiting vegetation productivity at the ecosystem scale remain unclear. With simultaneous use of several independent satellite observations of solar-induced chlorophyll fluorescence (SIF) and climate data sets, we first decouple the strong correlations between SM and VPD and disentangle their respective effects in limiting ecosystem production globally.

Results

Conclusion