Abstract

In arid and semiarid lands, canopy transpiration and its dynamics depend largely on stomatal sensitivity to drought. In this study, the sap flow of a dominant species, Haloxylon ammodendron growing in Central Asian deserts, was monitored using Granier-type sensors, from which the canopy stomatal conductance was derived. The responses of canopy transpiration and stomatal conductance to environmental variables during the second half of the growing season, when annual prolonged drought occurred, was analyzed for four continuous years, from 2013 to 2016. A soil water content (SWC) of 3% was identified as the lower soil water threshold for this species, below which the plant lost the ability for stomatal regulation on water loss and suffered the risk of mortality. Above this threshold, the sensitivity of canopy transpiration to vapor pressure deficit, VPD (K), was linearly correlated with SWC, which mainly resulted from different stomatal behaviors at varying drought intensities. Stomatal sensitivity to VPD (m/Gsref) increased linearly with soil moisture deficit, inducing a shift from more anisohydric to a more isohydric stomatal behavior. The flexibility of stomatal behavior regarding soil drought was one key element facilitating the survival of H. ammodendron in such an extreme dry environment.

Highlights

  • Central Asia is dominated by arid and semi-arid lands and is one of the most vulnerable regions to climate change [1]

  • Our results suggest the need for long-term monitoring of the interaction between plant transpiration and environmental variables, in order to accurately evaluate ecosystem functions and vulnerability in the arid lands, which suffer frequent and extended droughts

  • The indirect effect of soil water content (SWC) on canopy transpiration through vapor pressure deficit (VPD) could only be found on a long-term scale

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Summary

Introduction

Central Asia is dominated by arid and semi-arid lands and is one of the most vulnerable regions to climate change [1]. Based on regional climate models, the annual temperature and annual precipitation in northwest of China are predicted to increase by 2.0 ◦ C and. Area-averaged annual mean surface air temperature and precipitation is predicted to increase by. Summers are likely to experience a 3.55 ◦ C increase in temperature and 2.3% decline in precipitation [5]. These predictions generally point to drier summers or plant growing seasons, which has been demonstrated by an observation data-based analysis [6].

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