Abstract

Drought-induced tree mortality is occurring across all forested continents and is expected to increase worldwide during the coming century. Regional-scale forest die-off influences terrestrial albedo, carbon and water budgets, and land-surface energy partitioning. Although increased temperatures during drought are widely identified as a critical contributor to exacerbated tree mortality associated with “global-change-type drought”, corresponding changes in vapor pressure deficit (D) have rarely been considered explicitly and have not been disaggregated from that of temperature per se. Here, we apply a detailed mechanistic soil–plant–atmosphere model to examine the impacts of drought, increased air temperature (+2°C or +5°C), and increased vapor pressure deficit (D; +1 kPa or +2.5 kPa), singly and in combination, on net primary productivity (NPP) and transpiration and forest responses, especially soil moisture content, leaf water potential, and stomatal conductance. We show that increased D exerts a larger detrimental effect on transpiration and NPP, than increased temperature alone, with or without the imposition of a 3-month drought. Combined with drought, the effect of increased D on NPP was substantially larger than that of drought plus increased temperature. Thus, the number of days when NPP was zero across the 2-year simulation was 13 or 14 days in the control and increased temperature scenarios, but increased to approximately 200 days when D was increased. Drought alone increased the number of days of zero NPP to 88, but drought plus increased temperature did not increase the number of days. In contrast, drought and increased D resulted in the number of days when NPP = 0 increasing to 235 (+1 kPa) or 304 days (+2.5 kPa). We conclude that correct identification of the causes of global change-type mortality events requires explicit consideration of the influence of D as well as its interaction with drought and temperature.This study disaggregates the influence of temperature and vapour pressure deficit on net primary productivity of an Australian woodland and their interactions with drought as potential causal agents in recent widespread forest mortality.

Highlights

  • Extreme events such as drought are recognized as drivers of vegetation change under future climate (Overpeck and Cole 2006; Smith 2011)

  • Assessing trends in extreme events as opposed to mean conditions remains difficult due to much greater limitation in the available data (Dai 2011; IPCC 2011), recent analyses suggest an increase in aridity and drought across much of southern Europe, Africa, most of the Americas, Australia, and Southeast Asia (Dai 2011)

  • Our results show that drought plus increased D had a much larger negative impact on transpiration and net primary productivity (NPP) than drought plus increased temperature

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Summary

Introduction

Extreme events such as drought are recognized as drivers of vegetation change under future climate (Overpeck and Cole 2006; Smith 2011). Droughts have shifted vegetation boundaries substantially, as evident in both paleo- and historical (Davis et al 2002; Allen and Breshears 1998) data. Assessing trends in extreme events as opposed to mean conditions remains difficult due to much greater limitation in the available data (Dai 2011; IPCC 2011), recent analyses suggest an increase in aridity and drought across much of southern Europe, Africa, most of the Americas, Australia, and Southeast Asia (Dai 2011). Severity, and aerial extent of drought and concomitant regional-scale forest dieback are of concern because of the impact this has on terrestrial a 2013 The Authors.

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