Environmental Humidity Regulates Effects of Experimental Warming on Vegetation Index and Biomass Production in an Alpine Meadow of the Northern Tibet.

Gang Fu,Zhen Xi Shen,Dafeng Hui

doi:10.1371/journal.pone.0165643

Abstract

Uncertainty about responses of vegetation index, aboveground biomass (AGB) and gross primary production (GPP) limits our ability to predict how climatic warming will influence plant growth in alpine regions. A field warming experiment was conducted in an alpine meadow at a low (4313 m), mid- (4513 m) and high elevation (4693 m) in the Northern Tibet since May 2010. Growing season vapor pressure deficit (VPD), soil temperature (Ts) and air temperature (Ta) decreased with increasing elevation, while growing season precipitation, soil moisture (SM), normalized difference vegetation index (NDVI), soil adjusted vegetation index (SAVI), AGB and GPP increased with increasing elevation. The growing season Ta, Ts and VPD in 2015 was greater than that in 2014, while the growing season precipitation, SM, NDVI, SAVI, AGB and GPP in 2015 was lower than that in 2014, respectively. Compared to the mean air temperature and precipitation during the growing season in 1963–2015, it was a warmer and wetter year in 2014 and a warmer and drier year in 2015. Experimental warming increased growing season Ts, Ta,VPD, but decreased growing season SM in 2014–2015 at all the three elevations. Experimental warming only reduced growing season NDVI, SAVI, AGB and GPP at the low elevation in 2015. Growing season NDVI, SAVI, AGB and GPP increased with increasing SM and precipitation, but decreased with increasing VPD, indicating vegetation index and biomass production increased with environmental humidity. The VPD explained more variation of growing season NDVI, SAVI, AGB and GPP compared to Ts, Ta and SM at all the three elevations. Therefore, environmental humidity regulated the effect of experimental warming on vegetation index and biomass production in alpine meadows on the Tibetan Plateau.

Highlights

By the end of this century, the global surface temperature will increase by 1.0–3.7°C and the alpine ecosystems will be most likely sensitive to such climatic warming in the high altitudes and latitudes regions [1,2,3]
Experimental warming did not affect plant biomass in alpine meadows on the Tibetan Plateau [10,11,12]
The interannual variations of aboveground biomass (AGB), gross primary production (GPP) and vegetation index were in line with those of precipitation and soil moisture (SM), but in contrast with those of vapor pressure deficit (VPD), Ts and Ta

Summary

Introduction

By the end of this century, the global surface temperature will increase by 1.0–3.7°C and the alpine ecosystems will be most likely sensitive to such climatic warming in the high altitudes and latitudes regions [1,2,3]. Low temperature is a key limiting factor in alpine regions, indicating that climatic warming can generally stimulate alpine plant growth and biomass accumulation. A meta-analysis showed that experimental warming increased aboveground plant production in alpine regions [3]. Liu et al [4], Qin et al [5], Wang et al [6], and Zhang et al [7] found that experimental warming increased plant production in the alpine meadow on the Tibetan Plateau. Experimental warming did not affect plant biomass in alpine meadows on the Tibetan Plateau [10,11,12]. There remain uncertainties about how climatic warming will affect alpine plant growth and associated vegetation index

Objectives

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Results

Conclusion