Abstract

Net primary productivity (NPP) is an important indicator of plant dynamics and the net carbon exchange between the terrestrial ecosystem and atmosphere. Both the long-term shifts in climate mean (climate change) and short-term variations around the climate mean (climate variability) have impacts on NPP but studies examining both aspects of climate variations are rare especially in the data-scarce regions such as the Tibetan Plateau (TP). Here, we used a dynamic vegetation model to investigate the impacts of the changes and variabilities in temperature, precipitation, cloud cover and CO2 on NPP on the TP. The simulated NPP was evaluated using field and Moderate-Resolution Imaging Spectroradiometer NPP and was found to be reasonable. At monthly time scale, NPP significantly correlated concurrently and at 1-month lag with temperature, precipitation and cloud cover (coefficient of determination, R2, in 0.52–0.77). Annual NPP variability was high (low) where mean annual NPP was low (high). The effects of annual precipitation, cloud cover and temperature variability on annual NPP variability were spatially heterogeneous, and temperature variability appeared to be the dominant factor (R2 of 0.74). Whereas, NPP changes were very similar to CO2 increases across the TP (spatial correlation of 0.60), indicating that long-term changes in NPP were dominated by CO2 increases. For both variability and long-term changes in NPP, temperature was the major factor of influence (highest spatial correlation of 0.67). These findings could assist in making informed mitigation policies on the impacts of climate change and variability on ecosystem and local nomadic communities.

Highlights

  • Climate is defined as long-term averages and variations in weather conditions over a period of usually several decades in a region

  • Being the first of its kind on the Tibetan Plateau (TP), this study aims to deconvolve the impacts of annual variability and long-term change in major climate elements on annual Net primary productivity (NPP) by using a dynamic vegetation model with carefully designed scenarios (Table 1)

  • This study revealed the effects of inter-annual variability and long-term change in temperature, precipitation, cloud cover and ­CO2 on annual NPP variability and trend on the TP

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Summary

Introduction

Climate is defined as long-term averages and variations in weather conditions over a period of usually several decades in a region. Some of the variability occurs randomly (e.g., extreme events such as heat wave, deluge and drought) and some occurs periodically and relatively regularly (e.g., El Niño and Southern Oscillation or ENSO, Pacific Decadal Oscillation or PDO). Another aspect relates to a shift in the long-term (e.g., decadal) mean, often termed climate change and is represented by a long-term trend, e.g., global warming caused by humans. We define variation as the combination of long-term change and shortterm variability

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