Spatio-Temporal Change and Drivers of the Vegetation Trends in Central Asia
Author:
Li Moyan1, Yao Junqiang23ORCID, Zheng Jianghua4
Affiliation:
1. College of Geography and Tourism, Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Xinjiang Normal University, Urumqi 830054, China 2. Key Laboratory of Tree-Ring Physical and Chemical Research of CMA, Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China 3. Field Scientific Experiment Base of Akdala Atmospheric Background of CMA, Akdala 836499, China 4. Key Laboratory of Oasis Ecology of Ministry of Education, Institute of Arid Ecology and Environment, College of Geographical Sciences, Xinjiang University, Urumqi 830046, China
Abstract
The impact of changing climate on vegetation in dryland is a prominent focus of global research. As a typical arid region in the world, Central Asia is an ideal area for studying the associations between climate and arid-area vegetation. Utilizing data from the European Centre for Medium-Range Weather Forecasts fifth-generation reanalysis (ECMWF ERA-5) and normalized difference vegetation index (NDVI) datasets, this study investigates the spatio-temporal variation characteristics of the NDVI in Central Asia. It quantitatively assesses the contribution rates of climatic factors to vegetation changes and elucidates the impact of an increased vapor pressure deficit (VPD) on vegetation changes in Central Asia. The results indicate that the growing seasons’ NDVI exhibited a substantial increase in Central Asia during 1982–2015. Specifically, there was a pronounced “greening” process (0.012/10 yr, p < 0.05) from 1982 to 1998. However, an insignificant “browning” trend was observed after 1998. Spatially, the vegetation NDVI in the growing seasons exhibited a pattern of “greening in the east and browning in the west” of Central Asia. During spring, the dominant theme was the “greening” of vegetation NDVI, although there was noticeable “browning” observed in southwest region of Central Asia. During summer, the “browning” of vegetation NDVI further expanded eastward and impacted the entire western Central Asia in autumn. According to the estimated results computed via the partial differential equation method, the “browning” trend of vegetation NDVI during the growing seasons was guided by increased VPD and decreased rainfall in western Central Asia. Specifically, the increased VPD contributed 52.3% to the observed vegetation NDVI. Atmospheric drought depicted by the increase in VPD significantly lowers the “greening” trend of vegetation NDVI in arid regions, which further aggravates the “browning” trend of vegetation NDVI.
Funder
“Tianchi Talents” (Xinjiang) Plan Project Shanghai Cooperation Organization (SCO) Science and Technology Partnership and International S&T Cooperation Program Science and Technology Youth Top-notch Talent Support Program (Tianshan Talents) of Xinjiang
Reference51 articles.
1. Spatiotemporal precipitation variations in the arid Central Asia in the context of global warming;Chen;Sci. China Earth Sci. Chin. J.,2011 2. Progress and prospects of climate change impacts on hydrology in the arid region of northwest China;Chen;Environ. Res.,2015 3. Chen, Y., Li, W., Deng, H., Fang, G., and Li, Z. (2016). Changes in Central Asia’s Water Tower: Past, Present and Future. Sci. Rep., 6. 4. Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales;Chen;Earth Sci. Rev.,2019 5. Stocker, T.F., Qin, D., Plattner, G.K., Tignor, M., Allen, S.K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P.M. (2013). Climate change 2013: The physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press.
|
|