4.6 Article

Contributions of natural and anthropogenic factors to historical changes in vegetation cover and its future projections in the Yellow River basin, China

Journal

INTERNATIONAL JOURNAL OF CLIMATOLOGY
Volume -, Issue -, Pages -

Publisher

WILEY
DOI: 10.1002/joc.8213

Keywords

climate change; future projections; human activities; Yellow River basin

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The fragile ecology of the Yellow River basin is vulnerable to global warming and human activities. This study analyzed the variations in vegetation cover in different climate zones of the Yellow River basin from 1982 to 2019. The results showed that temperature is the main driver of vegetation cover variations in the source region, while the middle and lower reaches are influenced by both temperature and precipitation-evaporation differences.
The fragile ecology of the Yellow River basin (YRB) is vulnerable to global warming and human activities. As the second largest river in China, the YRB covers the subhumid, semi-arid, arid and alpine climate zones, with considerably spatial differences in vegetation cover (VC), thus demonstrating substantial variations in response to climate change. In this study, characteristics of VC variations in different climate zones of the YRB during 1982-2019 were analysed, impacts of climate change and human activities on VC variations were identified, and possible VC variations in the future were projected under different climate scenarios. Results show that NDVI in the YRB significantly increased at a rate of 2.3 x 10(-3) year(-1) from 1982 to 2019, especially in the middle reaches of the YRB. Temperature is the main driver of VC variations in the source region of the YRB (alpine zone), wherein the warming trend contributes to the greening. The internal variability of VC is also influenced by temperature, with a marginal effect of precipitation minus evaporation (P - E). In the middle and lower reaches of the YRB consisting of arid, semi-arid, and subhumid zones, VC benefited only from the warming trend and had a less relationship with the internal variability of temperature, whereas the internal variability of VC was influenced by P - E and had a weaker relationship with the P - E trend. Contributions of climate change to VC variations in the source region and middle and lower reaches of the YRB are approximately 62%, 42%, and 27%, respectively. Human activities considerably impact the ecological environment but mostly play a positive role. In the future, VC will increase in the YRB, especially under the SSP5-8.5 scenario, and VC reveals the most prominent changes in the lower reaches. This study suggests that climate change might be favourable to VC in YRB, and emphasizes that human activities should adapt to climate change in an orderly manner.

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