The Effects of Precipitation Event Characteristics and Afforestation on the Greening in Arid Grasslands, China

Author:

Guo Xuan12,Guo Qun123,Hu Zhongmin4,Li Shenggong123ORCID,Min Qingwen12ORCID,Mu Songlin5,Xu Chengdong12ORCID,Sun Linli6

Affiliation:

1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

2. College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China

3. National Ecosystem Science Data Center, Beijing 100101, China

4. Key Laboratory of Agro-Forestry Environmental Processes and Ecological Regulation of Hainan Province, Hainan University, Haikou 570228, China

5. Beijing Academy of Social Sciences, Beijing 100101, China

6. Tongliao Meteorological Bureau of Inner Mongolia, Tongliao 028000, China

Abstract

Global greening and its relationship with climate change remain the hot topics in recent years, and are of critical importance for understanding the interactions between the terrestrial ecosystem carbon cycle and the climate system. China, especially north China, has contributed a lot to global greening during the past few decades. As a water-limited ecosystem, human activities, not precipitation amount, were thought as the main contributor to the greening of north China. Considering the importance of precipitation event characteristics (PEC) in the altered precipitation regimes, we integrated long-term normalized difference vegetation index (NDVI) and meteorological datasets to reveal the role of precipitation regimes, especially PECs, on vegetation growth across temperate grasslands in north China. Accompanied with a significantly decreased growing season precipitation (GSP), NDVI increased significantly in the largest area of the temperate grasslands during 1982–2015, i.e., greening. We found that 28.44% of the area was explained by PECs, including more heavy or extreme precipitation events, alleviated extreme drought, and fewer light events, while only 0.92% of the area was associated with GSP. NDVI did not always increase over the 30 years and there was a decrease during 1996–2005. Taking afforestation projects in desertified lands into account, we found that precipitation, mainly PECs, explained more the increase and decline of NDVI during 1982–1995 and 1996–2005, respectively, while an equivalent explanatory power of precipitation and afforestation projects to the increase in NDVI after 2005. Our study indicates a possible higher productivity under future precipitation regime scenario (e.g., fewer but larger precipitation events) or intensive afforestation activity, implying more carbon sequestration or livestock production of temperate steppe in the future.

Funder

National Natural Science Foundation of China

Strategic Priority Research Program of Chinese Academy of Sciences

Key Projects of Beijing Academy of Social Sciences

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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