Monitoring of Flash Drought on the Loess Plateau and Its Impact on Vegetation Ecosystems

Author:

Jiang Yanmin1234,Shi Haijing123ORCID,Wen Zhongming125ORCID,Yang Xihua67ORCID,Wu Youfu3,Li Li8ORCID,Ma Yuxin9,Dymond John R.9ORCID,Guo Minghang123,Shui Junfeng123,Hu Hong123

Affiliation:

1. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, The Research Center of Soil and Water Conservation and Ecological Environment, Chinese Academy of Sciences and Ministry of Education, Yangling 712100, China

2. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, China

3. Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China

4. University of Chinese Academy of Sciences, Beijing 100049, China

5. College of Grassland Agriculture, Northwest A&F University, Yangling 712100, China

6. New South Wales Department of Planning and Environment, Parramatta, NSW 2150, Australia

7. School of Life Sciences, University of Technology Sydney, Broadway, NSW 2007, Australia

8. Ocean College, Zhejiang University, Zhoushan 316021, China

9. Manaaki Whenua–Landcare Research, Palmerston North 4442, New Zealand

Abstract

Flash drought (FD) has attracted much attention due to its severe stress on vegetation ecosystems. Yet to date, the impacts of FD on vegetation ecosystems in different regions have not been fully evaluated and explored, especially for ecologically fragile areas. In this study, we identified the FD events in the Loess Plateau from 2000 to 2023 based on the attenuation rate in soil moisture percentile over time. The evolution process of FD, the driving roles of meteorological conditions and the responses of different vegetation types to FD were explored by vegetation indicators such as solar-induced chlorophyll fluorescence (SIF), SIFyield, SIF-RCI, etc. The results showed that FD events were predominantly concentrated in wetter areas with dense vegetation, with the highest frequency being 29. Meteorological factors contributed differently to the occurrence and development of FD. The responses of vegetation to FD were not only related to vegetation types (cropland was more sensitive to FD than forest and grassland) but were also significantly influenced by background climate. The SIFyield anomaly of vegetation was more sensitive than SIF anomaly and SIF-RCI. The results advance our understanding of the formation mechanisms of FD and facilitate the exploration of vegetative photosynthetic responses to FD.

Funder

the CAS “light of West China” program

the National Natural Science Foundation of China

the High-end Foreign Experts Recruitment Plan of China

the National R&D Infrastructure and Facility Development Program of China

Publisher

MDPI AG

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