Response of vegetation to drought and yield monitoring based on NDVI and SIF

被引:43
作者
Ding, Yibo [1 ]
He, Xiaofeng [2 ]
Zhou, Zhaoqiang [3 ,6 ]
Hu, Jie [1 ]
Cai, Huanjie [4 ]
Wang, Xiaoyun [4 ]
Li, Lusheng [5 ,7 ]
Xu, Jiatun [4 ]
Shi, Haiyun [3 ]
机构
[1] Yellow River Engn Consulting Co Ltd, Zhengzhou 450003, Peoples R China
[2] Hangzhou River & Rural Water Conservancy Managemen, Hangzhou 310014, Peoples R China
[3] Southern Univ Sci & Technol, Sch Environm Sci & Engn, State Environm Protect Key Lab Integrated Surface, Shenzhen, Peoples R China
[4] Northwest A&F Univ, Coll Water Resources & Architectural Engn, Yangling 712100, Peoples R China
[5] North China Univ Water Resources & Elect Power, Sch Water Conservancy, Zhengzhou, Peoples R China
[6] Southern Univ Sci & Technol, Sch Environm Sci & Engn, Shenzhen 518055, Peoples R China
[7] North China Univ Water Resources & Elect Power, Sch Water Conservancy, 36 Beihuan Rd, Zhengzhou, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
NDVI; Solar -induced chlorophyll fluorescence; Crop yield; Drought; CROP YIELD; CHINA; COVER;
D O I
10.1016/j.catena.2022.106328
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
An increase in global warming has resulted in a global increase in meteorological droughts. As droughts play a key factor regulating vegetation growth, they inevitably have social and economic effects. Understanding vegetation dynamics and its response to climate change is therefor highly important to reveal the behavior mechanism of terrestrial ecosystems and to guide environmental management. In this investigation, Solarinduced Chlorophyll Fluorescence (SIF) and the Normalized Difference Vegetation Index (NDVI) were applied as vegetation indicators to describe vegetation dynamics and meteorological drought was described using the standardized precipitation evapotranspiration index (SPEI). Bias correction of precipitation and crop yield data of major crop producing areas was also used. By employing correlation coefficient of the maximum absolute value, a drought impact degree and propagation time to vegetation were defined. Dimensions of SIF and NDVI were unified by normalization. Results indicated that: (1) SIF and NDVI generally had a high level of consistency over China, and NDVI had a higher normalized value distribution level than SIF for different vegetation types. (2) Drought generally had a negative impact on vegetation in northern China and a positive impact in southern China. (3) Drought propagation time based on NDVI was larger than that based on SIF. (4) SIF had some advantages when monitoring crop yields among different crop producing areas. Results from this investigation will enable a greater understanding of SIF and NDVI for their application to monitor droughts and crop yield.
引用
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页数:15
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