Volume 28, Issue 23 pp. 6961-6972
RESEARCH ARTICLE

Contrasting temperature effects on the velocity of early- versus late-stage vegetation green-up in the Northern Hemisphere

Songbai Hong

Songbai Hong

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China

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Yichen Zhang

Yichen Zhang

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China

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Yitong Yao

Yitong Yao

Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France

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Fandong Meng

Fandong Meng

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China

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Qian Zhao

Qian Zhao

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China

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Yao Zhang

Corresponding Author

Yao Zhang

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, China

Correspondence

Yao Zhang, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.

Email: zhangyao@pku.edu.cn

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First published: 30 August 2022

Abstract

Global vegetation greening has been widely confirmed in previous studies, yet the changes in the velocity of green-up in each month of green-up period (GUP) remains unclear. Here, we defined the velocity of vegetation green-up as VNDVI (the monthly increase of Normalized Difference Vegetation Index [NDVI] during GUP) and further explored its response to climate change in middle-high-latitude Northern Hemisphere. We found that in early GUP, VNDVI generally showed positive trends from 1982 to 2015, whereas in late GUP, it showed negative trends in most areas. Such contrasting trends were mainly due to a positive temperature effect on VNDVI in early GUP, but this effect turned negative in late GUP. The increase of soil moisture also in part explained the accelerated vegetation green-up, especially in the arid and semi-arid ecosystems of inland areas. Our analyses also indicate that the first month of the GUP was the key stage impacting vegetation greenness in summer. Future warming may continuously speed up the early growth of vegetation, altering the seasonal trajectory of vegetation and its feedbacks to the Earth system.

CONFLICT OF INTEREST

The authors declare no competing interests.

DATA AVAILABILITY STATEMENT

All data used in this study are openly available from the following: GIMMS NDVI are available at http://poles.tpdc.ac.cn/en/data/9775f2b4-7370-4e5e-a537-3482c9a83d88/. CRU air temperature is available at https://crudata.uea.ac.uk/cru/data/hrg/cru_ts_4.05/cruts.2103051243.v4.05/; C3S soil moisture is available at https://cds.climate.copernicus.eu/cdsapp#!/dataset/satellite-soil-moisture?tab=overview; CRU-JRA v2.2 solar radiation is available at https://catalogue.ceda.ac.uk/uuid/7f785c0e80aa4df2b39d068ce7351bbb. MODIS EVI is available at https://lpdaac.usgs.gov/products/mod13c2v006/. All computer codes used in this study are available from the corresponding author upon reasonable request.

Volume28, Issue23

December 2022

Pages 6961-6972

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