Impact of Preseason Climate Factors on Vegetation Photosynthetic Phenology in Mid–High Latitudes of the Northern Hemisphere

Author:

Xiang Kunlun12,Guo Qian3,Zhang Beibei4,Wang Jiaming5,Jin Ning6,Wang Zicheng4,Liu Jiahui4,Wang Chenggong4,Du Ziqiang7,Wang Liang4,Zhao Jie45ORCID

Affiliation:

1. Guangdong Ecological Meteorology Center, Guangzhou 510640, China

2. Chongqing Institute of Meteorological Sciences, Chongqing 401147, China

3. Guangzhou Meteorological Satellite Ground Station, Guangzhou 510640, China

4. Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University, Linyi 276000, China

5. College of Natural Resources and Environment, Northwest A&F University, Xianyang 712100, China

6. Department of Resources and Environmental Engineering, Shanxi Institute of Energy, Jinzhong 030600, China

7. Institute of Loess Plateau, Shanxi University, Taiyuan 030006, China

Abstract

During the period preceding the vegetation growing season (GS), temperature emerges as the pivotal factor determining phenology in northern terrestrial ecosystems. Despite extensive research on the impact of daily mean temperature (Tmean) during the preseason period, the influence of diurnal temperature range (DTR) on vegetation photosynthetic phenology (i.e., the impact of the plant photosynthetic cycle on seasonal time scale) has largely been neglected. Using a long-term vegetation photosynthetic phenology dataset and historical climate data, we examine vegetation photosynthetic phenology dynamics and responses to climate change across the mid–high latitudes of the Northern Hemisphere from 2001 to 2020. Our data reveal an advancing trend in the start of the GS (SOS) by −0.15 days per year (days yr−1), affecting 72.1% of the studied area. This is particularly pronounced in western Canada, Alaska, eastern Asia, and latitudes north of 60°N. Conversely, the end of the GS (EOS) displays a delaying trend of 0.17 days yr−1, impacting 62.4% of the studied area, especially northern North America and northern Eurasia. The collective influence of an earlier SOS and a delayed EOS has resulted in the notably prolonged length of the GS (LOS) by 0.32 days yr−1 in the last two decades, affecting 70.9% of the studied area, with Eurasia and western North America being particularly noteworthy. Partial correlation coefficients of the SOS with preseason Tmean, DTR, and accumulated precipitation exhibited negative values in 98.4%, 93.0%, and 39.2% of the study area, respectively. However, there were distinct regional variations in the influence of climate factors on the EOS. The partial correlation coefficients of the EOS with preseason Tmean, DTR, and precipitation were positive in 58.6%, 50.1%, and 36.3% of the region, respectively. Our findings unveil the intricate mechanisms influencing vegetation photosynthetic phenology, holding crucial significance in understanding the dynamics of carbon sequestration within terrestrial ecosystems amidst climate change.

Funder

Natural Science Foundation of Guangdong Province

National Natural Science Foundation of China

Social Science Planning Research Project of Shandong Province

Publisher

MDPI AG

Reference56 articles.

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