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Responses of vegetation phenology to the asymmetric changes of temperature in daytime and night-time in the north of 20 degrees N

文献类型： 外文期刊

作者： Hou, Xuehui 1 ; Gao, Shuai 2 ; Li, Xinhua 1 ; Wang, Meng 1 ; Zhao, Jia 1 ; Sui, Xueyan 1 ; Liang, Shouzhen 1 ;

作者机构： 1.Shandong Acad Agr Sci, Key Lab East China Urban Agr, Minist Agr & Rural Affairs, Jinan, Peoples R China

2.Chinese Acad Sci, Aerosp Informat Res Inst, Beijing, Peoples R China

关键词： elevation gradient; normalized difference vegetation index (NDVI); Northern Hemisphere; plant phenology; spatial variability; warming in daytime and night-time

期刊名称：INTERNATIONAL JOURNAL OF CLIMATOLOGY （ 影响因子：3.651； 五年影响因子：4.914 ）

ISSN： 0899-8418

年卷期：

页码：

收录情况： SCI

摘要： Focusing on the regional differences in the asymmetric effects of daytime and night-time warming on plant phenology, (a) the start-of-season (SOS) and end-of-season (EOS) were extracted based on a normalized difference vegetation index (NDVI) dataset for areas north of latitude 20 degrees N during 1982-2015; (b) the partial Pearson correlation coefficient between phenology and temperature was calculated, excluding the effects of precipitation, drought, and evapotranspiration; and (c) the asymmetric effects of daytime and night-time temperatures on phenology were analysed from the perspectives of the entire study area, different climate regimes, and different altitudes. The results show that phenology showed opposing responses to changes in daytime temperature (Td) and night-time temperature (Tn) in spring as well as autumn. However, such asymmetric effects were dependent on the climate. In arid/semi-arid regions, increasing Td induced drought stress by facilitating evaporation from soil, resulting in a delayed SOS and an early EOS, while increasing Tn was beneficial for seed germination and leaf unfolding in the spring. In temperate climate regimes, the responses of phenology to warming in the day and night were more complicated due to different plant species and precipitation. In cold regions, increasing Td led to the advancement of the SOS, while increasing Tn delayed it. In contrast, night-time warming in autumn significantly delayed the EOS and daytime warming advanced the EOS in cold regions. Warming affected the seasonal dynamics of plants in spring and autumn to a greater degree at higher altitudes than at lower altitudes, which is consistent with the results of previous studies. These results provide valuable insights into the patterns of the asymmetric relationship between the effects of changes in daytime and night-time temperatures on plant phenology, over a range of regions and altitudes.

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