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Spatio-temporal variation of alpine grassland spring phenological and its response to environment factors northeastern of Qinghai-Tibetan Plateau during 2000-2016

文献类型： 外文期刊

作者： Li, Guangyong 1 ; Jiang, Guanghui 1 ; Bai, Ju 2 ; Jiang, Cuihong 3 ;

作者机构： 1.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Fac Geog Sci, Beijing 100875, Peoples R China

2.Natl Geomat Ctr China, Beijing 100830, Peoples R China

3.Beijing Acad Agr & Forestry Sci, Inst Agr Sci Tech Informat, Beijing 100097, Peoples R China

关键词： Phenology;Alpine grassland;Land surface temperature;Soil moisture;Vegetation degradation;Qinghai Lake watershed

期刊名称：ARABIAN JOURNAL OF GEOSCIENCES （ 影响因子：1.827； 五年影响因子：1.985 ）

ISSN： 1866-7511

年卷期： 2017 年 10 卷 22 期

页码：

收录情况： SCI

摘要： Vulnerable alpine grassland ecosystem is highly sensitive to climate change, and its response and feedback to climate change have been intensely studied by the scientific community. In this study, the alpine grassland ecosystem in the Qinghai Lake watershed of the northeastern Qinghai-Tibet Plateau was selected as the research subject, and MODIS time series data and field sampling data were used to analyze the characteristics of the beginning of the growing season (BGS) pattern and the spatio-temporal variation and responded to environmental factors. The results show that under the combined influence of elevation, land surface temperature (LST), and soil moisture, the multi-year alpine grassland BGS pattern presents zonal horizontal characteristics with increasing delays from the southeast to the northwest and also exhibits non-zonal vertical characteristics in the western mountainous area. Alpine grassland BGS shows significant negative correlations with elevation and the 0-10 cm soil moisture content but a significant positive correlation with the mean spring LST. The relationships among BGS, elevation, and LST change when the elevation is over 4200 m, but the relationship between BGS and soil moisture continues to be a significant negative correlation. In the period 2000-2016, the BGS of the alpine grassland in the watershed generally advanced at the rate of 1.4 days/10 years and in local areas showed spatially heterogeneous trends. Spring soil moisture plays a key role in controlling spatio-temporal variations of BGS in the arid and semi-arid areas of the alpine zone relative to LST. Grassland degradation also affects the BGS spatio-temporal pattern and shows grassland degradation result of BGS in advance. The findings would provide a scientific reference for further understanding the mechanism of alpine vegetation phenology.

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