Ma Pengfei, Zhao Jingxue, Zhang Haoze, Zhang Lin, Luo Tianxiang
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
College of Ecology, Lanzhou University, Lanzhou 730000, China.
Sci Total Environ. 2023 May 1;871:162000. doi: 10.1016/j.scitotenv.2023.162000. Epub 2023 Feb 3.
It is debatable whether warming or increased precipitation primarily drives the changes of spring and autumn phenology in alpine grasslands at high elevations like the Tibetan Plateau. We aim to test the hypothesis that increased precipitation and soil moisture rather than warming significantly advance spring green-up dates (GUD) of dominant species in a semiarid alpine grassland, while both increases of temperature and precipitation delay their autumn senescence dates (SD). We conducted a 2-year manipulative experiment with infrared warming (ambient, +2 °C) and precipitation increase for each of rainfall events (ambient, +15 %, +30 %) during the growing season in a Tibetan alpine grassland. GUD and SD of three dominant species and the relevant soil temperature (ST) and moisture (SM) were observed. Rainy season onset as well as Pre-GUD or Pre-SD (30 days before GUD or SD) mean air-temperature (T) and precipitation (P) and relevant soil temperature (ST) and moisture (SM) were calculated for each experimental treatment. GUD dates of the three dominant species were advanced by increased precipitation rather than by warming, which showed a robust positive correlation with rainy season onset. SD dates were independently delayed by both increases of temperature and precipitation. There was no interactive effect of warming and increased precipitation on GUD and SD across species and years. In general, GUD had a significant negative correlation with Pre-GUD P (SM) but not with Pre-GUD T (ST), while SD showed a significant positive correlation with Pre-SD T and P or Pre-SD ST and SM. Our data support the hypothesis, indicating that spring and autumn phenology of monsoon-adapted alpine vegetation are more sensitive to precipitation change than to warming. The prolonged growing season length under increased temperature and precipitation is more depended on the delay of autumn senescence than the advance of spring green-up.
在青藏高原这样的高海拔地区,是变暖还是降水增加主要驱动了高寒草原春秋季物候变化,这一问题尚无定论。我们旨在验证以下假设:在半干旱高寒草原,降水增加和土壤湿度增加而非变暖,会显著提前优势物种的春季返青日期(GUD),而温度和降水的增加都会延迟其秋季枯黄日期(SD)。我们在青藏高原的一个高寒草原进行了为期两年的控制实验,在生长季设置红外增温(环境温度、+2℃)以及每次降雨事件的降水增加处理(环境水平、+15%、+30%)。观测了三种优势物种的GUD和SD以及相关的土壤温度(ST)和湿度(SM)。计算了每个实验处理的雨季开始时间以及返青前或枯黄前(GUD或SD前30天)的平均气温(T)和降水量(P)以及相关的土壤温度(ST)和湿度(SM)。三种优势物种的GUD日期是由降水增加而非变暖提前的,且与雨季开始时间呈强正相关。SD日期则独立地受到温度和降水增加的延迟影响。在物种和年份间,增温和降水增加对GUD和SD没有交互作用。总体而言,GUD与返青前的降水量(土壤湿度)呈显著负相关,但与返青前的温度(土壤温度)无关,而SD与枯黄前的温度和降水量或枯黄前的土壤温度和湿度呈显著正相关。我们的数据支持了这一假设,表明适应季风的高寒植被的春秋季物候对降水变化比对变暖更敏感。温度和降水增加下生长季长度的延长更多地依赖于秋季枯黄的延迟而非春季返青的提前。