日尺度下水热因子变化对青藏高原高寒草原生产力的影响特征
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国家自然科学基金(41701606,U21A2021);中央高校基本科研业务费(2452020009);陕西省自然科学基础研究计划(2021JM-093)


Effects of daily variation of hydro-thermal factors on alpine grassland productivity on the Qinghai-Tibet Plateau
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National Natural Science Foundation of China (41701606、U21A2021);the Fundamental Research Funds for the Central Universities (2452020009)、Natural Science Basic Research Program of Shaanxi Province(2021JM-093)

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    摘要:

    温度和降水变化显著影响高寒生态系统植被生长和系统功能。草地生产力作为草地系统功能强弱的重要体现,对气候变化,特别是温度和降水变化十分敏感。探究高寒草原生产力如何响应气候变化,对预测未来气候变化情景下高寒草地系统功能变化意义重大。前期研究大都从年或季节尺度探究气候变化对草地生产力的影响特征,缺乏更精细时间尺度的关联分析。本研究基于 1997-2020 年青藏高原高寒草原长期植被观测数据及相应气候资料,应用简单线性回归及偏最小二乘回归法(Partial Least Squares regression, PLS)探究了研究区草地地上净初级生产力对日尺度温度和降水变化响应特征。结果表明:(1)近24 a来研究区年平均气温和降水量分别以0.03℃/a和4.36 mm/a的速率显著升高;(2)近24 a来研究区草地生产力显著升高(增幅为5.24 g m-2 a-1),且与年平均温度和降水量呈显著正相关关系;(3)日尺度分析表明,不同阶段温度和降水变化对草地生产力的影响不同,其中5-8月和9-10月的温度及5-7月和9-11月的降水是影响研究区草地生产力的气候因子关键作用期,尤以生长季温度(5-8月)和降水(5-7月)变化影响更高,这表明生长季气候变化是该高寒草地生产力变化的主要驱动因素。总之,本研究指出近24 a生长季温度和降水量显著增加对高寒草原生产力具有重要促进作用,这意味着青藏高原暖湿化对高寒草原生态系统功能(草地生产力)影响不仅依赖于温度和降水变化的幅度,同时亦与温度和降水变化的方向和是否同步密切相关。

    Abstract:

    Changes in temperature and precipitation significantly affect plant growth and system function in the alpine ecosystem. As an important reflection of grassland system function, grassland productivity is very sensitive to climate change, especially to temperature and precipitation. Therefore, it is significant to explore how grassland productivity responds to climate change for predicting system function in the alpine steppe under the background of future climate change. Previous studies often investigated the effects of climate change on grassland productivity at annual or seasonal scales, but there was a lack of correlation analysis at finer time scales. Based on the long-term productivity records and corresponding climatic data from 1997 to 2020, we used simple linear regression and partial least squares regression to reveal the responses of grassland productivity to temperature and precipitation on a daily scale. The results showed that: (1) the annual mean temperature and precipitation in the study area increased significantly in the past 24 years, with a rate of 0.03 ℃/a and 4.36 mm/a, respectively. (2) Meanwhile, grassland productivity increased significantly, with a rate of 5.24 g m-2 a-1, and had significantly positive responses to annual mean temperature and precipitation variation. (3) The results of the daily analysis showed that the effects of temperature and precipitation during different periods on grassland productivity were different. In specific, the temperature from May to August and September to October and precipitation from May to July and September to November were key periods to explain the impacts of climate change on grassland productivity, especially temperature (May to August) and precipitation (May to July) variations during the growing season had the higher impacts on grassland productivity, suggesting climate change in the growing season was the main driving factor for variation in grassland productivity. Overall, the present study indicated that increasing temperature and precipitation during the growing season in the past 24 years significantly promoted grassland productivity of the alpine steppe. The effects of warm-wet climate on alpine grassland ecosystem function (e.g., grassland productivity) were closely dependent on the magnitude, direction, and synchronization of altered temperature and precipitation.

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马扶林,刘小伟,朵莹,于宗恺,张强,温仲明,彭长辉,郭梁.日尺度下水热因子变化对青藏高原高寒草原生产力的影响特征.生态学报,2023,43(9):3719~3728

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