双月刊

ISSN 1006-9895

CN 11-1768/O4

青海高原生长季NDVI对气候暖湿化响应的年代际变化
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南京信息工程大学

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Interdecadal variation of NDVI response to climate warming and humidification in Qinghai Plateau during the growing season
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1.Nanjing University of Information Science & Technology;2.南京信息工程大学

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    摘要:

    本文利用1982-2018年美国国家海洋和大气局(NOAA)先进甚高分辨率辐射计(AVHRR)观测得到的归一化差值植被指数(NDVI)数据集和中国区域高分辨率近地面气温和地面降水率驱动数据集(CMFD),采用线性倾向估计、M-K检验、偏相关和方差分析等方法,研究了气候暖湿化背景下青海高原生长季(5-9月)地表植被变化特征及其对气候暖湿化响应的年代际变化。结果表明:(1) 1982-2018年,青海高原生长季地表植被呈由东南向西北逐渐减小的空间分布特征,整体呈显著增加趋势(P<0.01),气候倾向率达0.01/10a,但在空间上呈两极化发展,在青海高原东部和西南部植被显著变好(面积占57.3%)的同时,青海高原西北部的柴达木盆地地表植被表现为退化态势(面积占14.8%)。(2)1982-2018年青海高原气候整体呈暖湿化特征,但在不同时段气候暖湿化的区域和强度存在差异,P1时段(1982-1998年)的增温强于P2(1998-2018年)时段,而P2时段的变湿强于P1时段。青海高原生长季NDVI的增加趋势在1998年前后出现了显著突变,1998年之前为波动上升,趋势不显著,但从1998年开始出现显著增加趋势(P<0.05),这与青海高原的暖湿化趋势相一致。(3)青海高原地表植被对气候的暖湿化响应具有年代际变化,在P1时段,水分条件不足的情况下,热量因子(气温)抑制地表植被的生长,而在P2 时段,水分条件较充足的情况下,水分和热量因子均促进地表植被的生长,在两者共同作用下,青海高原生长季地表植被出现了大范围好转。

    Abstract:

    Based on the Normalized Differential Vegetation Index (NDVI) dataset obtained from the Advanced Very High Resolution Radiometer (AVHRR) of the National Oceanic and Atmospheric Administration (NOAA), as well as the high-resolution near-surface air temperature and surface precipitation rate of China meteorological forcing dataset (CMFD) from 1982 to 2018, the variation characteristics of vegetation and their response to climate warming and humidification in Qinghai Plateau during the growing season (May-September) were studied. The methods used in this study include linear tendency estimation, M-K test, partial correlation and analysis of variance, etc. The results show that: (1) During the growing season of Qinghai Plateau from 1982 to 2018, the vegetation exhibits a spatial distribution feature that decreases gradually from southeast to northwest, and there is a significant increasing trend overall with a climate tendency rate of 0.01/10a. However, the trend of vegetation has a bi-polar development feature in space, that is to say, while the vegetation in the eastern and southwestern parts of the Qinghai Plateau improves significantly (57.3% of the total area), the vegetation of the Qaidam Basin in the northwestern part of the Qinghai Plateau shows a deterioration trend (14.8% of the total area). (2) During 1982-2018, the climate of the Qinghai Plateau is characterized by warming and humidification as a whole, but there are differences in the regions and intensities of climate warming and humidification in different periods. The warming in P1 period (1982-1998) was stronger than that in P2 period (1998-2018), and the humidification in P2 period was stronger than that in P1 period. The trend of NDVI in the growing season of Qinghai Plateau shows a significant mutation around 1998. Before 1998, it fluctuates with no obvious trend, but after 1998, it shows a significant increasing trend, which is consistent with the warming and wetting trend of the Qinghai Plateau vegetation. (3) There is an interdecadal variation in the response of surface vegetation on the Qinghai Plateau to climate warming and humidification. In P1 period, the heat factor (air temperature) inhibits the growth of surface vegetation under insufficient water conditions, while in P2 period, under relatively sufficient water conditions, both water and heat factor promote the growth of surface vegetation. Therefore, the surface vegetation of Qinghai Plateau vastly improves in the growing season.

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历史
  • 收稿日期:2023-04-14
  • 最后修改日期:2023-08-19
  • 录用日期:2023-10-24
  • 在线发布日期: 2023-10-27
  • 出版日期: