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中国绿化趋势下的热条件对植被反馈的影响。

Impact of thermal condition on vegetation feedback under greening trend of China.

机构信息

Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.

Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

出版信息

Sci Total Environ. 2021 Sep 1;785:147380. doi: 10.1016/j.scitotenv.2021.147380. Epub 2021 Apr 27.

Abstract

In China, an unambiguous greening trend was observed over the last three decades. The feedback induced by vegetation growth can affect regional climate. Here, we investigated how vegetation feeds back to land surface temperature (LST) in temperature zones and land-use types in China using 18-years (2001-2018) of Moderate Resolution Imaging Spectroradiometer (MODIS) LST and Normalized Difference Vegetation Index (NDVI) data. We first showed that vegetation feedback was significantly negative (p < 0.1, t-test) in most parts of China. Specifically, we discovered a downtrend of vegetation feedback from the coldest temperature zone to the hottest temperature zone. Moreover, vegetation feedback and thermal condition showed an inverse relationship among temperature zones. The inverse relationship clarified that vegetation growth can cool most parts of China during climate change. In the end, we showed the pattern of vegetation feedback among land-use types. Due to the expansion of grassland, vegetation feedback may temporarily positive. Suitable vegetation coverage in urban land, banning deforestation, and cultivating land reasonably can decrease the local temperature by inducing negative vegetation feedback.

摘要

在中国,过去三十年中观察到了明确的绿化趋势。植被生长所引起的反馈会影响区域气候。在这里,我们利用 18 年(2001-2018 年)的 MODIS 陆地表面温度(LST)和归一化差异植被指数(NDVI)数据,研究了植被在温度带和土地利用类型中如何反馈到中国的 LST。我们首先表明,植被反馈在中国大部分地区具有显著的负相关(p < 0.1,t 检验)。具体而言,我们发现植被反馈从最冷温度带到最热温度带呈下降趋势。此外,植被反馈和热条件在温度带之间呈反比关系。这种反比关系表明,在气候变化期间,植被生长可以使中国大部分地区降温。最后,我们展示了土地利用类型之间植被反馈的模式。由于草原的扩张,植被反馈可能暂时为正。城市土地中适当的植被覆盖、禁止砍伐森林和合理耕种土地可以通过诱导负的植被反馈来降低局部温度。

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