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Global karst vegetation regime and its response to climate change and human activities

机译:全球喀斯特植被政权及其对气候变化和人类活动的回应

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摘要

The vegetation in karst regions (KR) is crucial to maintain fragile local ecosystems. Therefore, it is critical to understand the factors that affect their vitality. The objective of this work is to study global KR vegetation dynamics between 1986 and 2015 and the natural and anthropogenic factors that affect it. The results showed a significantly (p 0.05) positive greening trend (greening and browning trends were estimated to be 31.90% and 14.29%, respectively). The recuperation of KR vegetation was mainly observed at high latitudes and equatorial regions, where there is less human influence.Nevertheless, the growth of vegetation in some middle and low latitudes areas was a consequence of the human intervention. Vegetation degradation in KR was especially observed at middle latitudes due to the harsh environment and human impact. No significant correlation was observed between karst vegetation stability, the variation of annual average temperature and precipitation accumulated. Globally, karst vegetation dynamics depend more on precipitation than in temperature. In some areas, vegetation can recover gradually, even under extreme conditions and without human intervention. In areas with high population density, vegetation recuperation is mainly as a consequence of restoring programs.
机译:喀斯特地区(KR)的植被至关重要,以维持脆弱的局部生态系统。因此,了解影响其活力的因素至关重要。这项工作的目的是研究1986年至2015年间的全球KR植被动态以及影响它的自然和人为因素。结果显示出显着(P <0.05)正绿化趋势(绿化和褐变趋势估计分别为31.90%和14.29%)。 KR植被的恢复主要在高纬度和赤道地区观察,在那里存在较少的人类影响。无论如何,一些中低纬度地区的植被的生长是人为干预的结果。由于恶劣的环境和人类的影响,在中纬度地区尤其观察到KR中的植被降解。在岩溶植被稳定性之间没有观察到显着的相关性,年平均温度和降水的变化积累。在全球范围内,喀斯特植被动态比温度更依赖于沉淀。在某些地区,即使在极端条件下,植被也可以逐渐恢复,没有人为干预。在人口密度高的地区,植被恢复主要是恢复程序的结果。

著录项

  • 来源
    《Ecological indicators》 |2020年第6期|106208.1-106208.11|共11页
  • 作者单位

    Beijing Forestry Univ Sch Soil & Water Conservat Beijing 100083 Peoples R China|Beijing Forestry Univ Key Lab Soil & Water Conservat State Forestry Adm Beijing 100083 Peoples R China|Beijing Forestry Univ Sch Soil & Water Conservat Jianshui Res Stn Beijing 100083 Peoples R China;

    Mykolas Romeris Univ Environm Management Lab Ate G 20 LT-08303 Vilnius Lithuania;

    Beijing Forestry Univ Sch Soil & Water Conservat Beijing 100083 Peoples R China|Beijing Forestry Univ Key Lab Soil & Water Conservat State Forestry Adm Beijing 100083 Peoples R China|Beijing Forestry Univ Sch Soil & Water Conservat Jianshui Res Stn Beijing 100083 Peoples R China;

    Beijing Forestry Univ Sch Soil & Water Conservat Beijing 100083 Peoples R China|Beijing Forestry Univ Key Lab Soil & Water Conservat State Forestry Adm Beijing 100083 Peoples R China|Beijing Forestry Univ Sch Soil & Water Conservat Jianshui Res Stn Beijing 100083 Peoples R China;

    Chinese Acad Geol Sci Inst Karst Geol Key Lab Karst Dynam Minist Land & Resources & Sci & Technol Dept Guan Guilin 541004 Peoples R China|UNESCO Int Res Ctr Karst Auspices Guilin 541004 Peoples R China;

    Beijing Forestry Univ Sch Soil & Water Conservat Beijing 100083 Peoples R China|Beijing Forestry Univ Key Lab Soil & Water Conservat State Forestry Adm Beijing 100083 Peoples R China|Beijing Forestry Univ Sch Soil & Water Conservat Jianshui Res Stn Beijing 100083 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; First-order difference; Human footprint; Inter-annual variability; Karst vegetation; NDVI;

    机译:气候变化;一阶差异;人类足迹;年间变异性;喀斯特植被;NDVI;

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