吕梁山植被NDVI时空变化及气候因子探测
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Temporal and Spatial Variations of NDVI and Climate Factors in Lvliang Mountains
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    摘要:

    为揭示吕梁山植被覆盖的时空变化,厘清气候因子及相互作用对植被变化的影响机制,为植被长期稳定、良性发展和积极应对后续的气候变化提供指导,基于2002—2022年NDVI(归一化植被指数) 和气象数据,利用地理探测器分析NDVI与气象因子的关系。结果表明:2002—2022年吕梁山植被NDVI呈现增加趋势,空间上植被覆盖为西北低东南高的变化趋势,2012—2022年植被覆盖度较低覆盖、低覆盖、中覆盖向较高覆盖和高覆盖转换30.68%;不同时间尺度,NDVI对气候因子响应不同,且交互作用大于单因子对NDVI的解释度,2002—2012年年均气温和年均降水量共同作用达到最大解释0.685。

    Abstract:

    In order to reveal the temporal and spatial changes of vegetation cover in Lvliang Mountains, clarify the mechanism of influence of climate factors and their interactions on vegetation change, and provide guidance for long-term stability and benign development of vegetation and active response to subsequent climate change,based on NDVI(normalized difference vegetation index)and meteorological data from 2002 to 2022, the relationship between NDVI and meteorological factors was analyzed by using geodetector. The results showed that vegetation NDVI showed an increasing trend from 2002 to 2022. The spatial vegetation cover was lower in the northwest and higher in the southeast. From 2012 to 2022, the vegetation cover was 30.68% from lower cover, low cover, medium cover to higher cover and high cover.At different time scales, NDVI responds differently to climate factors, and the interaction is greater than the interpretation of single factor to NDVI. The combined effect of average annual temperature and average annual precipitation from 2002 to 2012 reaches the maximum explanation of 0.685.

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黎梅,李春雨,张玲艺,闫加亮.吕梁山植被NDVI时空变化及气候因子探测[J].科技与产业,2024,24(21):306-310

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  • 在线发布日期: 2024-11-19