黄土高原植被恢复对降水格局的调节作用

IF 2.8 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Chao Li, Guangshuai Li, Bin Zhu, Xi Chen, Chong-Yu Xu, Zengxin Zhang
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引用次数: 0

摘要

在中国黄土高原实施的大规模植被恢复计划通过改变地表-大气相互作用中的生物物理过程改变了区域降水状况。本研究将多年代际卫星记录(1982-2018)与WRF模式模拟相结合,揭示了植被介导降水调制的生物物理机制。结果表明:(1)1982 ~ 1999年黄土高原降水对植被恢复的响应不明显。2000年以后降水量呈上升趋势,干旱区多年平均降水量高于半干旱半湿润地区。然而,植被恢复对区域降水的积极作用在2015年后开始减弱。(2)植被恢复增加了蒸散量,通过地表热液动力和能量转换的变化改变了大气湿度和空气运动,从而促进了区域降水。2000—2018年植被恢复对区域PRE的贡献为3.68 mm/a,约占PRE增长率的31.32%。(3)植被恢复可以通过增加降水来补偿土壤蒸散发增加所消耗的水分;但在2015年以后,植被恢复对降水和土壤湿度的有利作用开始减弱。这些结果表明,植被恢复启动了一个正反馈循环,增加了土壤湿度和区域降水。但是,如果降水和土壤湿度没有按比例增加,植被的过度增加可能会加剧区域水资源短缺,并对当地生态构成重大威胁。这一发现对指导黄土高原植被恢复、优化水资源管理和促进生态可持续性具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Investigating the Regulation Effects of Vegetation Restoration on Precipitation Patterns Over the Loess Plateau, China

Investigating the Regulation Effects of Vegetation Restoration on Precipitation Patterns Over the Loess Plateau, China

Investigating the Regulation Effects of Vegetation Restoration on Precipitation Patterns Over the Loess Plateau, China

Investigating the Regulation Effects of Vegetation Restoration on Precipitation Patterns Over the Loess Plateau, China

Investigating the Regulation Effects of Vegetation Restoration on Precipitation Patterns Over the Loess Plateau, China

The large-scale vegetation restoration program implemented across China's Loess Plateau altered regional precipitation regimes by modifying biophysical processes in surface-atmosphere interactions. This study integrated multi-decadal satellite records (1982–2018) with WRF model simulations to reveal the biophysical mechanisms underlying vegetation-mediated precipitation modulation. The results indicated that: (1) The response of precipitation to vegetation restoration on the Loess Plateau was not obvious between 1982 and 1999. However, precipitation began to trend upward after 2000, with arid regions experiencing higher multi-year average precipitation compared to semi-arid and semi-humid regions. Nonetheless, the positive effect of vegetation restoration on regional precipitation started to diminish after 2015. (2) Vegetation restoration increased evapotranspiration, altering atmospheric humidity and air movement via changes in surface hydrothermal dynamics and energy conversion, thus boosting regional precipitation. Vegetation restoration contributed 3.68 mm/a to regional PRE between 2000 and 2018, accounting for about 31.32% of the PRE growth rate. (3) Vegetation restoration could compensate for the soil moisture consumption from increased evapotranspiration by increasing precipitation; however, after 2015, the beneficial effects of vegetation restoration on precipitation and soil moisture started to wane. These results indicated that vegetation restoration initiated a positive feedback loop, enhancing both soil moisture and regional precipitation. However, an excessive increase in vegetation might exacerbate regional water scarcity and pose a significant threat to the local ecology if precipitation and soil moisture did not increase proportionally. This finding held crucial implications for guiding vegetation restoration efforts on the Loess Plateau, optimising water resource management and promoting ecological sustainability.

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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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