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Ecosystem Evapotranspiration as a Response to Climate and Vegetation Coverage Changes in Northwest Yunnan, China

机译:滇西北地区生态系统蒸散量对气候和植被覆盖变化的响应

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摘要

Climate and human-driven changes play an important role in regional droughts. Northwest Yunnan Province is a key region for biodiversity conservation in China, and it has experienced severe droughts since the beginning of this century; however, the extent of the contributions from climate and human-driven changes remains unclear. We calculated the ecosystem evapotranspiration (ET) and water yield (WY) of northwest Yunnan Province, China from 2001 to 2013 using meteorological and remote sensing observation data and a Surface Energy Balance System(SEBS) model. Multivariate regression analyses were used to differentiate the contribution of climate and vegetation coverage to ET. The results showed that the annual average vegetation coverage significantly increased over time with a mean of 0.69 in spite of the precipitation fluctuation. Afforestation/reforestation and other management efforts attributed to vegetation coverage increase in NW Yunnan. Both ET and WY considerably fluctuated with the climate factors, which ranged from 623.29 mm to 893.8 mm and -51.88 mm to 384.40 mm over the time period. Spatially, ET in the southeast of NW Yunnan (mainly in Lijiang) increased significantly, which was in line with the spatial trend of vegetation coverage. Multivariate linear regression analysis indicated that climatic factors accounted for 85.18% of the ET variation, while vegetation coverage explained 14.82%. On the other hand, precipitation accounted for 67.5% of the WY. We conclude that the continuous droughts in northwest Yunnan were primarily climatically driven; however, man-made land cover and vegetation changes also increased the vulnerability of local populations to drought. Because of the high proportion of the water yield consumed for subsistence and poor infrastructure for water management, local populations have been highly vulnerable to climate drought conditions. We suggest that conservation of native vegetation and development of water-conserving agricultural practices should be implemented as adaptive strategies to mitigate climate change.
机译:气候和人类驱动的变化在区域干旱中起着重要作用。滇西北是中国生物多样性保护的重要地区,自本世纪初以来经历了严重的干旱。然而,气候和人为改变的贡献程度尚不清楚。我们使用气象和遥感观测数据以及地表能量平衡系统(SEBS)模型,计算了2001年至2013年中国云南西北地区的生态系统蒸散量(ET)和水产量(WY)。多元回归分析用于区分气候和植被覆盖对ET的贡献。结果表明,尽管降水量波动,但年平均植被覆盖度仍随时间显着增加,平均为0.69。云南西北地区由于植被覆盖率增加而进行的造林/再造林及其他管理工作。 ET和WY随气候因子的变化很大,在这段时间内,范围从623.29毫米到893.8毫米,从-51.88毫米到384.40毫米。在空间上,云南西北部(主要在丽江)东南部的ET显着增加,这与植被覆盖的空间趋势一致。多元线性回归分析表明,气候因素占ET变化的85.18%,而植被覆盖率占14.82%。另一方面,降水占WY的67.5%。我们得出的结论是,滇西北地区的持续干旱主要是由气候驱动的。然而,人为的土地覆盖和植被变化也增加了当地居民遭受干旱的脆弱性。由于用于维持生计的水产量所占比例很高,以及用于水资源管理的基础设施较差,因此当地居民极易遭受气候干旱条件的影响。我们建议应实施原生植被保护和节水农业实践的发展,作为缓解气候变化的适应性策略。

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