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Diverse responses of vegetation growth to meteorological drought across climate zones and land biomes in northern China from 1981 to 2014

机译:1981年至2014年,中国北部气候区气候区气候增长对气象干旱的多样性回应

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Improving our understanding of present and future impacts of drought on the vegetation in northern China is heightened by expectations that drought would increase its vulnerability and subsequently accelerate land degradation. The response of vegetation activity to drought and the underlying mechanisms are not well known. By using the third-generation Normalized Difference Vegetation Index (NDVI) and the Standardized Precipitation Evapotranspiration Index (SPEI), we investigated the relationship between NDVI and SPEI, across different climate regimes and land cover types, and determined the dominant time-scales at which different biome types respond to drought during the period of 1981-2014. Our results showed that biome response is coupled with drought trends in most regions of northern China. The highest correlation between monthly NDVI and SPEI at different time scales (1-48 months) assessed the impact of drought on vegetation, and the time scales resulting in the highest correlation were an effective indicator of drought resistance, which was related to the interactive roles of mean water balance and divergent drought survival traits and strategies. Diverse responses of vegetation to drought were critically dependent on characteristic drought time-scales and different growing environments. This study highlighted the most susceptible ecosystem types to drought occurrence under current climate, including temperate steppes, temperate desert steppes, warm shrubs and dry forests. Given that drought will be more frequent and severe under future climate scenarios, it may threaten the survival of mesic ecosystems, such as temperate meadows, alpine grasslands, dwarf shrubs, and moist forests not normally considered at drought risk. We propose that future research should be focused on arid and semi-arid ecosystems, where the strongest impact of drought on vegetation is occurring and the need for an early warning drought system is increasingly urgent.
机译:通过对干旱增加其脆弱性和随后加速土地退化的预期,提高对中国北方植被对中国植被的对策对现植植被的理解提高了。植被活性对干旱的响应和潜在机制尚不清楚。通过使用第三代归一化差异植被指数(NDVI)和标准化降水蒸发指数(SPEI),我们研究了NDVI和SPEI之间的关系,不同的气候制度和陆地覆盖类型,并确定了主要的时间尺度不同的生物群系类型在1981 - 2014年期间回应干旱。我们的研究结果表明,生物群落反应与中国北方大多数地区的干旱趋势相结合。每月NDVI和SPEI之间的不同时间尺度(1-48个月)之间的相关性评估了干旱对植被的影响,结果最高的时间尺度是干旱抵抗的有效指标,这与互动角色有关平均水平和发散性生存特质和策略。植被到干旱的不同反应尺寸依赖于特征干旱时间尺度和不同的生长环境。本研究强调了当前气候下干旱发生的最易受影响的生态系统类型,包括温带草原,温带沙漠草原,温暖的灌木和干燥森林。鉴于在未来的气候情景下,干旱将更加频繁,并且在未来的气候情景下,可能会威胁介于温带草地,高山草原,矮化灌木和通常考虑在干旱风险上的温带草甸的生存。我们提出了未来的研究应专注于干旱和半干旱的生态系统,其中干旱对植被的最强烈影响发生,需要提前预警系统的需求越来越紧急。

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