首页> 外文期刊>Journal of Hydrology >Impacts of moisture sources on the temporal and spatial heterogeneity of monsoon precipitation isotopic altitude effects
【24h】

Impacts of moisture sources on the temporal and spatial heterogeneity of monsoon precipitation isotopic altitude effects

机译:水分源对季风沉淀同位素高度效应的时间和空间异质性的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Moisture sources affect the temporal variations of the elevation effects on the stable isotopes in monsoon precipitation. However, whether it will lead to spatial variations and form a specific spatial-temporal heterogeneity pattern remains to be explored. Based on the monthly precipitation samples collected in Ailao Mountains of East Asian monsoon region, we computed and identified five moisture source regions to facilitate its comparison to the monthly oxygen isotope composition (delta O-18) of precipitation with HYSPLIT model. We analysed the influence mechanisms of the moisture sources on the temporal and spatial heterogeneity of the elevation effect on the hydrogen and oxygen stable isotopes during dry and rainy seasons. We found that the temporal heterogeneity of the elevation effects on the precipitation O-18 depends on the proportion of the moisture sources in the dominant direction, and as the proportion increases, the elevation effect becomes more significant. The spatial heterogeneity depends on the combination complexity of the moisture sources, the simpler the combinations, the more significant the elevation effects. The results demonstrate that for precipitation delta O-18 in Ailao Mountains, the dominant of monsoon moisture sources (the ratio higher than 50%) can result in significant elevation effects, while the mixtures of multiple moisture sources and the dominant of local moisture sources will lead to no elevation effects. Future studies should pay more attention to the influence mechanism of the spatial and temporal heterogeneity of the elevation effects on a relatively larger or global scale.
机译:水分源影响季风沉淀稳定同位素对稳定同位素的升高效应的时间变化。然而,它是否会导致空间变化并形成特定的空间 - 时均匀性模式,仍有待探索。基于东亚季风地区北部山脉收集的月度降水量,我们计算并确定了五个湿度区域,以促进与Hysplit模型沉淀的月度氧同位素组成(Delta O-18)的比较。我们分析了水分源对氢气和氧稳定同位素的升高效应的时间和空间异质性的影响机制。我们发现沉淀O-18上的升高效应的时间异质性取决于湿源在主导方向上的比例,并且随着比例的增加,升高效果变得更加显着。空间异质性取决于水分源的组合复杂性,较差的组合,升高效果越大。结果表明,对于北部山脉沉淀Delta O-18,季风湿度源的主导(比50%高的比例)可导致显着的升高效应,而多种水分源的混合物和局部水分源的主要源导致没有仰角效果。未来的研究应更加关注海拔效应的空间和时间异质性对相对较大或全球范围的影响机制。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号