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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Sources and behavior of monsoon air masses in the lowest-latitude region on the Tibetan Plateau, and their paleoclimatic implications
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Sources and behavior of monsoon air masses in the lowest-latitude region on the Tibetan Plateau, and their paleoclimatic implications

机译:藏高原最低纬度地区季风空气群众的来源与行为及其古叶病症

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摘要

To better understand the reported paleoclimate features and underlying mechanisms in the lowest-latitude region (similar to 28 degrees N to 29 degrees 30'N), where 12 major river gorges cross the Himalayas, of the southern Tibetan Plateau, we aim to elucidate the major sources and behavior of modern monsoon air masses in the region based on spatial variations in the delta O-18 and delta H-2 of stream water and precipitation, and vegetation during the summer monsoon season. Our main findings were following: The river gorges, high mountain ranges bearing extensive dense vegetation, and stronger solar insolation characteristic of the lowest-latitude region may have functioned for an extended period as the essential geological settings for strongly drawing significant amounts of moisture from the Indian Ocean toward the region without passing through the Yarlung Zangbo basin. The combination of such geological settings specific to this region may have caused its earlier response to the climate amelioration after a cold/dry event, such as the Younger Dryas and Heinrich-1, compared to other regions on the Plateau. Furthermore, gorge-derived monsoon air masses that blew through the lowest-latitude region are highly likely to have more significantly influenced the onset of the climate amelioration after a cold/dry event even in the southwestern, south-central, and southeastern regions, rather than the Yarlung Zangbo-derived monsoon air masses. Therefore, this caused the subsequent expansion of the Indian summer monsoon (ISM) over the Plateau. Thus, with its unique geological setting, the lowest-latitude region has presumably played a critical role as the key region, i.e. the initiator, for the early evolution of the ISM on the Tibetan Plateau by responding to climate amelioration after cold/dry events more rapidly than any other region and drawing gorge-derived monsoon air masses strongly toward the region.
机译:为了更好地了解所报告的古老气候特征和最低纬度地区的底层机制(类似于28度N至29度30'n),其中12个主要河道横跨喜马拉雅山脉,我们的目标是阐明基于夏季季风和沉淀的ΔO-18的空间变化的地区现代季风空气群体的主要来源和行为,夏季季季季节季节。我们的主要研究结果如下:河道,高山范围轴承广泛的密集植被,最低纬度地区的较强的太阳能呈现特性可能是一个延长的时期,作为强烈绘制大量水分的基本地质环境。印度洋走向该地区,而不通过Yarlung Zangbo盆地。与该地区特定于该地区的这种地区的这种地质环境的组合可能导致其与高原上的其他地区相比,较年轻的Dryas和Heinrich-1之后对气候改善的反应。此外,距离最低纬度地区的峡谷衍生的季风空气群体甚至在寒冷/干旱事件中甚至在西南部,南部和东南部地区,而且比雅隆Zangbo衍生的季风空气质量。因此,这导致印度夏季季风(ISM)的随后扩展了高原。因此,利用其独特的地质环境,最低纬度地区已经推测作为关键区域,即引发器,即引发器,即在藏高高原上的ISM早期演变,通过响应冷/干事件后的气候改善,对ISM的早期演变进行了关键作用迅速比任何其他地区都迅速地向该地区强烈地绘制峡谷衍生的季风空气肿块。

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