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Enhanced trans-Himalaya pollution transport to the Tibetan Plateau by cut-off low systems

机译:通过切断低层系统加强对喜马拉雅山的跨喜马拉雅山污染转移

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Long-range?transport followed by deposition of black carbon on glaciers of Tibet is one of the key issues of climate research as it induces changes on radiative forcing and subsequently impacting the melting of glaciers. The transport mechanism, however, is not well understood. In this study, we use short-lived reactive aromatics as proxies to diagnose transport of pollutants to Tibet. In situ observations of short-lived reactive aromatics across the Tibetan Plateau are analyzed using a regional chemistry and transport model. The model performance using the current emission inventories over the region is poor due to problems in the inventories and model transport. Top-down?emissions constrained by satellite observations of glyoxal are a factor of 2–6 higher than the a priori emissions over the industrialized Indo-Gangetic Plain. Using the top-down emissions, agreement between model simulations and surface observations of aromatics improves. We find enhancements of reactive aromatics over Tibet by a factor of 6 on average due to rapid transport from India and nearby regions during the presence of a high-altitude cut-off low system. Our results suggest that the cut-off low system is a major pathway for long-range transport of pollutants such as black carbon. The modeling analysis reveals that even the state-of-the-science high-resolution reanalysis cannot simulate this cut-off low system accurately, which probably explains in part the underestimation of black carbon deposition over Tibet in previous modeling studies. Another model deficiency of underestimating pollution transport from the south is due to the complexity of terrain, leading to enhanced transport. It is therefore challenging for coarse-resolution global climate models to properly represent the effects of long-range transport of pollutants on the Tibetan environment and the subsequent consequence for regional climate forcing.
机译:在西藏冰川上进行黑碳的长距离运输是气候研究的关键问题之一,因为它引起了辐射强迫的变化,进而影响了冰川的融化。然而,运输机制还没有被很好地理解。在这项研究中,我们使用寿命短的反应性芳族化合物作为诊断污染物向西藏的运输的代理。使用区域化学和运移模型分析了青藏高原短寿命反应性芳烃的原位观察。由于清单和模型传输方面的问题,使用该地区当前排放清单的模型性能很差。与工业化的印度恒河平原相比,由乙二醛的卫星观测所限制的自上而下的排放量比先验排放量高2-6倍。使用自上而下的排放,可以提高模型模拟与芳烃表面观察之间的一致性。我们发现,由于在高海拔低矮系统的存在下从印度和附近地区快速运输,西藏地区的活性芳香剂平均增加了6倍。我们的结果表明,低浓度截留系统是污染物(如黑碳)远程运输的主要途径。建模分析表明,即使是最先进的高分辨率再分析也无法准确地模拟该临界低层系统,这可能部分解释了先前建模研究中对黑碳沉积的低估。低估从南方来的污染的另一个模型缺陷是由于地形的复杂性,导致了运输的增加。因此,对于粗分辨率的全球气候模型而言,正确地表示污染物的远程迁移对西藏环境的影响以及对区域气候强迫的后续后果具有挑战性。

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