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Investigation of the 'elevated heat pump' hypothesis of the Asian monsoon using satellite observations

机译:利用卫星观测资料研究亚洲季风的“高热泵”假说

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摘要

The "elevated heat pump" (EHP) hypothesis has been a topic of intensiveresearch and controversy. It postulates that aerosol-induced anomalous mid-and upper-tropospheric warming in the Himalayan foothills and above theTibetan Plateau leads to an early onset and intensification of Asian monsoonrainfall. This finding is primarily based on results from a NASAfinite-volume general circulation model run with and without radiativeforcing from different types of aerosols. In particular, black carbonemissions from sources in northern India and dust from Western China,Afghanistan, Pakistan, the Thar Desert, and the Arabian Peninsula drive themodeled anomalous heating. Since the initial discussion of the EHP hypothesisin 2006, the aerosol–monsoon relationship has been investigated usingvarious modeling and observational techniques. The current study takes anovel observational approach to detect signatures of the "elevated heatpump" effect on convection, precipitation, and temperature for contrastingaerosol content years during the period of 2000–2012. The analysis benefitsfrom unique high-resolution convection information inferred from Meteosat-5observations as available through 2005. Additional data sources includetemperature data from the NCEP/NCAR Reanalysis and the European Reanalysis(ERA-Interim) precipitation data from the Global Precipitation ClimatologyProject (GPCP), aerosol optical depth from the Multi-angle ImagingSpectroradiometer (MISR) and the Moderate Resolution ImagingSpectroradiometer (MODIS), and aerosol optical properties from the Modern-EraRetrospective Analysis for Research and Applications (MERRA) aerosolreanalysis. Anomalous upper-tropospheric warming and the early onset andintensification of the Indian monsoon were not consistently observed duringthe years with high loads of absorbing aerosols. Possibly, model assumptionsand/or unaccounted semi-direct aerosol effects caused the disagreementbetween observed and hypothesized behavior.
机译:“高热泵”(EHP)假说一直是深入研究和争议的话题。它假设在喜马拉雅山麓和西藏高原以上,由气溶胶引起的异常对流层中和上对流层变暖导致亚洲季风降雨的早期发作和加剧。该发现主要基于NASA有限体积通用循环模型的结果,该模型在有和没有来自不同类型气溶胶的辐射强迫下运行。特别是来自印度北部的黑碳排放以及来自中国西部,阿富汗,巴基斯坦,塔尔沙漠和阿拉伯半岛的粉尘推动了异常加热。自2006年首次对EHP假设进行讨论以来,已经使用各种建模和观测技术研究了气溶胶与季风之间的关系。当前的研究采用anovel观测方法,以检测2000-2012年期间对比气溶胶含量年的“高热泵”对流,降水和温度影响的特征。该分析得益于从Meteosat-5观测获得的独特高分辨率高分辨率对流信息(可获取到2005年)。其他数据源包括来自NCEP / NCAR再分析的温度数据和来自全球降水气候项目(GPCP)的欧洲再分析(ERA-Interim)降水数据,多角度成像光谱仪(MISR)和中等分辨率成像光谱仪(MODIS)的气溶胶光学深度,以及现代研究和应用回顾性分析(MERRA)气溶胶分析的气溶胶光学特性。在大量吸收气溶胶的年份中,并没有持续观测到对流层上层异常变暖以及印度季风的早期发作和加剧。模型假设和/或未解释的半直接气溶胶效应可能导致观察到的行为与假设行为之间的分歧。

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