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A theoretical study of the effect of subsurface oceanic bubbles on the enhanced aerosol optical depth band over the southern oceans as detected from MODIS and MISR

机译:从MODIS和MISR探测到的地下海洋气泡对南部海洋增强的气溶胶光学深度带影响的理论研究。

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Submerged oceanic bubbles, which have a much longer life span than whitecapsor bubble rafts, have been hypothesized to increase the water-leavingradiance and thus affect satellite-based estimates of water-leaving radianceto non-trivial levels. This study explores this effect further to determinewhether such bubbles are of sufficient magnitude to impact satellite aerosoloptical depth (AOD) retrievals through perturbation of the lower boundaryconditions. There has been significant discussion in the communityregarding the high positive biases in retrieved AODs in many remote oceanregions. In this study, for the first time, the effects of oceanic bubbleson satellite retrievals of AOD are studied by using a linked Second Simulationof a Satellite Signal in the Solar Spectrum (6S) atmospheric and HydroLightoceanic radiative transfer models. The results suggest an insignificantimpact on AOD retrievals in regions with near-surface wind speeds of lessthan 12 m s?1. However, the impact of bubbles on aerosol retrievalscould be on the order of 0.02–0.04 for higher wind conditions within thescope of our simulations (e.g., winds < 20 m ?1. This bias ispropagated to global scales using 1 year of Moderate Resolution ImagingSpectroradiometer (MODIS) and Advanced Microwave Scanning Radiometer EOS(AMSR-E) data to investigate the possible impacts of oceanic bubbles on anenhanced AOD belt observed over the high-latitude southern oceans (alsocalled the enhanced southern oceans anomaly, or ESOA) by some passive satellitesensors. Ultimately, this study is supportive of the null hypothesis:submerged bubbles are not the major contributor to the ESOA feature. Thissaid, as retrievals progress to higher and higher resolutions, such as fromairborne platforms, the uniform bubble correction in clean marine conditionsshould probably be separately accounted for against individual brightwhitecaps and bubble rafts.
机译:据推测,水下气泡的寿命比白cap气泡筏的寿命长得多,可以增加水的辐照度,从而将基于卫星的水的辐照度推算为非平凡水平。这项研究进一步探讨了这种影响,以确定这些气泡是否足以扰动较低边界条件,从而影响卫星气溶胶深度(AOD)的获取。关于许多偏远海洋区域中回收的AOD的高度积极偏见,社区中进行了大量讨论。在这项研究中,这是第一次,通过使用太阳光谱(6S)大气和水光海洋辐射传输模型中的卫星信号的链接第二模拟,研究了海洋气泡对AOD卫星取回的影响。结果表明,在近地表风速小于12 m s ?1 的地区,对AOD的恢复影响不显着。但是,在我们的模拟范围内(例如,风<20 m ?1 ),对于较高的风况,气泡对气溶胶回收的影响应该在0.02–0.04的数量级上。一年的中等分辨率成像光谱仪(MODIS)和高级微波扫描辐射仪EOS(AMSR-E)数据,用于研究在高纬度南部海洋(也称为增强南部海洋异常)上观察到的气泡对增强的AOD带的可能影响最终,这项研究支持零假设:淹没的气泡并不是ESOA功能的主要贡献者,这就是说,随着从空中平台进行的越来越高的分辨率检索,统一的气泡校正在干净的海洋条件下,应该针对个别的白头and和泡泡筏分别考虑在内。

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