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Progress in satellite remote sensing for studying physical processes at the ocean surface and its borders with the atmosphere and sea ice

机译:用于研究海面及其与大气和海冰边界的物理过程的卫星遥感技术的进展

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Physical oceanography is the study of physical conditions, processes and variables within the ocean, including temperature-salinity distributions, mixing of the water column, waves, tides, currents and air-sea interaction processes. Here we provide a critical review of how satellite sensors are being used to study physical oceanography processes at the ocean surface and its borders with the atmosphere and sea ice. The paper begins by describing the main sensor types that are used to observe the oceans (visible, thermal infrared and microwave) and the specific observations that each of these sensor types can provide. We then present a critical review of how these sensors and observations are being used to study: (i) ocean surface currents, (ii) storm surges, (iii) sea ice, (iv) atmosphere-ocean gas exchange and (v) surface heat fluxes via phytoplankton. Exciting advances include the use of multiple sensors in synergy to observe temporally varying Arctic sea ice volume, atmosphere-ocean gas fluxes, and the potential for four-dimensional water circulation observations. For each of these applications we explain their relevance to society, review recent advances and capability, and provide a forward look at future prospects and opportunities. We then more generally discuss future opportunities for oceanography-focused remote sensing, which includes the unique European Union Copernicus programme, the potential of the International Space Station and commercial miniature satellites. The increasing availability of global satellite remote-sensing observations means that we are now entering an exciting period for oceanography. The easy access to these high quality data and the continued development of novel platforms is likely to drive further advances in remote sensing of the ocean and atmospheric systems.
机译:物理海洋学是对海洋中的物理条件,过程和变量的研究,包括温度-盐度分布,水柱混合,波浪,潮汐,洋流和海-气相互作用过程。在这里,我们对如何使用卫星传感器研究海洋表面及其与大气和海冰的边界处的物理海洋学过程进行了严格的审查。本文首先介绍用于观测海洋的主要传感器类型(可见光,热红外和微波)以及每种传感器类型可以提供的具体观测结果。然后,我们将对如何使用这些传感器和观测资料进行批判性回顾:(i)海面洋流,(ii)风暴潮,(iii)海冰,(iv)大气-海洋气体交换和(v)地表通过浮游植物的热通量。令人兴奋的进展包括协同使用多个传感器来观察随时间变化的北极海冰量,大气-海洋气体通量以及进行多维水循环观测的潜力。对于这些应用程序中的每一个,我们都将说明它们与社会的相关性,回顾最新的进展和功能,并对未来的前景和机遇进行前瞻性研究。然后,我们将更广泛地讨论以海洋学为重点的遥感技术的未来机会,其中包括独特的欧盟哥白尼计划,国际空间站的潜力和商业微型卫星。全球卫星遥感观测的可用性不断提高,这意味着我们现在正进入海洋学一个令人兴奋的时期。轻松访问这些高质量数据以及不断开发新颖的平台可能会推动海洋和大气系统遥感的进一步发展。

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