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SATELLITE ALTIMETRY: A REVOLUTION IN UNDERSTANDING THE WAVE CLIMATE

机译:卫星测高:对波浪气候的认识的一次革命

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Before the advent of radar altimeters our understanding of the world's climate was based on a few instruments moored off the coats of Europe, Japan and North America and visual observations taken from merchant ships. This information was patchy and in many cases of poor quality. It was difficult to relate what was happening at one location with another. The advent of the radar altimeter has changed all that. We had a series of satellite instruments that made consistent measurements of significant wave height across the globe. Initial work concentrated on simply mapping the wave climate and investigating means and seasonal variation. However with longer records came the ability to look at inter-annual variability. It had been known since the late 70's that wave heights measured at a few sites around the North East Atlantic had shown a dramatic increase. It was only the combination of spatial and temporal sampling from the altimeter that allowed us to discover the extent of the changes and how they related to the North Atlantic Oscillation index. Of course it is not only the mean wave conditions that are important, extreme waves are of vital interest to naval architects and the designers of offshore structures. Being able to estimate extreme waves from altimeter data enables us for the first time to establish what extreme conditions might be in any part of the world. At present we do not exploit the spatial nature of the altimeter data in our estimation of the extremes but this is an active research area. Research into further uses of altimeter data for looking at the wave climate continues apace. Algorithms for new parameters such as wave period are being developed. Real time applications are appearing. For such applications space-time sampling is an issue and people are coming up with innovative ideas using constellations of cheap altimeters. In this paper we review the progress made in the study of wave climate using the radar altimeter. In addition we look into current directions of new research and where we might be going next.
机译:在雷达高度计问世之前,我们对欧洲气候的了解是基于欧洲,日本和北美外层系泊的一些仪器以及从商船上进行的视觉观察得出的。该信息不完整,在许多情况下质量很差。很难将一个地点发生的事情与另一地点发生的事情联系起来。雷达高度计的出现改变了这一切。我们拥有一系列卫星仪器,可以对全球范围内的重要波高进行一致的测量。最初的工作集中在简单地绘制海浪气候以及调查手段和季节变化上。但是,随着记录的增加,可以查看年际变化。自70年代末以来,人们已经知道,在东北大西洋周围的几个地点测得的波高已显示出惊人的增长。只是从高度计进行的空间和时间采样的组合,才使我们能够发现变化的程度以及它们与北大西洋涛动指数的关系。当然,不仅平均波浪条件很重要,极端波浪对于海军建筑师和海上结构设计师也至关重要。能够根据高度计数据估算极端波,这使我们首次确定了世界任何地方可能存在的极端条件。目前,我们在估算极端值时并未利用高度计数据的空间性质,但这是一个活跃的研究领域。对高度计数据进一步用于观察海浪气候的研究仍在继续。正在开发诸如波浪周期等新参数的算法。实时应用程序正在出现。对于此类应用,时空采样是一个问题,人们正在使用廉价的高度计星座提出创新的想法。在本文中,我们回顾了使用雷达高度计在波浪气候研究中取得的进展。此外,我们研究了新研究的当前方向以及下一步的发展方向。

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