摘要
Laboratory measurements using both wave probe (contact and optical) and radar confirm the existence of a new type of overshoot phenomenon in the wind-wave development processes. With the existence of this overshoot it becomes obvious that the past assumed simple power law relationship between the rms value of surface slope at a fixed wavelength and the wind stress is untenable. Since such a relationship is one of the key assumptions invoked in the development of algorithms used to date in scatterometry, we have re-examined the published scatterometer data and pointed out the implications of this overshoot phenomenon.-from Authors
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 3679-3687 |
頁數 | 9 |
期刊 | Journal of Geophysical Research E: Planets |
卷 | 89 |
發行號 | C3 |
DOIs | |
出版狀態 | 已出版 - 1984 |