Self‐consistency between wind stress, wave spectrum, and wind‐induced wave growth for fully rough air‐sea interface

G Caudal - Journal of Geophysical Research: Oceans, 1993 - Wiley Online Library
When the flow at the air‐sea interface is aerodynamically rough (ie, for wind speeds above
7.5 ms− 1, typically), then form drag on the roughness elements accounts for virtually all the …

Self-consistency between wind stress, wave spectrum, and wind-induced wave growth for fully rough air-sea interface

GR Caudal - Journal of Geophysical Research, 1993 - ui.adsabs.harvard.edu
When the flow at the air-sea interface is aerodynamically rough (ie, for wind speeds above
7.5 ms-1, typically), then form drag on the roughness elements accounts for virtually all the …

Self-consistency between wind stress, wave spectrum, and wind-induced wave growth for fully rough air-sea interface

G Caudal - Journal of Geophysical Research, 1993 - osti.gov
When the flow at the air-sea interface is aerodynamically rough (ie, for wind speeds above
7.5 m/s, typically), then form drag on the roughness elements accounts for virtually all the …

Self‐consistency between wind stress, wave spectrum, and wind‐induced wave growth for fully rough air‐sea interface

G Caudal - 1993 - arch.neicon.ru
When the flow at the air‐sea interface is aerodynamically rough (ie, for wind speeds above
7.5 ms< sup>− 1, typically), then form drag on the roughness elements accounts for virtually …

[引用][C] Self-consistency between wind stress, wave spectrum, and wind-induced wave growth for fully rough air-sea interface

G CAUDAL - Journal of geophysical research, 1993 - pascal-francis.inist.fr
Self-consistency between wind stress, wave spectrum, and wind-induced wave growth for
fully rough air-sea interface CNRS Inist Pascal-Francis CNRS Pascal and Francis …

[引用][C] Self-consistency between wind stress, wave spectrum, and wind-induced wave growth for fully rough air-sea interface

G CAUDAL - Journal of geophysical research, 1993 - American Geophysical Union