Temporal and spatial variation of the drag coefficient of a developing sea under steady wind‐forcing
PA Hwang - Journal of Geophysical Research: Oceans, 2005 - Wiley Online Library
Field data indicate convincingly that the drag coefficient of the ocean surface is sea‐state
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
[PDF][PDF] Temporal and spatial variation of the drag coefficient of a developing sea under steady wind-forcing
PA Hwang - J. Geophys. Res, 2005 - researchgate.net
[I] Field data indicate convincingly that the drag coefficient of the ocean surface is seastate
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
[引用][C] Temporal and spatial variation of the drag coefficient of a developing sea under steady wind-forcing
PA HWANG - Journal of geophysical research, 2005 - pascal-francis.inist.fr
Temporal and spatial variation of the drag coefficient of a developing sea under steady wind-forcing
CNRS Inist Pascal-Francis CNRS Pascal and Francis Bibliographic Databases Simple …
CNRS Inist Pascal-Francis CNRS Pascal and Francis Bibliographic Databases Simple …
Temporal and spatial variation of the drag coefficient of a developing sea under steady wind-forcing
PA Hwang - Journal of Geophysical Research (Oceans), 2005 - ui.adsabs.harvard.edu
Field data indicate convincingly that the drag coefficient of the ocean surface is sea-state
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
Temporal and spatial variation of the drag coefficient of a developing sea under steady wind-forcing
PA Hwang - J. Geophys. Res, 2005 - apps.dtic.mil
Field data indicate convincingly that the drag coefficient of the ocean surface is sea-state
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …
dependent. As a result, under steady forcing by a constant wind velocity the wind stress on …