FN Archimer Export Format
PT J
TI On the limiting aerodynamic roughness of the ocean in very strong winds
BT 
AF DONELAN, MA
   HAUS, BK
   REUL, Nicolas
   PLANT, WJ
   STIASSNIE, M
   GRABER, HC
   BROWN, OB
   SALTZMAN, ES
AS 1:;2:;3:;4:;5:;6:;7:;8:;
FF 1:;2:;3:PDG-DRO-DOPS-LOS;4:;5:;6:;7:;8:;
C1 Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA.
   Inst Francais Rech Exploitat Mer, F-29280 Plouzane, France.
   Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA.
   Technion Israel Inst Technol, Fac Civil Engn, IL-32000 Haifa, Israel.
   Univ Calif Irvine, Irvine, CA 92697 USA.
C2 UNIV MIAMI, USA
   IFREMER, FRANCE
   UNIV WASHINGTON, USA
   TECHNION ISRAEL INST TECHNOL, ISRAEL
   UNIV CALIF IRVINE, USA
SI BREST
SE PDG-DRO-DOPS-LOS
IN WOS Ifremer jusqu'en 2018
   copubli-int-hors-europe
IF 2.378
TC 556
UR https://archimer.ifremer.fr/doc/00000/10873/9230.pdf
LA English
DT Article
AB The aerodynamic friction between air and sea is an important part of the momentum balance in the development of tropical cyclones. Measurements of the drag coefficient, relating the tangential stress ( frictional drag) between wind and water to the wind speed and air density, have yielded reliable information in wind speeds less than 20 m/s ( about 39 knots). In these moderate conditions it is generally accepted that the drag coefficient ( or equivalently, the "aerodynamic roughness'') increases with the wind speed. Can one merely extrapolate this wind speed tendency to describe the aerodynamic roughness of the ocean in the extreme wind speeds that occur in hurricanes ( wind speeds greater than 30 m/s)? This paper attempts to answer this question, guided by laboratory extreme wind experiments, and concludes that the aerodynamic roughness approaches a limiting value in high winds. A fluid mechanical explanation of this phenomenon is given.
PY 2004
PD SEP
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 31
IS 18
UT 000224408200001
DI 10.1029/2004GL019460
ID 10873
ER

EF