Bottom-Up Determination of Air-Sea Momentum Exchange Under a Major Tropical Cyclone
Ewa Jarosz,*
Douglas A. Mitchell,
David W. Wang,
William J. Teague
As a result of increasing frequency and intensity of tropical
cyclones, an accurate forecasting of cyclone evolution and ocean
response is becoming even more important to reduce threats to
lives and property in coastal regions. To improve predictions,
accurate evaluation of the air-sea momentum exchange is required.
Using current observations recorded during a major tropical
cyclone, we have estimated this momentum transfer from the ocean
side of the air-sea interface, and we discuss it in terms of
the drag coefficient. For winds between 20 and 48 meters per
second, this coefficient initially increases and peaks at winds
of about 32 meters per second before decreasing.
Naval Research Laboratory, Stennis Space Center, MS 395295004, USA.
Present address: Exxon Mobil Upstream Research Company, Houston, TX 770276019, USA.
* To whom correspondence should be addressed. E-mail: ewa.jarosz{at}nrlssc.navy.mil