The Performance Of A Coupled 1-D Circulation And Bottom Boundary Layer Model With Surface Wave Forcing
-
2001
Details
-
Personal Author:
-
NOAA Program & Office:
-
Sea Grant Program:
-
Description:The authors explore how a coupled numerical hydrodynamic 1- D circulation model and bottom boundary layer model can more accurately simulate the effects of the nonlinear interaction between current and prevailing surface gravity effects of the nonlinear interaction between current and prevailing surface gravity waves on local bottom stress. They focus on storm wave conditions typical to the Gulf of Maine. Specifically, National Data Buoy Center buoy measurements in the Gulf of Maine document the temporal variability of the significant wave height at the dominant storm wave period of about 12 seconds. Surface waves of this period interact with the bottom in water depths less than about 80 m.
-
Series:
-
Sea Grant Document Number:NHU-T-01-007
-
Document Type:
-
Rights Information:Public Domain
-
Compliance:Library
-
Download URL:
-
File Type:
-
Collection(s):
-
Main Document Checksum:urn:sha256:35a1fdccc2a8324b9a39bbcf59fd2e06197f76721b6537f08a87baa3e2c2618c
The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles,
guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the
NOAA IR retains documents in their original published format to ensure public access to scientific information.
You May Also Like