Statistics of Vertical Shear from a Hemispheric Model
Abstract
Using surface atmospheric momentum and heat fluxes derived from the Fleet Numerical Oceanography Center's weather prediction models, a computation of inertial and Ekman shear was done for the upper 400 m of the North Pacific and North Atlantic. Two 60-day periods were considered in November and December of 1976 and 1980. A capability to predict these types of shear in real-time, or near real-time, is demonstrated using the Navy's TOPS(Thermodynamic Ocean Prediction System) model, A statistical analysis of the vertical shear and associated Richardson number revealed that the time variability of shear appears to be linked primarily to the synoptic time scales of weather events; and the spatial distribution of shear instability (0 or = Ri < or = 0.25) and high shear are closely related to the position of atmospheric fronts.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 01, 1983
- Accession Number
- ADA136179
Entities
People
- J. M. Harding
- R. H. Preller
- S. A. Piacsek
Organizations
- United States Naval Research Laboratory