Satellite Oceanography
Abstract
Renewed interest in the inverted barometer effect has been spurred by altimetry, specifically, the accuracy of measurements of TOPEX/Poseidon. The change in SSH associated with this effect produces anomalous oceanographic features. it is, therefore, desirable to remove this signal. Currently, only one component of the inverted barometer is understood, the static response. The total effect was studied through implementation of a barotropic model. A region in the North Pacific with a February/March '93 time period was selected as an appropriate test area. The issue was addressed with model runs driven by 6- hourly FNOC wind and pressure fields to examine both the static and dynamic elements of the inverted barometric response. Methodology, Barometer, Altimeter
Document Details
- Document Type
- Technical Report
- Publication Date
- Jan 01, 1994
- Accession Number
- ADA277286
Entities
Organizations
- University of Colorado Boulder