INVERSION OF THE OMEGA-EQUATION.
Abstract
A formal method of inversion of the baroclinic Omega-equation of the quasigeostrophic models is proposed. An application to satellite meteorology is suggested, where a 500 millibar surface is obtained in regions of sparse data from a knowledge of the surface map and the vertical motion field. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Apr 01, 1964
- Accession Number
- AD0603571
Entities
People
- T. N. Krishnamurti
Organizations
- University of California, Los Angeles