THE STRUCTURE OF THE WIND-VELOCITY AND TEMPERATURE FIELDS IN THE ATMOSPHERIC SURFACE BOUNDARY LAYER.
Abstract
The term surface is used to designate the lowest layer of air, which is several tens of meters thick and in which the Coriolis force may be neglected.
Document Details
- Document Type
- Technical Report
- Publication Date
- Dec 01, 1965
- Accession Number
- AD0628973
Entities
People
- A. S. Monin
Organizations
- American Meteorological Society