THE STRUCTURE OF THERMAL CONVECTION IN THE LOWER ATMOSPHERE.
Abstract
An experimental study of atmospheric convection in lowest 100 m under conditions of strong surface heating and light winds is presented. Using an instrumented light aircraft, measurements were made of the fluctuating temperatures and vertical air speeds over a desert dry lake during the daytime. Root-mean-square values of these quantities and the convective heat flux were calculated and related to theoretical and laboratory results. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Feb 01, 1965
- Accession Number
- AD0619268
Entities
People
- Leonard O. Myrup
Organizations
- University of California, Los Angeles