The Morphogenic Layer of the Atmosphere,
Abstract
In the atmospheric layer immediately above uneven terrain, wind speeds and turbulence are either diminished or accelerated because of variations in the local relief, vegetation, and heights of man-made structures. In this layer, these factors tend to reduce turbulence more than wind speed. Radiation is also affected but to a lesser extent than wind speed. The relationship between valley climate and vegetation is close. Wind measurements are of minor value since they represent only small areas and short periods of time. The concept of a morphogenic atmospheric layer makes possible many satisfactory interpretations of meteorological phenomena without negating physical relationships. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 19, 1969
- Accession Number
- AD0864861
Entities
People
- G. Flemming
Organizations
- National Air and Space Intelligence Center