INFLUX OF METEOR PARTICLES IN THE UPPER ATMOSPHERE OF THE EARTH AS DETERMINED FROM STRATOSPHERIC CORONAGRAPH OBSERVATIONS
Abstract
This paper reports the observations of sky brightness near the sun at altitudes up to 25 km, using balloons. From the observed brightness the particle density is deduced as a function of altitude and divided into a component diffusing up from below and one settling from above. The deduced influx of particles in the size range of 0.1 to 2.8 microns radius is compared with rocket and other observations.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jan 01, 1961
- Accession Number
- AD0612572
Entities
People
- G. Newkirk Jr.
- J. A. Eddy
Organizations
- High Altitude Observatory