Author: H. T. Wadzinski
Publisher:
ISBN:
Category : Cross sections (Nuclear physics)
Languages : en
Pages : 244
Book Description
The purpose of this report is to provide a set of low energy (0-300 eV) cross sections for use in calculating the photoelectron flux in the terrestrial daytime ionosphere. Also given are data on the neutral particle composition of the upper atmosphere and ionizing electromagnetic radiation from the sun.
Low Energy Electron and Photon Cross Sections for O, N2, and O2, and Related Data
Author: H. T. Wadzinski
Publisher:
ISBN:
Category : Cross sections (Nuclear physics)
Languages : en
Pages : 244
Book Description
The purpose of this report is to provide a set of low energy (0-300 eV) cross sections for use in calculating the photoelectron flux in the terrestrial daytime ionosphere. Also given are data on the neutral particle composition of the upper atmosphere and ionizing electromagnetic radiation from the sun.
Publisher:
ISBN:
Category : Cross sections (Nuclear physics)
Languages : en
Pages : 244
Book Description
The purpose of this report is to provide a set of low energy (0-300 eV) cross sections for use in calculating the photoelectron flux in the terrestrial daytime ionosphere. Also given are data on the neutral particle composition of the upper atmosphere and ionizing electromagnetic radiation from the sun.
Low Energy Electron and Photon Cross Sections for O, N2, and O2, and Related Data
Author: H. T. Wadzinski
Publisher:
ISBN:
Category : Cross sections (Nuclear physics).
Languages : en
Pages : 339
Book Description
The purpose of this report is to provide a set of low energy (0-300 eV) cross sections for use in calculating the photoelectron flux in the terrestrial daytime ionosphere. Also given are data on the neutral particle composition of the upper atmosphere and ionizing electromagnetic radiation from the sun.
Publisher:
ISBN:
Category : Cross sections (Nuclear physics).
Languages : en
Pages : 339
Book Description
The purpose of this report is to provide a set of low energy (0-300 eV) cross sections for use in calculating the photoelectron flux in the terrestrial daytime ionosphere. Also given are data on the neutral particle composition of the upper atmosphere and ionizing electromagnetic radiation from the sun.
Bibliography of Low Energy Electron and Photon Cross Section Data (through December 1974)
Author: Lee Joseph Kieffer
Publisher:
ISBN:
Category : Cross sections (Nuclear physics)
Languages : en
Pages : 224
Book Description
Publisher:
ISBN:
Category : Cross sections (Nuclear physics)
Languages : en
Pages : 224
Book Description
Scientific and Technical Aerospace Reports
Author:
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 1252
Book Description
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 1252
Book Description
Energy Research Abstracts
Author:
Publisher:
ISBN:
Category : Power resources
Languages : en
Pages : 632
Book Description
Publisher:
ISBN:
Category : Power resources
Languages : en
Pages : 632
Book Description
Technical Abstract Bulletin
Nuclear Science Abstracts
Author:
Publisher:
ISBN:
Category : Nuclear energy
Languages : en
Pages : 912
Book Description
Publisher:
ISBN:
Category : Nuclear energy
Languages : en
Pages : 912
Book Description
Journal of Research of the National Bureau of Standards
Author: United States. National Bureau of Standards
Publisher:
ISBN:
Category : Chemistry
Languages : en
Pages : 474
Book Description
Publisher:
ISBN:
Category : Chemistry
Languages : en
Pages : 474
Book Description
Physics Briefs
Determination of Ionospheric Electron Density Profiles from Satellite UV Emission Measurements
Author: D. J. Strickland
Publisher:
ISBN:
Category : Ionospheric electron density
Languages : en
Pages : 74
Book Description
The possible use of satellite ultraviolet measurements to deduce the ionospheric electron density profile (EDP) on a global basis is discussed. A system concept is considered and analyzed which (a) develops and installs a UV sensor on the DMSP satellite and develops an associated automatic data processing (software) system, (b) utilities optical data together with DMSP electron density and temperature data to deduce the near real-time EDP near the satellite orbital plane, and (c) transmits this EDP data to be used together with ground-based ionosonde data and GPS total electron content data to specify the global EDP for systems users. The ionosonde and total electron content data would increase the EDP data base generated by the UV data and refine the UV based EDP where coincident data existed. This report considers (a) the daytime low to midlatitude ionosphere from 90 to 1000 km, (b) the nighttime midlatitude from about 250 km to 1000km, and (c) the auroral E layer from 90 to about 200 km for undisturbed conditions. The spatial resolution for the daytime and nighttime EDP is at least one vertical profile for each square 500 km on a side and for the auroral E layer at least one vertical profile for each square 50km on a side. Other ionospheric regions were not considered because of frequent occurrence of irregularities or highly variable transport conditions.
Publisher:
ISBN:
Category : Ionospheric electron density
Languages : en
Pages : 74
Book Description
The possible use of satellite ultraviolet measurements to deduce the ionospheric electron density profile (EDP) on a global basis is discussed. A system concept is considered and analyzed which (a) develops and installs a UV sensor on the DMSP satellite and develops an associated automatic data processing (software) system, (b) utilities optical data together with DMSP electron density and temperature data to deduce the near real-time EDP near the satellite orbital plane, and (c) transmits this EDP data to be used together with ground-based ionosonde data and GPS total electron content data to specify the global EDP for systems users. The ionosonde and total electron content data would increase the EDP data base generated by the UV data and refine the UV based EDP where coincident data existed. This report considers (a) the daytime low to midlatitude ionosphere from 90 to 1000 km, (b) the nighttime midlatitude from about 250 km to 1000km, and (c) the auroral E layer from 90 to about 200 km for undisturbed conditions. The spatial resolution for the daytime and nighttime EDP is at least one vertical profile for each square 500 km on a side and for the auroral E layer at least one vertical profile for each square 50km on a side. Other ionospheric regions were not considered because of frequent occurrence of irregularities or highly variable transport conditions.