193-194The variation of the effective collision frequency of electrons veff with solar zenith angle has been studied around sunrise and sunset by group retardation method [Appleton, E. V., Nature, Lond., 135(1935), 618] at different radio frequencies. The variation is found to be steeper at sunrise than at sunset. Taking a linear relationship between 'veff' and f2, the square of radio frequency, a rough estimate of the electron temperature Te has been made. The resulting values of Te at sunrise and sunset are found to be 1113 and 987o K., respectively
105-111Analytic expressions are given for the temperature dependent monoenergetic (vmln) and the two...
Presuming the total life-time for recombination of molecular ions with electrons remains constant at...
The local time, seasonal and solar activity variations of electron temperature T-e measured by the S...
138-140Electron-ion collision frequencies were calculated for the summer months of the years 1959-19...
The theory regarding electron temperatures within the F region of the ionosphere are reviewed. The r...
The theory regarding electron temperatures within the F region of the ionosphere are reviewed. The r...
160-163The effective collision frequency of electrons in the height range 100-460 km has been comput...
159-161Incoherent scatter radar measurements of electron temperature (Te) and electron concentration...
132-134Electron concentration profiles during sunrise and sunset periods, observed with the Arecibo ...
The daytime measurements of electron temperature (Te) and concentration (Ne) from incoherent scatter...
Incoherent scatter radar data from Arecibo, for high solar activity (HSA) (1989-1990) as well as for...
Electron and ion temperatures, derived from backscatter spectra, are examined during the current ris...
251-256The daytime measurements of electron temperature (Te) and concentration (Ne) from incoherent ...
Earth’s lower ionosphere is the region where terrestrial weather and space weather come together. He...
28-31The electron collision frequency variations in the E and F regions have been determined by many...
105-111Analytic expressions are given for the temperature dependent monoenergetic (vmln) and the two...
Presuming the total life-time for recombination of molecular ions with electrons remains constant at...
The local time, seasonal and solar activity variations of electron temperature T-e measured by the S...
138-140Electron-ion collision frequencies were calculated for the summer months of the years 1959-19...
The theory regarding electron temperatures within the F region of the ionosphere are reviewed. The r...
The theory regarding electron temperatures within the F region of the ionosphere are reviewed. The r...
160-163The effective collision frequency of electrons in the height range 100-460 km has been comput...
159-161Incoherent scatter radar measurements of electron temperature (Te) and electron concentration...
132-134Electron concentration profiles during sunrise and sunset periods, observed with the Arecibo ...
The daytime measurements of electron temperature (Te) and concentration (Ne) from incoherent scatter...
Incoherent scatter radar data from Arecibo, for high solar activity (HSA) (1989-1990) as well as for...
Electron and ion temperatures, derived from backscatter spectra, are examined during the current ris...
251-256The daytime measurements of electron temperature (Te) and concentration (Ne) from incoherent ...
Earth’s lower ionosphere is the region where terrestrial weather and space weather come together. He...
28-31The electron collision frequency variations in the E and F regions have been determined by many...
105-111Analytic expressions are given for the temperature dependent monoenergetic (vmln) and the two...
Presuming the total life-time for recombination of molecular ions with electrons remains constant at...
The local time, seasonal and solar activity variations of electron temperature T-e measured by the S...