Mechanism of negative disturbances of the midlatitude F2-region

Details Mechanism of negative disturbances of the midlatitude F2-region Mechanism of negative disturbances of the midlatitude F2-region

Apr 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990ge%26ae..30..255m&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 30, Mar.-Apr. 1990, p. 255-260. In Russian.

Computer Science

Sound

F 2 Region, Ionospheric Disturbances, Magnetic Storms, Midlatitude Atmosphere, Satellite Sounding, Thermosphere, Geomagnetism, Nitrogen, Oxygen

Scientific paper

The mechanism behind the formation of the negative disturbance of n(e)mF2 during the substorm of Jan. 25, 1974 is investigated on the basis of observations of f0F2 at the Winnipeg and Boulder stations as well as on the basis of AE-C satellite measurements of thermospheric parameters. It is shown that the observed decrease of n(e)mF2 can be explained in the framework of the traditional approach to the description of the midlatitude F2-region; thus, there is no need to revise the existing conception of the formation of negative disturbance of n(e)mF2. It is is noted, however, that the hypothesis of Rishbeth and Fuller-Rowell (1987) concerning increases in the O/N2 ratio during storms is in need of revision.

Affiliated with

Also associated with

No associations

Rating

Mechanism of negative disturbances of the midlatitude F2-region does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Mechanism of negative disturbances of the midlatitude F2-region, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Mechanism of negative disturbances of the midlatitude F2-region will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1380817