The term 'meteor wind' is used for the mesosphere wind estimates derived from meteor trail drifts measurements. Ionized meteor trails are produced by meteoroids (meteor particles) which enter the Earth's atmosphere. A meteor trail moves in the atmosphere due to the neutral wind and magnetic field. The radial component of this movement is measured using meteor radar. Estimates of 'meteor wind' are derived for each direction (North, South, East, West) from the set of measurements of radial components using statistical characteristics of meteor parameter distributions and parameters of antenna pattern. The 'hourly meteor rate' which is the number of registered meteors for which reliable estimates of radial components can be obtained can also be determined. Meteoroids occur in the height interval 80-100 km and are centered at 92-95 km (maximum for the apex time, near 6 a.m. LT, and minimum for anti-apex time, near 6 p.m. LT ).
The GLOBMET (Global Meteor Observation System) Project (1982-1990) was one of the MAP projects aimed at intensifying research in Meteor Geophysics and Meteor Astronomy in the 1980's by making wider use of the latest achievements in this field and expanding international coordination in meteor research. The main objective of the project was to organize a network of meteor observatories, which will provide experimental data : (1) for testing of models of atmospheric circulation which include the meteor region; (2) on the influx of meteors and the distribution of meteoroids in the neighborhood of the Earth; and (3) for testing models of meteoroid/atmosphere interaction.
The MAP (Middle Atmosphere Program) was an international cooperative enterprise scheduled for 1982-1985 and then continued as the Middle Atmosphere Cooperation (MAC) for 1986-1988. Its chief objective was to obtain a comprehensive understanding of the structure, chemistry, energetics, and dynamics of the middle atmosphere. For the purposes of the MAP, the middle atmosphere was defined to be the atmosphere from the tropopause to the lower thermosphere, that is, the region from about 10 to 100 km in altitude. The factors enumerated above all interact with each other in such complicated ways that the study of each of them in isolation leads to unreliable or even anomalous results. This can be remedied by a more integrated and unified attack - specifically by the coordination, in time and location, of observations of the various factors, and by cooperation in the interpretation of the results. This was the rationale for MAP. The operational basis for MAP was an international plan for coordinated observations from spacecraft, ground-based facilities, aircraft, balloons and rockets. The MAP also encouraged cooperative data management, information exchange on all appropriate time scales, and interaction between observationalists, modelers, and theoreticians.
Entry_ID: MAPDAMW021 (MD Identifier: 2048)
Temporal Coverage:
From: 1980-01-01 TO: 1985-02-16
Geographic Coverage:
Southwest Extent: 39N,37E Northeast Extent: 57N,104E
Source:
GROUND STATIONS
Sensor:
RADAR
Storage Media:
1 Magnetic Tape 1600 bpi
Campaign/Project:
GLOBMET>Global Meteor Observation System
MAP>Middle Atmosphere Program
Discipline, Subdiscipline:
EARTH SCIENCE > ATMOSPHERE
Location Keyword:
ASIA
EUROPE
IONOSPHERE
MESOSPHERE
MID-LATITUDE
Parameter Group, Parameter:
ATMOSPHERIC DYNAMICS > WINDS
General Keywords:
CLIMATOLOGY
HOURLY DATA
IDN_NODE GSFC/WDCB
MESOSPHERE WINDS
STATISTICS
UPPER AIR
Revision Date: 1991-11-05
Archive:
WDC-B>World Data Center B
Data Set ID: STM201
Contact: NECHITAILENKO, VITALY A.
Soviet Geophysical Committee
Molodezhnaya, 3
Moscow 117296
USSR
Electronic Mail: INTERNET> SGC@NODE.IAS.MSK.SU
Phone: (095)-930-56-49
FAX (095)-930-55-09
Entry Author: SCIALDONE, JOHN N.
Hughes STX
7701 Greenbelt Road, Suite 400
Greenbelt, MD 20770
USA
Electronic Mail: INTERNET> SCIALDONE@NSSDCA.GSFC.NASA.GOV
NSI/DECnet> NCF::SCIALDONE
Phone: (301) 441-4214
Information in this entry provided by WDCB
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