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Autor:
Gelman, Mel, Laver, Jim
Publikováno v:
Bulletin of the American Meteorological Society. Sep2000, Vol. 81 Issue 9, p2235. 2p.
Publikováno v:
Bulletin of the American Meteorological Society. 72:50-56
The tremendous interest in upper-air measurement quality by the meteorological community brought together experts from many agencies at a Workshop on Upper-Air Measurements and Instruments. The workshop was held at NASA's Wallops Island facility on 1
Autor:
Francis J. Schmidlin, Robert Leviton, Frederick G. Finger, Melvyn E. Gelman, Bruce W. Kennedy
Publikováno v:
Journal of the Atmospheric Sciences. 32:1705-1714
Results of two experiments involving intercomparisons of rocketsonde measurements of temperature and wind data in the 25 to 80 km altitude region in the CIMO (Commission for Instruments and Methods of Observations) program during September 1973 are r
Publikováno v:
Advances in Space Research. 4:29-32
The National Meteorological Center of the National Oceanic and Atmospheric Administration (NOAA) has archived global, daily synoptic analyses and computer gridded fields of geopotential height and temperature for 8 stratospheric pressure levels (70,
Publikováno v:
Bulletin of the American Meteorological Society. 66:413-420
A wide variety of current climate products are being developed, produced, and disseminated to a diverse group of users by the Climate Analysis Center (CAC). The Climate Assessment Data Base (CADB), a major resource used to generate many of these prod
Publikováno v:
Monthly Weather Review. 92:243-250
The diurnal change in temperature and height measured by the new U.S. Weather Bureau outrigger radiosonde at and above 100 mb. has been determined from pairs of successive radiosonde observations taking place in daylight and darkness. Analyzed graphs
Publikováno v:
Science. 167:16-25
Publikováno v:
Monthly Weather Review. 101:244-251
The usefulness of Nimbus 4 satellite infrared spectrometer (SIRS)-derived temperature and height data for constant-pressure analyses at stratospheric levels is investigated by comparing SIRS data with rawinsonde observations and objective analyses of
Publikováno v:
Journal of the Atmospheric Sciences. 25:1116-1128
An attempt is made to determine empirically the diurnal temperature range between 24 and 36 km, by using means of 12-hr temperature differences obtained from successive rawinsonde observations over North America. With a technique for isolating effect