z-logo
open-access-imgOpen Access
Remote sensing of mesospheric temperature and O 2 ( 1 Σ) band volume emission rates with the high‐resolution Doppler imager
Author(s) -
Ortland D. A.,
Hays P. B.,
Skinner W. R.,
Yee J.H.
Publication year - 1998
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/97jd02794
Subject(s) - thermosphere , mesopause , mesosphere , equator , volume (thermodynamics) , brightness , doppler effect , atmospheric sciences , physics , oscillation (cell signaling) , brightness temperature , airglow , computational physics , environmental science , stratosphere , ionosphere , optics , latitude , geophysics , chemistry , biochemistry , quantum mechanics , astronomy
An algorithm for obtaining temperatures and volume emission rate profiles in the mesosphere and lower thermosphere from HRDI measurements is described. Temperature and volume emission rates are derived via perturbation theory by comparing measured brightness to brightness computed from the forward model described here. Error analysis shows that the method recovers the temperatures with an error of 7° K and volume emission rates with an error of 3% from 80 to 100 km, providing global measurements of these fields in this altitude range for the first time. Results show the structure of the cold summer mesopause near the poles, the semiannual oscillation, and the diurnal tidal oscillations at the equator.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here