Zobrazeno 1 - 10
of 35
pro vyhledávání: '"R. P. Lowe"'
Autor:
F. J. Mulligan, R. P. Lowe
Publikováno v:
Annales Geophysicae, Vol 26, Pp 795-811 (2008)
OH-equivalent temperatures were derived from all of the temperature profiles retrieved in 2004 and 2005 by the ACE-FTS instrument in a 5 degree band of latitude centred on a ground-based observing station at Maynooth. A globally averaged OH volume
Externí odkaz:
https://doaj.org/article/6dbe8e4cb22a42edb0ffb73924fc9269
Publikováno v:
Annales Geophysicae, Vol 22, Pp 1549-1561 (2004)
Rotational temperatures derived from the OH(8–3) band may vary by ~18K depending on the choice of transition probabilities. This is of concern when absolute temperatures or trends determined in combination with measurements of other hydroxyl ban
Externí odkaz:
https://doaj.org/article/eabe183c7ed24ceeb422b7355f93c883
Publikováno v:
Annales Geophysicae, Vol 18, Pp 1293-1303 (2000)
OH(6–2) Q1/P1 and R1/P1 airglow emission intensity ratios, for rotational states up to j' = 4.5, are measured to be lower than implied by transition probabilities published by various authors including Mies, Langhoff et al. and Turnbull and Lo
Externí odkaz:
https://doaj.org/article/6330682e504349309b48b80608931e79
Publikováno v:
Annales Geophysicae, Vol 16, Pp 77-89 (1998)
The OH(6-2) band was monitored during 1990 at Davis, Antarctica (68.6°S, 78.0°E) using a Czerny-Turner scanning spectrometer. Spectra obtained with a 0.15-nm bandwidth and wavelength steps of 0.005 nm have been recorded in an attempt to isolate
Externí odkaz:
https://doaj.org/article/49aae49b01eb4221834f384bf5d686ef
Publikováno v:
Annales Geophysicae, Vol 13, Pp 1107-1116 (1995)
Two Fourier transform spectrometers have been used to investigate the properties of the near-infrared hydroxyl (OH) nightglow emission under high-latitude summertime conditions and any association with noctilucent clouds (NLCs). The measurements w
Externí odkaz:
https://doaj.org/article/fca2d7e9acdf44fd8c797e872e224243
Publikováno v:
Annales Geophysicae, Vol 13, Iss 10, Pp 1107-1116 (0000)
Two Fourier transform spectrometers have been used to investigate the properties of the near-infrared hydroxyl (OH) nightglow emission under high-latitude summertime conditions and any association with noctilucent clouds (NLCs). The measurements were
Externí odkaz:
https://doaj.org/article/07a6ca30e9a441fabb2726373a41dec3
Publikováno v:
Canadian Journal of Physics. 85:173-187
A new method is introduced that allows meteor radars to potentially produce height-dependent temperatures, rather than simply averages over the meteor region. The method is applied to data from the Clovar radar, near London, Ontario, and then a three
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b124cead2c35d619eb8cdd0d3c4e306
https://doi.org/10.1139/p07-038
https://doi.org/10.1139/p07-038
Publikováno v:
Journal of Geophysical Research. 106:30381-30388
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e3750df9a988104d7701fd6e3ac5147
https://doi.org/10.1029/2001ja001104
https://doi.org/10.1029/2001ja001104
Publikováno v:
Annals of Glaciology. 27:669-673
The polar mesopause region (80-100 km) is the coldest region of the Earth's atmosphere and is expected to be sensitive to global change. Reported increases in observations of polar mesospheric clouds over the last 100 years have been postulated to be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::45a6fda01613efe7a30bfdfec647e794
https://doi.org/10.3189/1998aog27-1-669-673
https://doi.org/10.3189/1998aog27-1-669-673
Autor:
R. P. Lowe, R. J. Sica
Publikováno v:
Journal of Geophysical Research: Atmospheres. 98:1051-1055
The ability to routinely acquire measurements of the ozone density profile in the mesosphere and lower thermosphere is important for use in chemical-dynamical models of the middle atmosphere. Zenith measurements of the O2(1Δg) (0,1) band emission ra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40cf73b4843b999f811030e5c1a51228
https://doi.org/10.1029/92jd02518
https://doi.org/10.1029/92jd02518