Temperature Sounding Experiments for the Jovian PlanetsSource: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 005::page 950Author:Taylor, F. W.
DOI: 10.1175/1520-0469(1972)029<0950:TSEFTJ>2.0.CO;2Publisher: American Meteorological Society
Abstract: The possibilities for vertical temperature sounding experiments by medium-resolution measurements of outgoing radiance are examined for non-scattering models of Jupiter, Saturn, Uranus and Neptune. It is shown that for Jupiter the widest vertical coverage of the atmosphere results from five or six channels placed in the ?4 band of methane at 7.5 ?, but energy constraints render this experiment marginal at Saturn and useless at Uranus and Neptune. For the outermost planets, the best experiment is three or four channels located in the long-wavelength half of the pressure-induced S(O) line of hydrogen, in the range 25?40 ? with which a limited vertical range of about two scale heights can be covered. Some results of inversion of synthetic data are presented in each case, and the likely effect of clouds on the measurements is discussed.
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contributor author | Taylor, F. W. | |
date accessioned | 2017-06-09T14:16:29Z | |
date available | 2017-06-09T14:16:29Z | |
date copyright | 1972/07/01 | |
date issued | 1972 | |
identifier issn | 0022-4928 | |
identifier other | ams-16207.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151965 | |
description abstract | The possibilities for vertical temperature sounding experiments by medium-resolution measurements of outgoing radiance are examined for non-scattering models of Jupiter, Saturn, Uranus and Neptune. It is shown that for Jupiter the widest vertical coverage of the atmosphere results from five or six channels placed in the ?4 band of methane at 7.5 ?, but energy constraints render this experiment marginal at Saturn and useless at Uranus and Neptune. For the outermost planets, the best experiment is three or four channels located in the long-wavelength half of the pressure-induced S(O) line of hydrogen, in the range 25?40 ? with which a limited vertical range of about two scale heights can be covered. Some results of inversion of synthetic data are presented in each case, and the likely effect of clouds on the measurements is discussed. | |
publisher | American Meteorological Society | |
title | Temperature Sounding Experiments for the Jovian Planets | |
type | Journal Paper | |
journal volume | 29 | |
journal issue | 5 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1972)029<0950:TSEFTJ>2.0.CO;2 | |
journal fristpage | 950 | |
journal lastpage | 958 | |
tree | Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 005 | |
contenttype | Fulltext |