Remote sensing of neutral temperatures in the Earth's thermosphere using the Lyman-Birge-Hopfield bands of N2: Comparisons with satellite drag data

被引：10

作者：

Krywonos, Andrey ^{[1
]}

Murray, D. J. ^{[2
]}

Eastes, R. W. ^{[1
,2
]}

Aksnes, A. ^{[1
]}

Budzien, S. A. ^{[3
]}

Daniell, R. E.

机构：

[1] Univ Cent Florida, Florida Space Inst, Orlando, FL 32826 USA

[2] Univ Cent Florida, Dept Phys, Orlando, FL 32826 USA

[3] USN, Res Lab, Washington, DC 20375 USA

来源：

JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS | 2012年 / 117卷

基金：

美国国家科学基金会;

关键词：

DAYGLOW;

D O I：

10.1029/2011JA017226

中图分类号：

P1 [天文学];

学科分类号：

0704 ;

摘要：

This paper presents remotely sensed neutral temperatures obtained from ultraviolet observations and compares them with temperatures from the NRLMSISE-00 version of the Mass Spectrometer and Incoherent Scatter (MSIS) model (unconstrained and constrained to match the total densities from satellite drag). Latitudinal profiles of the temperatures in the Earth's thermosphere are obtained by inversion of high-resolution (similar to 1.3 angstrom) observations of the (1,1) and (5,4) Lyman-Birge-Hopfield (LBH) bands of N-2. The spectra are from the High resolution Ionospheric and Thermospheric Spectrograph (HITS) instrument aboard the Advanced Research and Global Observation Satellite (ARGOS). The results indicate that on each day examined there was consistency between the remotely sensed thermospheric temperatures, the densities from coincident satellite drag measurements at adjacent altitudes, and the NRLMSISE-00 model.

引用

页数：9

共 12 条

[1] Remote sensing of lower-middle-thermosphere temperatures using the N2 Lyman-Birge-Hopfield (LBH) bands
Eastes, Richard
Evans, J. Scott
Gan, Quan
Mcclintock, William
Lumpe, Jerry
ATMOSPHERIC MEASUREMENT TECHNIQUES, 2025, 18 (04) : 921 - 928
[2] Neutral temperatures in the lower thermosphere from N2 Lyman-Birge-Hopfield (LBH) band profiles
Aksnes, A.
Eastes, R.
Budzien, S.
Dymond, K.
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (15)
[3] Emissions from the N2 Lyman-Birge-Hopfield bands in the Earth's atmosphere
Eastes, RW
PHYSICS AND CHEMISTRY OF THE EARTH PART C-SOLAR-TERRESTIAL AND PLANETARY SCIENCE, 2000, 25 (5-6): : 523 - 527
[4] Luminescence of Lyman-Birge-Hopfield Bands of N2 in the Earth's Atmosphere during the Precipitation of High-Energy Electrons
Kirillov, A. S.
Belakhovsky, V. B.
GEOMAGNETISM AND AERONOMY, 2020, 60 (06) : 781 - 786
[5] SELF-ABSORPTION OF THE N2 LYMAN-BIRGE-HOPFIELD BANDS IN THE FAR ULTRAVIOLET DAYGLOW
CONWAY, RR
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1982, 87 (NA2): : 859 - 866
[6] EXCITATION OF N-2 LYMAN-BIRGE-HOPFIELD BANDS EMISSION BY LOW EARTH ORBITING SPACECRAFT
KOFSKY, IL
GEOPHYSICAL RESEARCH LETTERS, 1988, 15 (03) : 241 - 244
[7] FLUORESCENT SCATTERING IN PLANETARY ATMOSPHERES .4. FORMATION OF LYMAN-BIRGE-HOPFIELD BANDS OF N2 IN TERRESTRIAL ATMOSPHERE
SOBOUTI, Y
ASTROPHYSICAL JOURNAL, 1963, 138 (03): : 748 - &
[8] Modeling the N2 Lyman-Birge-Hopfield bands in the dayglow:: Including radiative and collisional cascading between the singlet states
Eastes, RW
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2000, 105 (A8) : 18557 - 18573
[9] FLUORESCENT SCATTERING IN PLANETARY ATMOSPHERES .3. FORMATION OF LYMAN-BIRGE-HOPFIELD BANDS OF N2 IN MARTIAN ATMOSPHERE
SOBOUTI, Y
ASTROPHYSICAL JOURNAL, 1963, 138 (03): : 720 - &
[10] Luminescence of Lyman–Birge–Hopfield Bands of N2 in the Earth’s Atmosphere during the Precipitation of High-Energy Electrons
A. S. Kirillov
V. B. Belakhovsky
Geomagnetism and Aeronomy, 2020, 60 : 781 - 786

← 1 2 →