Standard

IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method. / Yankovsky, V. A. ; Martyshenko, K.V.

в: Geomagnetism and Aeronomy, Том 57, № 2, 2017, стр. 229-241.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Yankovsky, VA & Martyshenko, KV 2017, 'IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method', Geomagnetism and Aeronomy, Том. 57, № 2, стр. 229-241. https://doi.org/10.1134/S0016793217020098

APA

Yankovsky, V. A., & Martyshenko, K. V. (2017). IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method. Geomagnetism and Aeronomy, 57(2), 229-241. https://doi.org/10.1134/S0016793217020098

Vancouver

Yankovsky VA, Martyshenko KV. IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method. Geomagnetism and Aeronomy. 2017;57(2):229-241. https://doi.org/10.1134/S0016793217020098

Author

Yankovsky, V. A. ; Martyshenko, K.V. / IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method. в: Geomagnetism and Aeronomy. 2017 ; Том 57, № 2. стр. 229-241.

BibTeX

@article{e72237a69885427297fb6e76791a28b5,
title = "IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method",
abstract = "The problem of systematic overestimation (20-50%) of the retrieved ozone concentrations in the altitude range of 60-80 km in the TIMED-SABER satellite experiment in the daytime has been solved. The reason for overestimation is the neglect of the electronic vibrational kinetics of photolysis products of ozone and molecular oxygen O2(b1Σg +, ν) and O2(a1Δg, ν). The IR emission band of O2(a1Δg, ν = 0) at 1.27 μm can be correctly used in remote sensing in order to obtain the ozone altitude profile in the altitude range of 50-88 km only with the use of a complete model of electronic vibrational kinetics of O2 and O3 photolysis products (YM2011) in the Earth's mesosphere and lower thermosphere. Alternative ozone tracers have been considered, and an optimum tracer in the altitude range of 50-100 km such as O2(b1Σg +, ν = 1) molecule emissions has been proposed.",
keywords = "ozone vertical profile, daylow oxygen emission, mesosphere, kinetics, electronical-vibrational excitation",
author = "Yankovsky, {V. A.} and K.V. Martyshenko",
note = "Martyshenko, K.V., Yankovsky, V.A. IR band of O2 at 1.27 μm as the tracer of O3 in the mesosphere and lower thermosphere: Correction of the method. Geomagn. Aeron. 57, 229–241 (2017). https://doi.org/10.1134/S0016793217020098",
year = "2017",
doi = "10.1134/S0016793217020098",
language = "English",
volume = "57",
pages = "229--241",
journal = "Geomagnetism and Aeronomy",
issn = "0016-7932",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - IR Band of O2 at 1.27 μm as the Tracer of O3 in the Mesosphere and Lower Thermosphere: Correction of the Method

AU - Yankovsky, V. A.

AU - Martyshenko, K.V.

N1 - Martyshenko, K.V., Yankovsky, V.A. IR band of O2 at 1.27 μm as the tracer of O3 in the mesosphere and lower thermosphere: Correction of the method. Geomagn. Aeron. 57, 229–241 (2017). https://doi.org/10.1134/S0016793217020098

PY - 2017

Y1 - 2017

N2 - The problem of systematic overestimation (20-50%) of the retrieved ozone concentrations in the altitude range of 60-80 km in the TIMED-SABER satellite experiment in the daytime has been solved. The reason for overestimation is the neglect of the electronic vibrational kinetics of photolysis products of ozone and molecular oxygen O2(b1Σg +, ν) and O2(a1Δg, ν). The IR emission band of O2(a1Δg, ν = 0) at 1.27 μm can be correctly used in remote sensing in order to obtain the ozone altitude profile in the altitude range of 50-88 km only with the use of a complete model of electronic vibrational kinetics of O2 and O3 photolysis products (YM2011) in the Earth's mesosphere and lower thermosphere. Alternative ozone tracers have been considered, and an optimum tracer in the altitude range of 50-100 km such as O2(b1Σg +, ν = 1) molecule emissions has been proposed.

AB - The problem of systematic overestimation (20-50%) of the retrieved ozone concentrations in the altitude range of 60-80 km in the TIMED-SABER satellite experiment in the daytime has been solved. The reason for overestimation is the neglect of the electronic vibrational kinetics of photolysis products of ozone and molecular oxygen O2(b1Σg +, ν) and O2(a1Δg, ν). The IR emission band of O2(a1Δg, ν = 0) at 1.27 μm can be correctly used in remote sensing in order to obtain the ozone altitude profile in the altitude range of 50-88 km only with the use of a complete model of electronic vibrational kinetics of O2 and O3 photolysis products (YM2011) in the Earth's mesosphere and lower thermosphere. Alternative ozone tracers have been considered, and an optimum tracer in the altitude range of 50-100 km such as O2(b1Σg +, ν = 1) molecule emissions has been proposed.

KW - ozone vertical profile

KW - daylow oxygen emission

KW - mesosphere

KW - kinetics

KW - electronical-vibrational excitation

UR - https://www.elibrary.ru/item.asp?id=41773636

U2 - 10.1134/S0016793217020098

DO - 10.1134/S0016793217020098

M3 - Article

VL - 57

SP - 229

EP - 241

JO - Geomagnetism and Aeronomy

JF - Geomagnetism and Aeronomy

SN - 0016-7932

IS - 2

ER -

ID: 37549461