TY - CONF

T1 - Proposals on methods for the simultaneous retrievals of [O3] and [CO2] altitude profiles in the mesosphere

AU - Мануйлова, Рада Олеговна

AU - Янковский, Валентин Андреевич

N1 - Conference code: 18

PY - 2018/4/7

Y1 - 2018/4/7

N2 - The small components O3 and CO2 are responsible for the thermal regime of the daytime mesosphere and lower thermosphere (MLT) of the Earth. The CO2 concentration in the MLT region is usually retrieved indirectlyby solving the complicated problem of radiative transfer at conditions of the breaking of local thermodynamic equilibrium (LTE). The analogous difficulties of [O3] retrieval from the observation of emission in 9.6 µm band are explained by complexity of vibrational kinetics of the O3 molecule. The problem of independent and simultaneous retrieval of [O3] and [CO2] can be solved by using individual proxy for each of the target component. In this study we present the method of simultaneously retrieval of [O3] and [CO2] worked out on the base of the model of electronic-vibrational kinetics of the products of O2 and O3 photodissociation in the MLT, YM2011. We use the altitude dependence of the concentration of the excited component O2(b1, v = 0) (where v is vibrational quantum number) as a proxy to retrieve [CO2] and of the O2(b1,v = 1) concentration as a proxy for retrieval of [O3] altitude profile. The concentration indicator for the O2(b1,v = 0) is emission from this level in the O2 bands Atm (0, 0) at 762 nm, O2 Atm (0, 1) at 865 nm and for the O2(b1, v = 1) is emission from this level in the O2 bands Atm (1, 1) at 771 nm, O2 Atm (1, 0) at 688 nm or Atm (1, 2) at 874 nm [1]. The method of retrieving the altitude dependence of the volume mixing ratio of theCO2, Cv,CO2, in the mesosphere (nearly 50 – 85 km) is based on measurement of the ratio of concentrations of two excited components: [O2(b1, v = 1)]/[O2(b1, v = 0)]. In this study we have showed, that to determine Cv,CO2, it is necessary to measure the absolute value of volume emission rate (VER) of the radiation produced by transitions from the level O2(b1, v=0), as well as VER of the radiation generated by the transitions from the level O2(b1, v=1). For the O3 volume mixing ratio, Cv,O3, we have showed, that the error of the Cv,O3 retrieval mainly depends not on all reactions included in the model YM2011, but on the following parameters: on the accuracy of the measurements of VER of the radiation generated by the transitions from the level O2(b1, v=1) and also onerrors in the rate coefficients of reactions O2(b1, v=1) + O2 → O2(X3, v=1) + O2(b1, v=0) and O2(b1, v=0) + O3 → products. The funding of the study was provided by RFBR, grant N 17-05-00532-a.

AB - The small components O3 and CO2 are responsible for the thermal regime of the daytime mesosphere and lower thermosphere (MLT) of the Earth. The CO2 concentration in the MLT region is usually retrieved indirectlyby solving the complicated problem of radiative transfer at conditions of the breaking of local thermodynamic equilibrium (LTE). The analogous difficulties of [O3] retrieval from the observation of emission in 9.6 µm band are explained by complexity of vibrational kinetics of the O3 molecule. The problem of independent and simultaneous retrieval of [O3] and [CO2] can be solved by using individual proxy for each of the target component. In this study we present the method of simultaneously retrieval of [O3] and [CO2] worked out on the base of the model of electronic-vibrational kinetics of the products of O2 and O3 photodissociation in the MLT, YM2011. We use the altitude dependence of the concentration of the excited component O2(b1, v = 0) (where v is vibrational quantum number) as a proxy to retrieve [CO2] and of the O2(b1,v = 1) concentration as a proxy for retrieval of [O3] altitude profile. The concentration indicator for the O2(b1,v = 0) is emission from this level in the O2 bands Atm (0, 0) at 762 nm, O2 Atm (0, 1) at 865 nm and for the O2(b1, v = 1) is emission from this level in the O2 bands Atm (1, 1) at 771 nm, O2 Atm (1, 0) at 688 nm or Atm (1, 2) at 874 nm [1]. The method of retrieving the altitude dependence of the volume mixing ratio of theCO2, Cv,CO2, in the mesosphere (nearly 50 – 85 km) is based on measurement of the ratio of concentrations of two excited components: [O2(b1, v = 1)]/[O2(b1, v = 0)]. In this study we have showed, that to determine Cv,CO2, it is necessary to measure the absolute value of volume emission rate (VER) of the radiation produced by transitions from the level O2(b1, v=0), as well as VER of the radiation generated by the transitions from the level O2(b1, v=1). For the O3 volume mixing ratio, Cv,O3, we have showed, that the error of the Cv,O3 retrieval mainly depends not on all reactions included in the model YM2011, but on the following parameters: on the accuracy of the measurements of VER of the radiation generated by the transitions from the level O2(b1, v=1) and also onerrors in the rate coefficients of reactions O2(b1, v=1) + O2 → O2(X3, v=1) + O2(b1, v=0) and O2(b1, v=0) + O3 → products. The funding of the study was provided by RFBR, grant N 17-05-00532-a.

M3 - Abstract

T2 - European Geosciences Union General Assembly 2018

Y2 - 7 April 2018 through 12 April 2018

ER -