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• W1782562765 abstract "Abstract Monthly averaged zonal mean temperature and ozone volume mixing ratios obtained from “Sounding of the Atmosphere using Broadband Emission Radiometry” instrument on board “Thermosphere Ionosphere Mesosphere Energetics and Dynamics” satellite for the years 2002–2012 are used to study the seasonal and solar cycle variabilities of tropical (10°N–15°N) mesopause structure. The mesopause temperature and ozone mixing ratios are positively correlated with solar cycle due to changes in CO 2 and O, respectively. Although the seasonal variation in mesopause temperatures is quite small, the mesopause altitudes are comparatively higher (~99–100 km) in April and lower (~95 km) in September. The factors controlling the tropical mesopause structure are investigated by taking the mesopause variability for the year 2011 as a case study as it resembles the long‐term mean seasonal variation. It is found that the radiative cooling due to 15 µm CO 2 infrared emissions is the only cooling mechanism in the mesopause region. The net heating rates obtained from (i) solar heating by O 2 and O 3 , (ii) chemical heating due to seven major exothermic reactions, (iii) O 3 long‐wave radiative heating, and (iv) CO 2 cooling are smaller (~20 K/d) in April and larger (~85 K/d) in September at lower thermosphere (~99–101 km). The downward heat conduction from the lower thermosphere forces the mesopause to lower heights in September, although no downward heat conduction is observed in April." @default.
• W1782562765 created "2016-06-24" @default.
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• W1782562765 date "2015-05-01" @default.
• W1782562765 modified "2023-09-25" @default.
• W1782562765 title "Influence of solar cycle and chemistry on tropical (10°N-15°N) mesopause variabilities" @default.
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• W1782562765 doi "https://doi.org/10.1002/2014ja020930" @default.
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