By Daniel R. Marsh (auth.), Mangalathayil Ali Abdu, Dora Pancheva (eds.)
This e-book is a multi-author treatise at the most eminent study difficulties within the box of the aeronomy of the Earth’s surroundings and ionosphere, encompassing the technology lined through the department II of the foreign organization of Geomagnetism and Aeronomy (IAGA). It comprises numerous evaluate articles and unique papers through top scientists within the box. The booklet is prepared in five elements: 1) Mesosphere-Lower Thermosphere Dynamics and Chemistry; 2) Vertical Coupling through Upward Propagating Waves; three) Ionospheric Electrodynamics and Structuring; four) Thermosphere- Ionosphere Coupling, Dynamics and developments and five) Ionosphere-Thermosphere Disturbances and Modeling. The publication consolidates the development acheived within the box in recent times and it serves as an invaluable reference for graduate scholars in addition to skilled researchers.
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Additional info for Aeronomy of the Earth's Atmosphere and Ionosphere
R. Marsh Clerbaux C, Coheur P-F, Hurtmans D, Barret B, Carleer M, Colin R, Semeniuk K, McConnell JC, Boone C, Bernath P (2005) Carbon monoxide distribution from the ACEFTS solar occultation measurements. Geophys Res Lett 32:L16S01. 1029/2005GL022394 Dunkerton T, Hsu C-PF, McIntyre ME (1981) Some Eulerian and Lagrangian diagnostics for a model stratospheric warming. J Atmos Sci 38:819–843 Fomichev VI, Fu C, de Grandpré J, Beagley SR, Ogibalov VP, McConnell JC (2004) Model thermal response to minor radiative energy sources and sinks in the middle atmosphere.
In: Siskind DE, Eckermann SD, Summers ME (eds) Atmospheric science across the stratopause. Geophysical monograph series, vol 123. AGU, Washington, DC, pp 83–100 Lossow S, Urban J, Schmidt H, Marsh DR, Gumbel J, Eriksson P, Murtagh D (2009) Wintertime water vapor in the polar upper mesosphere and lower thermosphere: first satellite observations by Odin submillimeter radiometer. J Geophys Res 114:D10304. 1029/2008JD011462 Manney GL et al (2008) The evolution of the stratopause during the 2006 major warming: satellite data and assimilated meteorological analyses.
7b). The reversal of the zonal winds occurs because of a dramatic change in the acceleration due to the dissipation of breaking gravity waves (shown in Fig. 7a) which changes from more than 50 m/s/day westward in December to more than 75 m/s/day eastward in January. The westward stratospheric winds that occur during the SSW allow waves with eastward phase speed to propagate into the mesosphere where they dissipate and cause an eastward acceleration. 01 hPa is again westward, driving a polward and downward residual circulation and a warming of the mesosphere through adiabatic heating.
Aeronomy of the Earth's Atmosphere and Ionosphere by Daniel R. Marsh (auth.), Mangalathayil Ali Abdu, Dora Pancheva (eds.)