Mostrar el registro sencillo del ítem Hysell, D. L. Aveiro, H. C. Chau Chong Shing, Jorge Luis 2018-06-28T15:58:56Z 2018-06-28T15:58:56Z 2014-03-14
dc.identifier.govdoc index-oti2018
dc.description En: Modeling the Ionosphere–Thermosphere System / Book editors, Joseph Huba Robert Schunk George Khazanov, 14 March 2014. es_ES
dc.description.abstract There are several thermosphere ionosphere models with bottom boundaries somewhere in the middle atmosphere. Achieving a true whole atmosphere modeling capability requires the specification of atmospheric conditions at a boundary. This chapter discusses the use of the Navy Operational Global Atmospheric Prediction System‐Advanced Level Physics High Altitude (NOGAPS‐ALPHA) model as a bottom boundary for the thermosphere ionosphere electrodynamics general circulation model (TIEGCM). The results are compared with Sounding of the Atmosphere with Broadband Emission Radiometry (SABER) observations and previously published model results. The chapter presents an evaluation of the behavior of tidal components at the interface between the two models, and suggests a method to reduce the discontinuities. Consistent with previous models, a marked decrease is found in the semidiurnal tide after the dramatic sudden stratospheric warming in late January 2009. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher American Geophysical Union es_ES
dc.relation.ispartofseries urn:isbn:9781118704417
dc.rights info:eu-repo/semantics/restrictedAccess es_ES
dc.subject Ionosphere es_ES
dc.subject Thermosphere es_ES
dc.subject Atmospheric tides es_ES
dc.subject Atmospheric circulation es_ES
dc.subject Atmospheric thermodynamics es_ES
dc.title Ionospheric Irregularities: Frontiers es_ES
dc.type info:eu-repo/semantics/bookPart es_ES
dc.subject.ocde es_ES
dc.identifier.doi es_ES




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