The response of a nonlinear, time-dependent, baroclinic model of the atmosphere to tropical thermal forcing

التفاصيل البيبلوغرافية
العنوان: The response of a nonlinear, time-dependent, baroclinic model of the atmosphere to tropical thermal forcing
المؤلفون: William L. Grose, R. E. Turner, W. T. Blackshear
المصدر: Quarterly Journal of the Royal Meteorological Society. 110:981-1002
بيانات النشر: Wiley, 1984.
سنة النشر: 1984
مصطلحات موضوعية: Atmospheric Science, Atmospheric models, Atmospheric wave, Baroclinity, Barotropic fluid, Primitive equations, Extratropical cyclone, Atmospheric model, Forcing (mathematics), Mechanics, Atmospheric sciences, Physics::Atmospheric and Oceanic Physics, Geology
الوصف: A multi-level, sigma coordinate, primitive equation atmospheric model has been utilized to study both the tropical and extratropical response to an isolated region of steady thermal forcing in the tropics. The nonlinear response during the first 28 days of the simulation is described. The response can be generally characterized by two distinct components. The first component is a quasi-stationary disturbance which extends eastward and poleward away from the source region along a 'great circle' path. The structure of this disturbance is essentially barotropic away from the source region. The second component is a growing baroclinic wave propagating zonally at mid-latitudes. Significantly, this disturbance is apparently the result of baroclinic instability induced by the quasi-stationary wavetrain. The discussion is predominantly heuristic in form and relies heavily on graphical presentation and quasi-geostrophic theory to interpret the response and individual components of the thermodynamic energy and momentum equations.
تدمد: 1477-870X
0035-9009
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_________::e9a7585a2be7ea6c88061d071cd42edb
https://doi.org/10.1002/qj.49711046611
حقوق: CLOSED
رقم الأكسشن: edsair.doi...........e9a7585a2be7ea6c88061d071cd42edb
قاعدة البيانات: OpenAIRE