Naslov
Environmental influences on the spinup of tropical cyclones

Autori
Raymond, David J. ; Cisneros, Jorge ; Sessions, Sharon L. ; Marin, J. C. ; Raga, Graciela ; Fuchs, Željka

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Skup
28th Conference on Hurricanes and Tropical Meteorology

Mjesto i datum
Orlando (FL), Sjedinjene Američke Države, 28.04.2008. - 02.05.2008

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
cyclone; spinup; humidity

Sažetak
We outline here a theory for the spinup of tropical cyclones, based on a particular form of the circulation theorem. The development or non-development of a cyclone results from the interplay between the convergence of vorticity, which tends to spin up the cyclone, and surface friction, which tends to spin it down. The theory provides a quantitative estimate all of the qualitative environmental factors which are commonly thought to control cyclone spinup. The vorticity convergence depends on the mass convergence and the vorticity of the surrounding environment. The mass convergence is in turn driven primarily by deep convection within the cyclone. Rainfall from convection in the tropics tends to be closely related to low-level convergence and plays an important role in spinup. Recent work by Bretherton and others shows that the production of rainfall by convection is a steeply increasing function of the column relative humidity or saturation fraction of the surrounding air, i. e., the precipitable water divided by the saturated precipitable water. Factors affecting the humidity in the cyclone core, such as wind shear, which can transport dry environmental air into the core, thus become key to cyclone development. Our theory provides a quantitative measure of this ventilation. Another factor relevant to cyclone core thermodynamics is the surface moist entropy flux, which is a strong function of sea surface temperature, wind and ocean heat content. The classical picture of surface friction in tropical cyclones has the surface stress distributed through the boundary layer. However, the transport of momentum through the top of the boundary layer due either to entrainment processes or to deep convection is bound to have an important effect on frictional spindown as well. This is an area needing extensive investigation, as its strength and even sign have not been measured in the context of tropical cyclones. This paper will serve as an introduction to two other papers: (1) evaluation of the theory from IFEX dropsonde observations (Cisneros) ; and (2) the workings of the theory in the NCEP GFS model, which has shown some success in predicting tropical cyclogenesis (Marin).

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA