The local balances of vorticity and heat for blocking anticyclones in a spectral general circulation model

• Published in: Journal of the atmospheric sciences 1986-07, Vol.43 (13), p.1406-1441
• Main Author: MULLEN, S. L
• Format: Article
• Language: English
• Subjects: Convection, turbulence, diffusion. Boundary layer structure and dynamics; Earth, ocean, space; Exact sciences and technology; External geophysics; Meteorology
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/1520-0469(1986)043<1406:tlbova>2.0.co;2

Blocking anticyclones that appear in perpetual Jan. simulations of a spectral general circulation model are examined. Blocks in three geographical regions are studied: the North Pacific, the North Atlantic, and western North America. Local time-averaged balances of vorticity and heat are evaluated for composite cases of blocking. The following common relationships emerged from these budgets. The time-mean divergence term is, in general, a first-order term in the vorticity balance throughout the troposphere, and its pattern over severe orography is closely related to the underlying topography. Above the surface layer, the horizontal advection of time-mean absolute vorticity by the mean wind mainly balances the divergence term, with the net effect of the time-mean vorticity forcing being a tendency for the blocking pattern to propagate downstream. The transient eddy vorticity transports act to shift the block upstream and, therefore, they mainly offset the downstream tendency resulting from the time-mean flow; the magnitude of the eddy vorticity term is typically one-third to one-half that of the divergence or advection terms alone. Frictional dissipation is negligible everywhere except near the ground where it primarily offsets the divergence term. The horizontal advection of the time-mean temperature field by the mean wind throughout the troposphere is a first-order term in the heat balance and is mainly responsible for maintaining the block's thermal perturbations; it is predominately balanced by adiabatic heating in the free troposphere and by diabatic heating near the surface. Transient eddy heat transports act to dissipate the block's thermal perturbations at all levels, while diabatic heating does not exhibit a systematic relationship with the temperature field at any level. A quasi-geostrophic diagnosis of the ageostrophic motion field suggests that dynamical processes that strongly affect the vorticity balance may be more important to the maintenance of model blocks than processes that strongly affect the heat balance. The mountains appear capable of influencing the shape of the model blocks, but preliminary results indicate that orographic forcing may not be absolutely essential for the blocking process to occur in the model.