Linear baroclinic instability in the presence of heat inflow from the lower boundary

Details Linear baroclinic instability in the presence of heat inflow from the lower boundary Linear baroclinic instability in the presence of heat inflow from the lower boundary

Apr 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995angeo..13..419f&link_type=abstract

Annales Geophysicae, vol. 13, Issue 4, pp.419-426

Physics

2

Scientific paper

A linear Eady model with a parameterization of heat influx from the lower boundary is studied analytically in order to obtain the characteristics of baroclinic normal modes modified by this non-adiabatic source. The results display a secondary maximum of growth rate at high wave numbers and a range of absolutely unstable waves, thus suggesting that the property observed among mid-latitude explosive cyclones of being near-stationary in the phase of maximum growth may be captured by this representation of the air-sea energy exchange.

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