Baroclinic outbreak episodes in wavenumber domain

Abstract

In contrast to the common definition of anomalous atmospheric flow by persistent and localized geopotential height anomalies, we define significant excursions from normal conditions by persistent anomalies of a single spectral energy conversion on a circumpolar scale. Whereas amplification of transient geopotential height or streamfunction anomalies generally involves a variety of possible processes and complex energetics, our approach defines strongly distorted energetics of a certain kind. With data covering 10 years (1967)(1968)(1969)(1970)(1971)(1972)(1973)(1974)(1975)(1976), we study baroclinic energy conversions from zonal mean to zonal wavenumber m available potential energy, C(A,A,), when these exceed the long-term average by more than a standard deviation for at least 3 consecutive days. During these episodes, called baroclinic outbreaks (BO), C(A,K,,,) and the kinetic energy of wave m, K,,,, are also large in all probability. Although short BO cases are frequent for all m, there is a secondary maximum of frequency at about 7 days for the ultralong wave m = 2. Composite energetics of BO's are presented, and a profound transformation of the 500 mb flow is shown for a long lasting m = 2 BO event.

Zonal wave number 2 baroclinic outbreak episodes in winter

“…We can only hope to draw definite conclusions for an ensemble of events which is more or less homogeneous by definition. In the companion study (Schilling, 1988, hereafter referred to as S88), an improvement is achieved by defining episodes by extraordinarily strong developments of a single energy conversion. This conversion should represent a definite process.…”