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Chapter 5.5 Deep convection

2001
Publisher Summary This chapter reviews deep convection with emphasis on advances made during the World Ocean Circulation Experiment (WOCE) observing period. It describes some features of plumes, the convective mixing agents. The chapter also discusses two phenomena's associated with the convection.
John Lazier   +2 more
openaire   +1 more source

On the Thermodynamic Equation for Deep Convection

Monthly Weather Review, 1977
Abstract A review is given of six equations that are used to approximate reversible saturated parcel ascent. These approximations are compared with the aid of several examples and their appropriateness for use in modeling deep clouds discussed.
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Rotating deep annulus convection

Tellus, 1969
Sixteen meridian-plane temperature profiles were obtained in the upper symmetric regime of a differentially heated rotating annulus of water by means of a thermocouple probe. This probe, though made as small as practicable, disturbed the flow field, and the nature of the disturbance and its correction is discussed.
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The Mesoscale Organization of Deep Convection

1997
The organization of systems at all scales has long been an observed feature in meteorology. Coherent structures can be found from eddies in the planetary boundary layer up to tropical cyclones and mid-latitude depressions. The problem of organization is thus of a fundamental nature. An understanding of the organization of deep convection is relevant to
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Changing Spatial Patterns of Deep Convection in the Subpolar North Atlantic

Journal of Geophysical Research: Oceans, 2021
S Rühs, Eric C J Oliver, Arne Biastoch
exaly  

On the Anelastic Approximation for Deep Convection

Journal of the Atmospheric Sciences, 1990
Abstract A brief review of the scale analysis of Lipps and Hemler is given without any reference to the parameters G and B. The resulting anelastic equations conserve energy, in contrast to the modified anelastic set of equations analyzed by Durran. In addition, the present equations give an accurate solution for the frequency of gravity waves in an ...
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Status of deep convection nowcasting

1996
The techniques commonly uses in Europe for the nowcasting of deep convection are presented and analysed in this chapter, after a survey among 38 European institutions.
V. Ducroq   +3 more
openaire   +1 more source

Lagrangian Floats for Deep Convection

1997
Abstract : I aim to understand the process of deep convection in the ocean. Near surface water is mixed to great depth at a few high latitude locations, thereby forming the deep and bottom masses of the ocean. This proposal has supported the development and deployment of neutrally buoyant floats in the Labrador Sea in the winters of 1997 and 1998 and ...
openaire   +1 more source

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