Self-organisation of convection as a mechanism for memory

Convection is a well-observed atmospheric phenomenon, which has a fundamental role in global weather and climate. The transport of heat, moisture and momentum that result from convection are significant at a range of temporal and spatial scales. Convective clouds have a wide range of non-linear inte...

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Bibliographic Details
Main Author: Davies, Laura
Published: University of Reading 2008
Subjects:
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.501345
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Summary:Convection is a well-observed atmospheric phenomenon, which has a fundamental role in global weather and climate. The transport of heat, moisture and momentum that result from convection are significant at a range of temporal and spatial scales. Convective clouds have a wide range of non-linear interactions with other atmospheric processes which make them difficult to understand and model numerically. Due to resolution constraints in climate models, sub-grid convection is represented by a parameterisation. Many parameterisation schemes are based on an assumed temporal and spatial separation between convection and its forcing. The implied equilibrium relates current convection directly to the large-scale forcing. The validity of the temporal scale separation is directly tested in this thesis by examining the convective response to a time-varying forcing.