A Stochastic Lagrangian Basis for a Probabilistic Parameterization of Moisture Condensation in Eulerian Models
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Open Access
- 25 October 2018
- journal article
- research article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 75 (11) , 3925-3941
Abstract
In this paper, we describe the construction of an efficient probabilistic parameterization that could be used in a coarse-resolution numerical model in which the variation of moisture is not properly resolved. An Eulerian model using a coarse-grained field on a grid cannot properly resolve regions of saturation—in which condensation occurs—that are smaller than the grid boxes. Thus, in the absence of a parameterization scheme, either the grid box must become saturated or condensation will be underestimated. On the other hand, in a stochastic Lagrangian model of moisture transport, trajectories of parcels tagged with humidity variables are tracked, and small-scale moisture variability can be retained; however, explicitly implementing such a scheme in a global model would be computationally prohibitive. One way to introduce subgrid-scale saturation into an Eulerian model is to assume the humidity within a grid box has a probability distribution. To close the problem, this distribution is conventionally determined by relating the required subgrid-scale properties of the flow to the grid-scale properties using a turbulence closure. Here, instead, we determine an assumed probability distribution by using the statistical moments from a stochastic Lagrangian version of the system. The stochastic system is governed by a Fokker–Planck equation, and we use that, rather than explicitly following the moisture parcels, to determine the parameters of the assumed distribution. We are thus able to parameterize subgrid-scale condensation in an Eulerian model in a computationally efficient and theoretically well-founded way. In two idealized advection–condensation problems, we show that a coarse Eulerian model with the subgrid parameterization is well able to mimic its Lagrangian counterpart.Keywords
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Funding Information
- Wolfson Foundation
- Leverhulme Trust
- Natural Environment Research Council
- Engineering and Physical Sciences Research Council
This publication has 35 references indexed in Scilit:
- Minimal models for precipitating turbulent convectionJournal of Fluid Mechanics, 2013
- The advection–condensation model and water‐vapour probability density functionsQuarterly Journal of the Royal Meteorological Society, 2011
- An improved PDF cloud scheme for climate simulationsQuarterly Journal of the Royal Meteorological Society, 2010
- PC2: A prognostic cloud fraction and condensation scheme. I: Scheme descriptionQuarterly Journal of the Royal Meteorological Society, 2008
- Diagnosis of Subtropical Humidity Dynamics Using Tracers of Last SaturationJournal of the Atmospheric Sciences, 2005
- PARAMETERIZATION OF PHYSICAL PROCESSES | Clouds2003
- Toward a Unified Parameterization of the Boundary Layer and Moist Convection. Part I: A New Type of Mass-Flux ModelJournal of the Atmospheric Sciences, 2001
- Evidence for control of Atlantic subtropical humidity by large scale advectionGeophysical Research Letters, 1998
- A parameterization of mixdown time for atmospheric chemicalsJournal of Geophysical Research: Atmospheres, 1997
- Modeling the Trade-Wind Cumulus Boundary Layer. Part I: Testing the Ensemble Cloud Relations Against Numerical DataJournal of the Atmospheric Sciences, 1981