### Abstract

An idealized framework to study the impacts of phase transitions on atmospheric dynamics is described. Condensation of water vapor releases a significant amount of latent heat, which directly affects the atmospheric temperature and density. Here, phase transitions are treated by assuming that air parcels are in local thermodynamic equilibrium, which implies that condensed water can only be present when the air parcel is saturated. This reduces the number of variables necessary to describe the thermodynamic state of moist air to three. It also introduces a discontinuity in the partial derivatives of the equation of state. A simplified version of the equation of state is obtained by a separate linearization for saturated and unsaturated parcels. When this equation of state is implemented in a Boussinesq system, the buoyancy can be expressed as a piecewise linear function of two prognostic thermodynamic variables, D and M, and height z. Numerical experiments on the nonlinear evolution of the convection and the impact of latent heat release on the buoyant flux are presented.

Original language | English (US) |
---|---|

Pages (from-to) | 295-319 |

Number of pages | 25 |

Journal | Communications in Mathematical Sciences |

Volume | 8 |

Issue number | 1 |

State | Published - 2010 |

### Fingerprint

### Keywords

- Atmospheric dynamics
- Clouds
- Convection

### ASJC Scopus subject areas

- Mathematics(all)
- Applied Mathematics

### Cite this

*Communications in Mathematical Sciences*,

*8*(1), 295-319.

**Idealized moist Rayleigh-Bénard convection with piecewise linear equation of state.** / Pauluis, Olivier; Schumacher, Jörg.

Research output: Contribution to journal › Article

*Communications in Mathematical Sciences*, vol. 8, no. 1, pp. 295-319.

}

TY - JOUR

T1 - Idealized moist Rayleigh-Bénard convection with piecewise linear equation of state

AU - Pauluis, Olivier

AU - Schumacher, Jörg

PY - 2010

Y1 - 2010

N2 - An idealized framework to study the impacts of phase transitions on atmospheric dynamics is described. Condensation of water vapor releases a significant amount of latent heat, which directly affects the atmospheric temperature and density. Here, phase transitions are treated by assuming that air parcels are in local thermodynamic equilibrium, which implies that condensed water can only be present when the air parcel is saturated. This reduces the number of variables necessary to describe the thermodynamic state of moist air to three. It also introduces a discontinuity in the partial derivatives of the equation of state. A simplified version of the equation of state is obtained by a separate linearization for saturated and unsaturated parcels. When this equation of state is implemented in a Boussinesq system, the buoyancy can be expressed as a piecewise linear function of two prognostic thermodynamic variables, D and M, and height z. Numerical experiments on the nonlinear evolution of the convection and the impact of latent heat release on the buoyant flux are presented.

AB - An idealized framework to study the impacts of phase transitions on atmospheric dynamics is described. Condensation of water vapor releases a significant amount of latent heat, which directly affects the atmospheric temperature and density. Here, phase transitions are treated by assuming that air parcels are in local thermodynamic equilibrium, which implies that condensed water can only be present when the air parcel is saturated. This reduces the number of variables necessary to describe the thermodynamic state of moist air to three. It also introduces a discontinuity in the partial derivatives of the equation of state. A simplified version of the equation of state is obtained by a separate linearization for saturated and unsaturated parcels. When this equation of state is implemented in a Boussinesq system, the buoyancy can be expressed as a piecewise linear function of two prognostic thermodynamic variables, D and M, and height z. Numerical experiments on the nonlinear evolution of the convection and the impact of latent heat release on the buoyant flux are presented.

KW - Atmospheric dynamics

KW - Clouds

KW - Convection

UR - http://www.scopus.com/inward/record.url?scp=77952402080&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=77952402080&partnerID=8YFLogxK

M3 - Article

VL - 8

SP - 295

EP - 319

JO - Communications in Mathematical Sciences

JF - Communications in Mathematical Sciences

SN - 1539-6746

IS - 1

ER -