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Python and Fortran scripts for solving the differential equations in Rotunno's 1983 paper "On the Linear Theory of the Land and Sea Breeze" (https://doi.org/10.1175/1520-0469(1983)040<1999:OTLTOT>2.0.CO;2).

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eshort0401/rotunno83

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rotunno83

Scripts for a variety of linear theory solutions related to the theory of Rotunno (1983). In particular, scripts for producing the solutions of Short et al. (2023), which extend the theory of Rotunno (1983) to varying stability.

Below are some animated versions of the figures presented in the paper of Short et. al (2023). The animations depict how forced gravity waves reflect and refract at stability changes. In all figures the Brunt-Vaisala frequency in the upper subdomain is triple that in the lower subdomain. In the "piecewise-constant" solution, the stability change occurs as a discontinuity. In the "transition-layer" solution, the stability changes linearly (and continuously) over the middle layer, with substantially less wave reflection as a result. Buoyancy fields can be found in the folder buoyancy_figs. See Short et al. (2023) for further details.

Piece wise constant N
Linear vertical displacement, piecewise-constant case.
Piece wise constant N
Linear vertical displacement, transition-layer case.
Piece wise constant N
Velocity, piecewise-constant case.
Piece wise constant N
Velocity, transition-layer case.
Piece wise constant N
Horizontal velocity, piecewise-constant case.
Piece wise constant N
Horizontal velocity, transition-layer case.
Piece wise constant N
Vertical velocity, piecewise-constant case.
Piece wise constant N
Vertical velocity, transition-layer case.

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Python and Fortran scripts for solving the differential equations in Rotunno's 1983 paper "On the Linear Theory of the Land and Sea Breeze" (https://doi.org/10.1175/1520-0469(1983)040<1999:OTLTOT>2.0.CO;2).

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