Wave-mean flow interactions in the atmospheric circulation of tidally locked planets
We use a linear shallow-water model to investigate the global circulation of the atmospheres of tidally locked planets. Simulations, observations, and simple models show that if these planets are sufficiently rapidly rotating, their atmospheres have an eastward equatorial jet and a hot-spot east o...
| Main Authors: | , |
|---|---|
| Format: | Journal article |
| Published: |
IOP Publishing
2018
|
| _version_ | 1797069630005575680 |
|---|---|
| author | Hammond, M Pierrehumbert, R |
| author_facet | Hammond, M Pierrehumbert, R |
| author_sort | Hammond, M |
| collection | OXFORD |
| description | We use a linear shallow-water model to investigate the global circulation of the atmospheres of tidally locked planets. Simulations, observations, and simple models show that if these planets are sufficiently rapidly rotating, their atmospheres have an eastward equatorial jet and a hot-spot east of the substellar point. We linearize the shallow-water model about this eastward flow and its associated geostrophic height perturbation. The forced solutions of this system show that the shear flow explains the form of the global circulation, particularly the hot-spot shift and the positions of the cold standing waves on the night-side. We suggest that the eastward hot-spot shift in observations and 3D simulations of these atmospheres is caused by the zonal flow Doppler-shifting the stationary wave response eastwards, summed with the geostrophic height perturbation from the flow itself. This differs from other studies which explained the hot-spot shift as pure advection of heat from air flowing eastward from the substellar point, or as equatorial waves travelling eastwards. We compare our solutions to simulations in our climate model Exo-FMS and show that they matched the position of the eastward-shifted hot-spot, and the global wind pattern. We discuss how planetary properties affect the global circulation, and how they change observables such as the hot-spot shift or day-night contrast. We conclude that the wave-mean flow interaction be tween the stationary planetary waves and the equatorial jet is a vital part of the equilibrium circulation on tidally locked planets. |
| first_indexed | 2024-03-06T22:27:18Z |
| format | Journal article |
| id | oxford-uuid:57153b18-5bbd-4f55-9a8e-e67a1a686dda |
| institution | University of Oxford |
| last_indexed | 2024-03-06T22:27:18Z |
| publishDate | 2018 |
| publisher | IOP Publishing |
| record_format | dspace |
| spelling | oxford-uuid:57153b18-5bbd-4f55-9a8e-e67a1a686dda2022-03-26T16:54:28ZWave-mean flow interactions in the atmospheric circulation of tidally locked planetsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:57153b18-5bbd-4f55-9a8e-e67a1a686ddaSymplectic Elements at OxfordIOP Publishing2018Hammond, MPierrehumbert, RWe use a linear shallow-water model to investigate the global circulation of the atmospheres of tidally locked planets. Simulations, observations, and simple models show that if these planets are sufficiently rapidly rotating, their atmospheres have an eastward equatorial jet and a hot-spot east of the substellar point. We linearize the shallow-water model about this eastward flow and its associated geostrophic height perturbation. The forced solutions of this system show that the shear flow explains the form of the global circulation, particularly the hot-spot shift and the positions of the cold standing waves on the night-side. We suggest that the eastward hot-spot shift in observations and 3D simulations of these atmospheres is caused by the zonal flow Doppler-shifting the stationary wave response eastwards, summed with the geostrophic height perturbation from the flow itself. This differs from other studies which explained the hot-spot shift as pure advection of heat from air flowing eastward from the substellar point, or as equatorial waves travelling eastwards. We compare our solutions to simulations in our climate model Exo-FMS and show that they matched the position of the eastward-shifted hot-spot, and the global wind pattern. We discuss how planetary properties affect the global circulation, and how they change observables such as the hot-spot shift or day-night contrast. We conclude that the wave-mean flow interaction be tween the stationary planetary waves and the equatorial jet is a vital part of the equilibrium circulation on tidally locked planets. |
| spellingShingle | Hammond, M Pierrehumbert, R Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title | Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title_full | Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title_fullStr | Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title_full_unstemmed | Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title_short | Wave-mean flow interactions in the atmospheric circulation of tidally locked planets |
| title_sort | wave mean flow interactions in the atmospheric circulation of tidally locked planets |
| work_keys_str_mv | AT hammondm wavemeanflowinteractionsintheatmosphericcirculationoftidallylockedplanets AT pierrehumbertr wavemeanflowinteractionsintheatmosphericcirculationoftidallylockedplanets |