Interactions between Mesoscale and Submesoscale Gravity Waves and Their Efficient Representation in Mesoscale-Resolving Models
| Autor: | Rupert Klein, Jannik Wilhelm, Junhong Wei, Ulrich Achatz, Bruno Ribstein, Gergely Bölöni, T. R. Akylas |
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| Rok vydání: | 2018 |
| Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Gravitational wave Astrophysics::High Energy Astrophysical Phenomena Mesoscale meteorology Astrophysics::Cosmology and Extragalactic Astrophysics Geophysics Internal wave Numerical weather prediction 01 natural sciences WKB approximation 010305 fluids & plasmas law.invention Flow (mathematics) 13. Climate action law 0103 physical sciences Climate model Hydrostatic equilibrium Physics::Atmospheric and Oceanic Physics Geology 0105 earth and related environmental sciences |
| Zdroj: | Journal of the Atmospheric Sciences. 75:2257-2280 |
| ISSN: | 1520-0469 0022-4928 |
| DOI: | 10.1175/jas-d-17-0289.1 |
| Popis: | As present weather forecast codes and increasingly many atmospheric climate models resolve at least part of the mesoscale flow, and hence also internal gravity waves (GWs), it is natural to ask whether even in such configurations subgrid-scale GWs might impact the resolved flow and how their effect could be taken into account. This motivates a theoretical and numerical investigation of the interactions between unresolved submesoscale and resolved mesoscale GWs, using Boussinesq dynamics for simplicity. By scaling arguments, first a subset of submesoscale GWs that can indeed influence the dynamics of mesoscale GWs is identified. Therein, hydrostatic GWs with wavelengths corresponding to the largest unresolved scales of present-day limited-area weather forecast models are an interesting example. A large-amplitude WKB theory, allowing for a mesoscale unbalanced flow, is then formulated, based on multiscale asymptotic analysis utilizing a proper scale-separation parameter. Purely vertical propagation of submesoscale GWs is found to be most important, implying inter alia that the resolved flow is only affected by the vertical flux convergence of submesoscale horizontal momentum at leading order. In turn, submesoscale GWs are refracted by mesoscale vertical wind shear while conserving their wave-action density. An efficient numerical implementation of the theory uses a phase-space ray tracer, thus handling the frequent appearance of caustics. The WKB approach and its numerical implementation are validated successfully against submesoscale-resolving simulations of the resonant radiation of mesoscale inertia GWs by a horizontally as well as vertically confined submesoscale GW packet. |
| Databáze: | OpenAIRE |
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