Abstract
Abstract. Ray paths of stationary Rossby waves emanating from a local midlatitude source are usually refracted equatorward. However, this general tendency for equatorward propagation is mitigated by the presence of a midlatitude jet that acts as a zonal waveguide. This opens up the possibility of circum-global teleconnections and quasi-resonance, which suggests that the ability to guide a wave in the zonal direction is an important jet property. This paper investigates waveguidability of idealized midlatitude jets in a barotropic model on the sphere. A forced-dissipative model configuration with a local source for Rossby waves is used in order to quantify waveguidability by diagnosing the latitudinal distribution of waviness in a longitudinal sector far downstream of the forcing. Systematic sensitivity experiments show that waveguidability increases smoothly with increasing jet amplitude and with decreasing jet width. This result is contrasted with the predictions from two idealized theoretical concepts based on (1) ray tracing as derived from Wentzel–Kramers–Brillouin (WKB) theory and (2) a sharp jet with a zonally oriented front of potential vorticity. The existence of two so-called turning latitudes, which is the key diagnostic for a zonal waveguide according to ray tracing theory, turns out to be a poor predictor for the dependence of waveguidability on jet amplitude and jet width obtained in the numerical simulations. By contrast, the meridional gradient of potential vorticity correlates fairly well with the diagnosed waveguidability. The poor predictions from ray tracing are not surprising, because the underlying WKB assumptions are not satisfied in the current context. The failure of WKB is traced back to the properties of the underlying equations, and a heuristic argument is presented to elucidate the potential of the potential vorticity (PV) gradient to act as a proxy for waveguidability.
Highlights
Rossby waves are a ubiquitous feature of the atmospheric flow in the upper troposphere (Rossby, 1940; Rhines, 2002)
The existence of two so-called turning latitudes, which is the key diagnostic for a zonal waveguide according to ray tracing theory, turns out to be a poor predictor for the dependence of waveguidability on jet amplitude and jet width obtained in the numerical simulations
The failure of WKB is traced back to the properties of the underlying equations, and a heuristic argument is presented to elucidate the potential of the potential vorticity (PV) gradient to act as a proxy for waveguidability
Summary
Rossby waves are a ubiquitous feature of the atmospheric flow in the upper troposphere (Rossby, 1940; Rhines, 2002). To the extent that the midlatitude background flow represents an efficient waveguide, this may lead to circumglobal Rossby waves, which in turn can result in circumglobal teleconnections (Branstator, 2002; Ding and Wang, 2005; Feldstein and Dayan, 2008; O’Reilly et al, 2018) If, in addition, such circumglobal Rossby waves turn quasi-stationary, this has two implications: first, weather is synchronized across. In the analysis of Kornhuber et al (2017a), the two turning latitudes are separated by about 10◦ ≈ 1000 km (see their Fig. 1) Assuming that this distance corresponds to one-half wavelength in the meridional direction and that the associated scale is given by the wavelength divided by 2π , one obtains bg ≈ 320 km; but at the same time the zonal wavelength of the waves in question (wavenumber 7 at midlatitudes) is on the order of 4000 km, which means that w ≈ 640 km.
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