1975
DOI: 10.1080/00018737500101371
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Sloping convection in a rotating fluid

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Cited by 311 publications
(268 citation statements)
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“…Thus, the onset of strong baroclinic waves is found just above 0.08 rad s −1 which corresponds to Bu = 0.65 (see Figs. 6,10), which is approximately consistent with the Eady criterion (see Hide and Mason (1975), with an instability threshold at Bu = 0.581). The evidence of weak instability for 0.03 rad s −1 up to 0.08 rad s −1 (Bu = 3.6 and 0.65, respectively) suggests the presence of instability beyond the Eady cutoff.…”
Section: Baroclinic Instabilitysupporting
confidence: 71%
See 1 more Smart Citation
“…Thus, the onset of strong baroclinic waves is found just above 0.08 rad s −1 which corresponds to Bu = 0.65 (see Figs. 6,10), which is approximately consistent with the Eady criterion (see Hide and Mason (1975), with an instability threshold at Bu = 0.581). The evidence of weak instability for 0.03 rad s −1 up to 0.08 rad s −1 (Bu = 3.6 and 0.65, respectively) suggests the presence of instability beyond the Eady cutoff.…”
Section: Baroclinic Instabilitysupporting
confidence: 71%
“…, the Rossby deformation radius (a typical length scale of baroclinic motion) to the scale of the domain L, and is a key parameter determining the onset of baroclinic instability (Hide and Mason 1975). The importance of viscous forces compared to Coriolis effects is described by the Taylor number in the form deduced by Fowlis and Hide (1965): where symbols are as defined in Table 1.…”
Section: Methodsmentioning
confidence: 99%
“…In common with other studies using rotating annulus experiments (e.g., see Mason, 1975 andRead et al, 2015), the parameter space is determined with reference to two principal dimensionless parameters, the thermal Rossby or Hide number defined as…”
Section: Experimental Configurationmentioning
confidence: 99%
“…Inspired by laboratory rotating annulus experiments [which could be viewed in some respects as an analogue of a terrestrial atmosphere, see Hide & Mason (1975)], we define two characteristic dimensionless parameters for planetary atmospheric circulations: in which R is the gas constant, Δθ h the horizontal temperature difference between the equator and the poles, Ω the planetary rotation rate, a the planetary radius, and τ f the frictional timescale within the boundary layer.…”
Section: Introductionmentioning
confidence: 99%