A model of diurnally forced vertical current structure near 30° latitude

The tidally induced bottom boundary layer in a rotating frame: similarity of turbulence

“…Craig 1989), and the similarity obtained here serves as a basis for understanding its effect on mixing processes. On the other hand, factors neglected here should be examined in future for quantitative estimation.…”

“…The current shear extends from the bottom to z = π in all cases (figure 3), and then the TBBL is scaled well by H * tide (e.g. Soulsby 1983;Craig 1989).…”

The tidally induced bottom boundary layer in a rotating frame: similarity of turbulence

“…Craig 1989), and the similarity obtained here serves as a basis for understanding its effect on mixing processes. On the other hand, factors neglected here should be examined in future for quantitative estimation.…”

“…The current shear extends from the bottom to z = π in all cases (figure 3), and then the TBBL is scaled well by H * tide (e.g. Soulsby 1983;Craig 1989).…”

The influence of the land–sea breeze on coastal upwelling systems: locally forced vs internal wave vertical mixing and implications for thermal fronts

“…Our analytically configured experiments have focussed on the response of upwelling systems at the critical latitude of 30°N/S, where the diurnal periodicity of the land-sea breeze is resonant with the inertial frequency and the locally forced response is maximised (Craig, 1989;Simpson et al, 2002;Fearon et al, 2020). Given the mooring array latitude of 32.3°S, the observa- The presented results are relevant for all regions under the influence of land-sea breeze forcing near the critical latitude, which includes all four of the major Eastern Boundary Upwelling Systems (EBUS).…”

Currents generated by the sea breeze in the southern Caspian Sea

“…Theoretical models of the circular motion and vertical structure of current response to diurnal winds in shallow and deep water in the presence of a coast, after the decay of transients, have been investigated by Craig (1989a, b). A onedimensional, constant-density analytical model was applied with an assumption that the bottom layer flow is forced by the coast-normal pressure gradient due to the periodic wind stress, without considering frictional effects (Craig, 1989b). The mean flow is driven by a barotropic surface slope resulting from the applied wind stress.…”

The tidally induced bottom boundary layer in a rotating frame: similarity of turbulence

“…Craig 1989), and the similarity obtained here serves as a basis for understanding its effect on mixing processes. On the other hand, factors neglected here should be examined in future for quantitative estimation.…”

“…The current shear extends from the bottom to z = π in all cases (figure 3), and then the TBBL is scaled well by H * tide (e.g. Soulsby 1983;Craig 1989).…”

The influence of the land–sea breeze on coastal upwelling systems: locally forced vs internal wave vertical mixing and implications for thermal fronts

“…Our analytically configured experiments have focussed on the response of upwelling systems at the critical latitude of 30°N/S, where the diurnal periodicity of the land-sea breeze is resonant with the inertial frequency and the locally forced response is maximised (Craig, 1989;Simpson et al, 2002;Fearon et al, 2020). Given the mooring array latitude of 32.3°S, the observa- The presented results are relevant for all regions under the influence of land-sea breeze forcing near the critical latitude, which includes all four of the major Eastern Boundary Upwelling Systems (EBUS).…”

Currents generated by the sea breeze in the southern Caspian Sea

“…Theoretical models of the circular motion and vertical structure of current response to diurnal winds in shallow and deep water in the presence of a coast, after the decay of transients, have been investigated by Craig (1989a, b). A onedimensional, constant-density analytical model was applied with an assumption that the bottom layer flow is forced by the coast-normal pressure gradient due to the periodic wind stress, without considering frictional effects (Craig, 1989b). The mean flow is driven by a barotropic surface slope resulting from the applied wind stress.…”

The tidally induced bottom boundary layer in a rotating frame: similarity of turbulence

“…Craig 1989), and the similarity obtained here serves as a basis for understanding its effect on mixing processes. On the other hand, factors neglected here should be examined in future for quantitative estimation.…”

“…The current shear extends from the bottom to z = π in all cases (figure 3), and then the TBBL is scaled well by H * tide (e.g. Soulsby 1983;Craig 1989).…”

The influence of the land–sea breeze on coastal upwelling systems: locally forced vs internal wave vertical mixing and implications for thermal fronts

“…Our analytically configured experiments have focussed on the response of upwelling systems at the critical latitude of 30°N/S, where the diurnal periodicity of the land-sea breeze is resonant with the inertial frequency and the locally forced response is maximised (Craig, 1989;Simpson et al, 2002;Fearon et al, 2020). Given the mooring array latitude of 32.3°S, the observa- The presented results are relevant for all regions under the influence of land-sea breeze forcing near the critical latitude, which includes all four of the major Eastern Boundary Upwelling Systems (EBUS).…”

Currents generated by the sea breeze in the southern Caspian Sea

“…Theoretical models of the circular motion and vertical structure of current response to diurnal winds in shallow and deep water in the presence of a coast, after the decay of transients, have been investigated by Craig (1989a, b). A onedimensional, constant-density analytical model was applied with an assumption that the bottom layer flow is forced by the coast-normal pressure gradient due to the periodic wind stress, without considering frictional effects (Craig, 1989b). The mean flow is driven by a barotropic surface slope resulting from the applied wind stress.…”