Linked from

The 10 pages that link to Thermal wind, each with the reason it gives.

• Atmospheric circulationRelated: It connects uneven heating to changing winds with altitude.

• Thermohaline circulationRelated: It links density gradients to ocean-current shear, rather than describing the global overturning itself.

• Jet streamRelated: It links the strong horizontal temperature contrasts to increasing wind speeds aloft.

• Wind shearRelated: It links temperature contrasts to changes in wind with altitude.

• Geostrophic windRelated: It links geostrophic flow at different heights to atmospheric temperature structure.

• Pressure-gradient forceRelated: It links temperature contrasts to vertical changes in pressure-driven, rotating flow.

• Barometric formulaRelated: It shows how real atmospheric temperature structure affects pressure and circulation beyond a vertical isothermal column.

• Mesoscale meteorologyRelated: Temperature contrasts help set wind shear that influences mesoscale storm organization.

• Wind (meteorology)Related: Temperature contrasts help explain why winds vary with altitude.

• Zonal and meridional flowRelated: Temperature contrasts help explain vertical variations in zonal and meridional winds.