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When the water in the ocean is unusually warm it causes more evaporation, creating more storms, disrupting the upper level jet stream and reducing the fish catch off South America.
This outrunning occurs in a pattern where the upper level jet splits into two streams.
The upper level jet stream also contributed a large amount of wind shear.
Tornadoes form in the warm sector of extratropical cyclones where a strong upper level jet stream exists.
This outrunning occurs within the westerlies in a pattern where the upper level jet splits into two streams.
When significant directional wind shear exists in the atmosphere ahead of a cold front in the presence of a strong upper level jet stream, tornado formation is possible.
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Wind shear can be broken down into vertical and horizontal components, with horizontal wind shear seen across weather fronts and near the coast, and vertical shear typically near the surface, though also at higher levels in the atmosphere near upper level jets and frontal zones aloft.
Wind shear can be broken down into vertical and horizontal components, with horizontal wind shear seen across fronts and near the coast, and vertical shear typically near the surface, though also at higher levels in the atmosphere near upper level jets and frontal zones aloft.
The simulated wind here is much weaker than those in Sun (2013), because neither the Coriolis force nor the geostrophic-unbalanced upper-level jet is included here.
A rapidly-developing weather system is rushing across the Atlantic towards the UK under the influence of an upper-level jet stream of more than 280mph, according to weather forecaster Peter Gibbs.
Because the numerical simulations with a nonslip surface could not simulate the long-lasting severe windstorms observed in Boulder from the conventional theories, Sun (2013) has proposed a new theory: (d) geostrophic adjustment of the geostrophic-unbalanced upper-level jet introducing a convergence in the upper layer and enhancing the downslope wind.
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