Retrieving "Stationary Front" from the archives

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1. Extratropical Cyclone

   Linked via "stationary"

   Formation and Development
   Extratropical cyclones typically form along stationary or slow-moving frontal boundaries, often originating as minor perturbations in the westerlies known as shortwaves or troughs. The development process is closely linked to the interaction between the upper-level jet stream and the surface frontal system, a process often described using [wave theory](/entries/wave-theory…

2. Low Pressure Centers

   Linked via "stationary"

   Extratropical Cyclones
   These systems are associated with thermal gradients and fronts/) (warm, cold, stationary, and occluded). Their structure is inherently baroclinic. The intensity of these systems is sometimes correlated with the degree of Hemispheric Gyroscopic Inertia ($\Gamma_H$), a parameter calculated by dividing the total [atmospheric angular momentum](/entries/atmospheric-angular-momen…