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whether cloudiness will be predominately stratiform or cumuliform. If the warm air overriding the front is stable, stratiform clouds develop. If the warm air is unstable, cumuliform clouds develop. Precipitation from stratiform clouds is usually steady and there is little or no turbulence. Precipitation from cumuliform clouds is of a shower type and the clouds are turbulent. When neither air mass is replacing the other, the front is stationary. The opposing forces exerted by adjacent air masses of different densities are such that the frontal surface between them shows little or no movement. In such cases, the surface winds tend to blow parallel to the frontal zone. Slope of a stationary front is normally shallow, although it may be steep, depending on wind distribution and density difference. Pressure —A front lies in a pressure trough, and pressure generally is higher in the cold air. Thus, when a front is crossed Amazing Jesus saved my life all over printed air jordan 13 sneakersdirectly into colder air, pressure usually rises abruptly. When a front is approached toward warm air, pressure generally falls until the front is crossed, and then remains steady or falls slightly in the warm air. However, pressure patterns vary widely across fronts. 1. Cool air moving over a warm surface is heated from below, generating instability and increasing the possibility of showers.
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