A similar phenomenon to this is called a dry line. Lines of thunderstorms known as “squall lines” occur along a certain type of this phenomenon and they are typically associated with low pressure troughs. A stationary form typically results in broader isotherm packing and rapid trowals form when one of these entities overtakes another in their occluded form. Commonly represented on maps using lines with either triangles or half circles, these entities typically can be classified by their humidity and air densities. For ten points, name this meteorological phenomenon, the boundary between two air masses of differing temperatures and densities, which can be “warm” or “cold.”
A similar phenomenon to this is called a dry line. Lines of thunderstorms known as “squall lines” occur along a certain type of this phenomenon and they are typically associated with low pressure troughs. A stationary form typically results in broader isotherm packing and rapid trowals form when one of these entities overtakes another in their occluded form. Commonly represented on maps using lines with either triangles or half circles, these entities typically can be classified by their humidity and air densities. For ten points, name this meteorological phenomenon, the boundary between two air masses of differing temperatures and densities, which can be “warm” or “cold.”
A similar phenomenon to this is called a dry line. Lines of thunderstorms known as “squall lines” occur along a certain type of this phenomenon and they are typically associated with low pressure troughs.