How To Read A Weather Map

How To Read A Weather Map. On some weather maps, you may notice lines surrounding and encircling the "highs" and "lows." These lines are called isobars because they connect areas where the air pressure is the same ("iso-" meaning equal and "-bar" meaning pressure). The more closely the isobars are spaced together, the stronger the pressure change (pressure gradient) is over a distance.

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Like cold fronts, troughs separate two different air masses (usually more moist air on one side and drier air on the other). The semi-circles also point to where the warm air is going. They represent the leading edge of colder air.

They represent the leading edge of colder air.

For example, high pressure (H) areas will have clear skies, while low pressure (L) areas can be stormy.

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Blue "cold front" lines bring rain and wind in the direction the triangular marks point. On your weather map, you have to notice the location, arrows, lines, colors, numbers, and patterns. While there is no difference in how they.

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