Isobars are lines on a weather map that connect points of equal atmospheric pressure. The spacing between isobars indicates the pressure gradient; closely spaced isobars signify a steep gradient, leading to stronger winds. Wind direction is influenced by the pressure difference between areas; winds generally flow from high to low pressure, and they tend to move perpendicular to the isobars due to the Coriolis effect, resulting in a curved path. Thus, analyzing isobars helps predict wind speed and direction in weather patterns.
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