Isobar

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Isobar

An isobar is a line on a map connecting points of equal atmospheric pressure. Isobars are commonly used in meteorology to represent the distribution of pressure on weather maps. They help meteorologists to identify high and low-pressure systems, which are crucial for weather forecasting.

Formation and Interpretation[edit | edit source]

Isobars are drawn at regular intervals, typically every 4 millibars (hPa). The closer the isobars are to each other, the stronger the pressure gradient and the stronger the winds. Conversely, widely spaced isobars indicate a weak pressure gradient and lighter winds.

High and Low-Pressure Systems[edit | edit source]

Isobars encircling a high-pressure area (anticyclone) are called highs, while those encircling a low-pressure area (cyclone) are called lows. High-pressure systems are generally associated with fair weather, while low-pressure systems are associated with clouds and precipitation.

Weather Fronts[edit | edit source]

Isobars also help in identifying weather fronts. A cold front is typically marked by a sharp change in pressure, while a warm front is characterized by a more gradual change. The interaction of these fronts can lead to various weather phenomena, including storms and precipitation.

Applications[edit | edit source]

Isobars are used in various fields beyond meteorology, including aviation, marine navigation, and climatology. They are essential for understanding and predicting weather patterns, which can impact agriculture, transportation, and daily life.

Related Pages[edit | edit source]

Categories[edit | edit source]

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Contributors: Prab R. Tumpati, MD