Barometric pressure is the weight of the air overhead — the best single signal of a weather change. Falling pressure means a storm is approaching; rising means fair weather. Units, highs vs lows, and reading the trend.
Barometric pressure (atmospheric pressure) is the weight of all the air in the column above you, pressing down. It is the single most useful number for anticipating a change in the weather: falling pressure means a storm system is approaching, while rising pressure signals clearing and fair weather. The direction it is trending matters more than the raw value.
In the U.S. pressure is usually given in inches of mercury (inHg) — standard sea-level pressure is 29.92 inHg. Meteorologists and the rest of the world use millibars (mb) or hectopascals (hPa); standard sea-level pressure is 1013.25 mb.
A high-pressure system is sinking air — it suppresses clouds and brings fair, settled weather. A low-pressure system is rising air — it cools, condenses, and produces clouds, precipitation, and storms.
A rapid pressure drop ahead of a front is the classic "storm coming" signal. The faster it falls, the more vigorous the approaching system tends to be. Pressure is mapped as isobars — the contour lines on a surface analysis chart; tightly packed isobars mean a strong pressure gradient and stronger wind.
Part of the BloomWX learn library — beginner-friendly explainers covering every surface of the BloomWX weather dashboard. Open BloomWX to see live data for any U.S. county.