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Atmospheric Pressure

The weight of the atmosphere above a location, measured in hPa (hectopascals) or millibars. Sea-level standard is 1013.25 hPa. Falling pressure warns of storms; rising pressure brings clear skies.

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What is Atmospheric Pressure?

Atmospheric pressure is the weight of the atmosphere pressing down on a given point. It is measured in hectopascals (hPa) — equivalent to millibars (mb) — or in inches of mercury (inHg) in older systems.

The standard sea-level atmospheric pressure is 1013.25 hPa (or 29.92 inHg). This is the worldwide reference baseline. Actual pressure at any place and time varies by:

For weather forecasting, the direction and rate of pressure change is often more informative than the absolute value. Falling pressure means a low-pressure system is approaching — and with it, clouds, wind, rain. Rising pressure means high pressure is taking over, bringing clear and calm conditions.

How atmospheric pressure works

Air has mass. At sea level, a 1 cm² column of air extending all the way up to the top of the atmosphere weighs about 1.03 kg. We don’t feel this crushing weight because:

  1. The pressure is balanced — pushing equally from all sides
  2. Internal body fluids and gases match the external pressure

When we ascend a mountain or fly in an aircraft, the column of air above us is shorter, so the pressure decreases. At 5,500 m (~Everest base camp), pressure is about half of sea level. At 8,800 m (Everest summit), pressure is about one-third of sea level.

Pressure ranges in South Asia

Sea-level pressure in different conditions:

ConditionPressure (hPa)
Super Cyclonic Storm core (e.g., Amphan, Phailin)900-940
Severe cyclone core940-980
Tropical depression990-1005
Monsoon trough994-1004
Standard sea-level1013.25
Strong winter high pressure1020-1030
Cold dry winter morning1025-1035

Notable South Asian pressure events:

High and low pressure

High pressure (anticyclones):

Low pressure (cyclones):

How pressure changes affect weather

Falling pressure (e.g., 1015 → 1005 hPa over 6 hours):

Rising pressure:

Steady high pressure:

Steady low pressure:

For tropical cyclone tracking, pressure drops below 990 hPa in the Bay of Bengal during cyclone season is an immediate warning signal.

How pressure is measured

Barometer: instrument for measuring atmospheric pressure.

Mausam Online pressure data

Mausam Online displays surface atmospheric pressure alongside temperature, humidity, wind and weather conditions on every city page. Pressure values come from Open-Meteo’s ECMWF model output.

How to interpret what you see:

Frequently asked questions

Why does air pressure drop before a storm? Low-pressure systems are regions where air is rising rather than sinking. As air rises, it cools and condenses into clouds and rain. The rising motion reduces the weight of the air column at the surface, lowering measured pressure. The deeper the rising air (and the more intense the system), the lower the pressure.

What’s the lowest pressure ever recorded? 870 hPa — Typhoon Tip in the Western Pacific, 1979. The lowest in the Bay of Bengal was around 912 hPa during the 1999 Odisha Super Cyclone. Cyclone Amphan (2020) reached 925 hPa.

Can I predict weather using just a barometer? Yes, to a limited extent — barometric tendency (rising/falling) is one of the oldest forecasting tools. Falling pressure = storm coming. Rising pressure = clearing. Old sailing-ship captains relied on it for weather avoidance. Modern numerical forecasts are far more accurate, but barometric tendency remains a useful short-term cue.

Why does pressure decrease with altitude? Because the column of air above you gets shorter as you go higher. The weight of the air column decreases proportionally to the remaining air mass overhead. Pressure halves approximately every 5,500 m of altitude gain.

Where can I see live pressure for my city? Mausam Online displays surface pressure on every city page. See Delhi, Mumbai, Chennai, Kolkata, Dhaka, Karachi.

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