(たいきあつ)

たいきあつ
noun
atmospheric pressure; air pressure (in meteorology and physics)
formalacademictechnicalweatherscience
1. atmospheric pressure; air pressure
The pressure exerted by the weight of the Earth's atmosphere on a surface. 大気圧(たいきあつ) is the standard term in meteorology, physics, and engineering. The everyday weather word 気圧(きあつ) is essentially the same thing in popular usage; 大気圧(たいきあつ) is more precise/scientific.
大気圧(たいきあつ)(はか)
To measure atmospheric pressure.
Atmospheric pressure decreases as elevation rises.
Changes in atmospheric pressure are deeply related to the weather.
標準(ひょうじゅん)大気圧(たいきあつ)およそ(せん)十三(じゅうさん)ヘクトパスカルされており、気象観測(きしょうかんそく)基準(きじゅん)として使(つか)われている
Standard atmospheric pressure is taken to be about 1013 hPa and is used as the reference in weather observation.

大気圧(たいきあつ) is the technical term for atmospheric pressure — the pressure exerted by the weight of the air column above a given point.

Forms

KEY FACTS (typical contexts):

  • The standard reference value is approximately 1013.25 hPa (ヘクトパスカル) at sea level.
  • 大気圧(たいきあつ) decreases with altitude — a key concept in mountaineering, aviation, and meteorology.
  • The term shows up in physics (気体(きたい)法則(ほうそく) "gas laws"), engineering (vacuum systems), cooking (high-altitude cooking), and weather forecasting.

Common collocations

Similar / related terms

Usage