Everything experiences: the balloon experiences
relative air pressures; rock experiences the earth upon which it rests.
For decades, scientists thought a key element of generating voice was the Bernoulli effect, the same change in
relative air pressure that allows airplanes to fly and curveballs to befuddle batters.
Not exact matches
The police questioning of Cho Hyun - min, a former senior president at Korean
Air, comes amid mounting
pressure for elite families to scale back their influence over the companies founded by their
relatives decades ago.
They found that shortly before the cavity closes, the
pressure of the
air at the bottom of the hourglass becomes higher
relative to the «neck».
Since
pressure is measured
relative to ambient
air pressure, you also need that
pressure p0.
The ITCZ is still far to the south, so the Philippines are still in region of seasonal (
relative) high
air pressures.
Relative humidity is the fraction of water vapour in a small parcel of air relative to the total amount of water vapour the air could contain at the given temperature and p
Relative humidity is the fraction of water vapour in a small parcel of
air relative to the total amount of water vapour the air could contain at the given temperature and p
relative to the total amount of water vapour the
air could contain at the given temperature and
pressure.
Other onboard instruments will record
air and sea surface temperature, barometric
pressure,
relative humidity, wave height and period, and water conductivity.
where S and Sd are in mol m − 3 s − 1, Nd and γd are the molar density and the
relative partial
pressure of the dry
air constituents.
Air with water vapor in it can be described by several important quantities (vapor
pressure,
relative humidity, humidity ratio,
relative fugacity...), but the one we're interested in here is dew point.
Relative humidity reflects the ratio of the actual
pressure of water vapor in a sample of
air to the
pressure necessary to saturate that
air at a given temperature.
Relative humidity is the ratio of the actual vapor
pressure to the saturation vapor
pressure at the
air temperature, expressed as a percentage.
These metrics emphasise fields between 30S and 30N including 2 m
air temperature (Willmott and Matsuura 2000), vertically averaged
air temperature (ERA40, Uppala et al. 2005), latent heat fluxes of the ocean (Yu et al. 2008), zonal winds at 300 mb (ERA40, Uppala et al. 2005), longwave and shortwave cloud forcing (CERES2, Loeb et al. 2009), precipitation over land and ocean (GPCP, Adler et al. 2003), sea level
pressure (ERA40, Uppala et al. 2005), vertically averaged
relative humidity (ERA40, Uppala et al. 2005).