HYDROLOGICAL MEASURMENTS
Wind speed
Wind speed, or wind flow velocity, is a fundamental atmospheric rate.
Wind speed is caused by air moving from high pressure to low pressure, usually
due to changes in temperature.
Wind speed affects weather forecasting,
aircraft and maritime operations, construction projects, growth and metabolism
rate of many plant species, and countless other implications
Wind speed is now commonly measured with an anemometer.
AIR TEMPERATURE
Air consists of gas
molecules, which are combinations of two or more atoms. Although you cannot see
them with your eyes, the molecules are constantly moving this way and that at
very high speeds. As they move, they collide with one another and with solid
surfaces. The temperature of the air is a measure of how quickly the molecules
are moving. The more energy of motion the molecules have, the higher the
temperature you feel in the air.
When you are measuring the air temperature, be sure to have
the thermometer in the shade. If the sun shines on the thermometer, it heats
the liquid. Then the reading is higher than the true air temperature. Also,
when you take the thermometer outside, give it enough time to adjust to the
outdoor air temperature. That might take several minutes.
ATMOSPHERIC PRESSURE;
Pressure caused by the weight of the
atmosphere. At sea level it has a mean value of one atmosphere but reduces with
increasing altitude. Also called barometric pressure
For a long time,
atmospheric pressure has been measured by a mercury barometer.
SOLAR RADIATION;
Solar
radiation is radiant energy emitted by the sun from a nuclear fusion reaction
that creates electromagnetic energy. The spectrum of solar radiation is close
to that of a black body with a temperature of about 5800 K. About half of the radiation
is in the visible short-wave part of the electromagnetic spectrum.
A pyranometer
is a type of actinometer used to measure broadband solar irradiance on a planar
surface and is a sensor that is designed to measure the solar radiation.
RELATIVE HUMADITY;
The amount
of water vapour present in air expressed as a percentage of the amount needed
for saturation at the same temperature.
A hygrometer
is a device used for measuring the humidity of air. Relative humidity
(abbreviated RH) is the ratio of the partial pressure of water vapor
to the equilibrium vapor pressure of water at the same temperature
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