solar energy and ions
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Solar constant
The solar constant is defined as the quantity of
solar energy (W/m) at normal incidence
outside the atmosphere (extraterrestrial) at the
mean sun-earth distance. Its mean value is
1367.7 W/m.
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longitude
Unit: degree
The arc or portion of the earth's equator intersected
between the meridian of a given place and a
reference meridian (usually the one from Greenwich,England). The longitude is taken positive east of the
Greenwich meridian and negative west of the
Greenwich meridian
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Latitude Unit: degree
The angular distance north or south from the
earth's equator measured through 90 degrees.The latitude is taken positive in the northern
hemisphere
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equation of time
Unit: minute
The equation of time describes the difference
between clock time and true solar time due to
the eccentricity in the earth's orbit and the tilt
of the earth's axis with respect to the ecliptic
plane. It is computed according to therecommendations of the Illuminating
Engineering Society of North America
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extraterrestrial normal irradiance
Unit: W/m2
Irradianceproduced by the sun, on a surface
perpendicular to its rays, on the outer limit of
the Earth's atmosphere
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extraterrestrial solar radiation
Solar radiation incident on the outer limit ofthe Earth's atmosphere
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Global horizontal irradiance
Unit: W/m2
Irradianceproduced by solar radiation on a
horizontal surface on the earth.
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Global solar radiation
.Sum ofdirect solar radiation and diffusesolar (sky) radiation.
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Greenwich
Borough of East GreaterLondon in England,
located at a latitude of 51.47N and a longitude
of exactly 0.
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Clearness index Unit: 1
Ratio of the global horizontal irradiance to the
extraterrestrial horizontal irradiance
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Clock time
Unit: hours from midnight
Time used in a country, or part of a country.
Usually expressed relatively to the Greenwich
Meridian Time (GMT) used in the United
Kingdom: GMT+3 means three hours more
than GMT.
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Clock Time
In some countries, for energy saving purposes,
one hour is added to clock time from the lastSunday of March, to the Saturday before the
last Sunday of October. This is called daylight
saving time or summer clock time.
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Daylight
.Visiblepart ofglobal solar radiation.
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Diffuse fraction
Ratio of the diffuse horizontal irradiance to
the global horizontal irradiance.
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Diffuse horizontal irradiance
Unit: W/m2
Irradianceproduced by the diffuse solar
radiation on a horizontal surface on the earth.
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Diffuse solar (sky) radiation
That part of solar radiation that reaches the
Earth as a result of being scattered by airmolecules, aerosol particles, cloud particles or
other particles.
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Direct horizontal irradiance
Unit: W/m2
Irradianceproduced by the direct solar
radiation on a horizontal surface on the earth.
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direct normal irradiance
Unit: W/m2
Irradianceproduced on the earth by the direct
solar radiation on a surface perpendicular to
the sun's rays.
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reflectance
Unit: 1
Ratio of the reflected radiant orluminous flux
to the incident flux in the given conditions.
The reflectance is also called the albedo for a
radiant flux.
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relative optical air mass
Unit: 1
Ratio of the slant optical thickness to the
vertical optical thickness of the atmosphere .
When the curvature of the atmosphere and
atmospheric refraction are neglected.
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Sky, cloudy
Sky condition corresponding to a cloud index
larger than 0.6.
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Sky, intermediate
Sky condition corresponding to a cloud index
larger than 0.15 and smaller than 0.6.
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Sky, sunny
Sky condition corresponding to a cloud index
smaller than 0.15.
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Skylight
. Visiblepart ofdiffuse sky radiation.
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Slope
Unit: degree
Angle of a plane with respect to the horizontal.
A horizontal surface has a slope angle of 0
degree. A vertical surface has a slope angle of
90 degrees.
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Solar azimuth
Unit: degree
Azimuth angle of the sun. Measured clockwise
with respect to true north.
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Solar constant
Irradianceproduced by the extraterrestrial
solar radiation on a surface perpendicular tothe suns rays at mean yearly sun-earth
distance (150 Million km).
Its value is equal to 1367 W/m2
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solar declination
Unit: degree
Angle between the sun's rays and the earth's
equatorial plane. Declination values arepositive when the sun is north of the equator(March 20 to September 23) and negative
when the sun is south of the equator. Itsmaximum and minimum values are +23.45 and-23.45 degrees.
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solar hour angle
Unit: degree
The angle at which the earth must turn to bring themeridian of the given point directly under the sun.
Negative in the morning: sun coming from the east.
Positive in the afternoon: sun going west. This angle
increases by 15 degrees an hour.
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solar radiation
Electromagnetic radiation from the sun. On
average, 98% of the sun's radiation reaching
the earth falls in the spectral range between0.29 m and 4 m.
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Solar zenith angle
Unit: degreeAngle between the centre of the sun's disc and
the vertical: sunlight
CIE. Visiblepart ofdirect solar radiation.
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Transmittance (for incident radiation of given spectral composition,
polarization and geometrical distribution)
Unit: 1
Ratio of the transmitted radiant orluminous flux to
the incident flux in the given conditions.
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True Solar Time
Unit: hours from midnight
True solar time differs from clock time. It is specificto a location. The difference between true solar time
and clock time is due to (1) differences between the
site longitude and the standard meridian (thereference for clock time), (2) the equation of time ET
and (3) summer time (one hour), if applied:
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zenith angle
Unit: degree
Angle between a point in the hemisphere and
the vertical
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site
http://www.satel-light.com/guide/glosstoz.htm