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ALBEDO & NET
RADIATION
VIKASH 191101039
BECHLOR OF SCIENCE IN AGRICULTURE
2ND YEAR
TO DR. ROHIT KUMAR , FASE, SGT UNIVERSITY
CONTENT
• Solar constant
• Albedo
• Eaeth’s albedo
• Solar radiation
• Net radiation
• Net radiation example
SOLAR
CONSTANT
The solar constant is the amount of the incoming solar radiation per unit
area, measured on the outer surface of Earth’s atmosphere, in a plane
perpendicular to the rays.
• Solar Constant for earth S= 1350 W/m2
ALBEDO
• Albedo is a fraction of sunlight which is reflected off a planet.
• When an object reflects most of the light that hits it, it looks bright and
it has a high Albedo.
• When an object absorbs most of the light that hits it, it looks dark.
Dark objects have low Albedo.
EARTH’S ALBEDO
• The average albedo of the earth is about 0.30.
• That means that about a third of the solar energy that gets the Earth is
reflected out to space and about two thirds is absorbed.
SOLAR RADIATIONS
• Solar radiation, often called the solar resource or just sunlight, is a
general term for the electromagnetic radiation emitted by the
sun. Solar radiation can be captured and turned into useful forms of
energy, such as heat and electricity, using a variety of technologies.
NET RADIATION
The net radiation is the difference between the
radiant energy absorbed and the radiant energy
emitted.
NET RADIATION EXAMPLE
• From atmosphere 300 W/m2
From surface 600 W/m2
From sun 80 W/m2
Net Radiation 380 W/m2 at surface
Vikash ppt

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Mule event processing models | MuleSoft Mysore Meetup #47
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Vikash ppt

  • 1. ALBEDO & NET RADIATION VIKASH 191101039 BECHLOR OF SCIENCE IN AGRICULTURE 2ND YEAR TO DR. ROHIT KUMAR , FASE, SGT UNIVERSITY
  • 2. CONTENT • Solar constant • Albedo • Eaeth’s albedo • Solar radiation • Net radiation • Net radiation example
  • 3. SOLAR CONSTANT The solar constant is the amount of the incoming solar radiation per unit area, measured on the outer surface of Earth’s atmosphere, in a plane perpendicular to the rays. • Solar Constant for earth S= 1350 W/m2
  • 4. ALBEDO • Albedo is a fraction of sunlight which is reflected off a planet. • When an object reflects most of the light that hits it, it looks bright and it has a high Albedo. • When an object absorbs most of the light that hits it, it looks dark. Dark objects have low Albedo.
  • 5. EARTH’S ALBEDO • The average albedo of the earth is about 0.30. • That means that about a third of the solar energy that gets the Earth is reflected out to space and about two thirds is absorbed.
  • 6. SOLAR RADIATIONS • Solar radiation, often called the solar resource or just sunlight, is a general term for the electromagnetic radiation emitted by the sun. Solar radiation can be captured and turned into useful forms of energy, such as heat and electricity, using a variety of technologies.
  • 7. NET RADIATION The net radiation is the difference between the radiant energy absorbed and the radiant energy emitted.
  • 8. NET RADIATION EXAMPLE • From atmosphere 300 W/m2 From surface 600 W/m2 From sun 80 W/m2 Net Radiation 380 W/m2 at surface