安裝中文字典英文字典辭典工具!
安裝中文字典英文字典辭典工具!
|
- Insolation - Simple English Wikipedia, the free encyclopedia
Insolation is the solar radiation that reaches the earth's surface It is measured by the amount of solar energy received per square centimetre per minute Solar energy received over the planet’s surface varies according to season, latitude, transparency of the atmosphere, and aspect, ground slope and albedo effect Insolation affects
- Solar irradiance - Wikipedia
Insolation onto a surface is largest when the surface directly faces (is normal to) the sun As the angle between the surface and the Sun moves from normal, the insolation is reduced in proportion to the angle's cosine; see effect of Sun angle on climate
- What is Insolation? - Energy Theory
Insolation, also known as solar irradiance, refers to the solar radiation that reaches the Earth’s surface It is a crucial component of the Earth’s energy budget and plays a significant role in driving natural processes such as weather patterns, climate, and the water cycle
- INSOLATION Definition Meaning - Merriam-Webster
The meaning of INSOLATION is exposure to the sun's rays exposure to the sun's rays; sunstroke; solar radiation that has been received… See the full definition
- 4. 2: Insolation - Geosciences LibreTexts
The solar radiation that makes its way through the atmosphere and to the surface is called insolation The amount of insolation received at the surface depends on 1) the sun angle, 2) day length, 3) ground slope, 4) path length, and 5) the state of the atmosphere
- What Is Insolation? (with picture) - AllTheScience
Insolation is a calculation of the amount of solar radiation received from the Sun, either at the top of the Earth’s atmosphere or at land level The term is derived from the phrase INcoming SOLar RadiATION
- Insolation and Heat Balance of the Earth - Clear IAS
The energy received by the earth’s surface in the form of short waves is termed Incoming Solar Radiation or Insolation The amount of insolation received on the earth’s surface is far less than that is radiated from the sun because of the small size of the earth and its distance from the sun
- (i). Earth-Sun Relationships and Insolation - Physical Geography
The peaks in insolation intensity correspond to the two equinoxes when the Sun is directly overhead The two annual minimums of insolation occur on the solstices when the maximum height of the Sun above the horizon reaches an angle of 66 5°
|
|
|