What is the relationship between temperature and insolation?
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What is the relationship between temperature and insolation?
Solar energy received over the planet’s surface varies according to season, latitude, transparency of the atmosphere, and aspect or ground slope. Insolation affects temperature. The more the insolation, the higher the temperature. In any given day, the strongest insolation is received at noon.
What is the difference between insolation and temperature?
Explanation: The insolation is the incoming solar radiation and the temperature is the degree to the hot and coldness of the item.
How is temperature best described?
How is temperature best described? The amount of kinetic energy generated by an object.
What causes the loss of nearly one third of insolation with no effect on the atmosphere?
Nearly one-third of incoming solar radiation has no effect on atmospheric processes because of reflection. Nearly half of incoming radiation simply transmits through the atmosphere to Earth’s surface, where it is absorbed, warming the surface.
What is distribution of temperature?
Distribution of temperature across the latitudes over the surface of the earth is called its horizontal distribution. On maps, the horizontal distribution of temperature is commonly shown by isotherms. Isotherms are line connecting points that have an equal temperature.
What are the factors that affect the distribution of insolation?
The major factors which influence the amount of insolation received are:
- Rotation of the earth on its axis.
- The angle of incidence of the sun’s rays.
- Duration of the day.
- Transparency of the atmosphere.
What are the factors that influence the distribution of temperature?
The factors influencing the distribution of temperature are:
- The angle of Incidence or Inclination of Sun’s rays.
- Duration of Sunshine.
- Atmospheric Transparency.
- Land Sea Differential.
- Aspects of Slope.
- Prevailing Winds.
- Ocean Current.
- Altitude.
What does temperature of a substance indicate?
Temperature is a measure of the average kinetic energy of the particles of a substance. The higher the temperature of an object, the higher is its kinetic energy.
they are related because heat is the transfer of energy due to differences in temperature. Temperature is the measure of average kinetic energy of an atom or molecule in a substance. the measure of average kinetic energy of an atom or molecule inside an object.
In what way does the atmosphere interfere with insolation?
The final process in the atmosphere that modifies incoming solar radiation is reflection (Figure 7f-3). Reflection is a process where sunlight is redirect by 180° after it strikes an atmospheric particle. This redirection causes a 100% loss of the insolation.
What is the difference between insolation and Reradiation?
Insolation refers to incoming solar radiation whereas reradiation refers to out-going radiation after it has entered into the Earth’s atmosphere. The long wave radiation is absorbed by the atmosphere resulting in energy becoming thermal.
What are the major factors influencing distribution of temperature?
Factors Controlling Temperature Distribution The latitude of the Place. The altitude of the Place. Distance From The Sea. The presence of warm and cold ocean Currents.