1 / 30

Climates

Climates. What is Climate. Climate is an average of weather conditions in a region over a long-term period of time. Weather is the short-term condition of the atmosphere over a region. Global Climate.

wlinda
Télécharger la présentation

Climates

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Climates

  2. What is Climate Climate is an averageof weather conditions in a region over a long-term period of time. Weather is the short-termcondition of the atmosphere over a region.

  3. Global Climate Global climate is determined by the interaction of solar energy with the Earth’s surface and atmosphere: - by conditions of temperature and humidity. Climate is important is determining: habitability land use Effect of climate is the availability of water at the surface and within the ground.

  4. The Water Cycle and Climate • The water cycle involves the transfer of moisture between the land and sea, and between different latitudes. • Since climate is determined by the amount of moisture and the potential for evapotranspiration, climate is tied to the water cycle.

  5. The Earth’s Water CycleIs a Closed System

  6. Latitude Affects Moisture Exchange • Some latitudes have a surplus of precipitation over evaporation, other latitudes have a precipitation deficit. • 3 main belts of surplus are: • the equatorial zone 0o to 10o North and South • mid-latitude zones 40o to 70o in each hemisphere • 2 main belts of deficit are: • ~10o to 40o in each hemisphere

  7. Insolation INcomingSOLar radiATION Insolationis the term that refers to the amount of radiation from the Sun that is received by the Earth. Intensity of insolation is the rate at which solar energy is received by a given area of the Earth’s surface per unit of time.

  8. Intensity and Area Intensity of insolation is inverselyrelatedto the area of the Earth’s surface receiving it. As area gets bigger, intensity gets lower.

  9. Intensity vs Area

  10. Factors Affecting Insolation • Some of the many factors that affect insolation are: • Angle of insolation • Type of surface • Length of time insolation is received • Atmospheric conditions

  11. Angle of Insolation The angle which the Sun’s rays strike the surface is called the angle of insolation. The angle can be from 0o to 90o. Rays at a 90o angle are called direct, or vertical, rays. Areas receiving more direct rays will have higher temperatures.

  12. Angle of Insolation

  13. Time and Intensity • Angle of the Sun varies with time, so time will affect intensity. • At sunrise and sunset the angle of the Sun’s rays is the least and so the intensity is least. • At noon the Sun’s rays are at their greatest angle (most direct) and so the intensity of insolation is also the greatest.

  14. Time and Angle

  15. Earth’s Shape Affects Intensity of Insolation • Since the Earth is an oblate sphere, there is only one location that receives vertical rays from the sun. • The more you move away from the direct rays, the lower the angle of the rays and the lower the intensity.

  16. Intensity of Insolation Diagram

  17. Vertical Rays at Summer in Northern Hemisphere

  18. Seasons and Intensity of Insolation • Intensity of isolation varies with the seasons of the year. • Seasonsare caused by the tilt of the Earth’s axis and the revolution around the Sun.

  19. Seasons of the Earth

  20. Latitude and Intensity of Insolation • At noon on the date of the equinoxes, the sun is directly over the equator. • At this time the angle of the sun is the same as the observers latitude.

  21. Seasonal Angles of the Sun

  22. Duration of Insolation • The duration of insolation is the number of daylight hours at a given location. • Daylight hours vary with latitude and time of year. • There is a direct correlation between angle and intensity of insolation and duration of insolation. • Ex. Jun. 21 in Northern Hemisphere when angle and intensity are greatest, duration is longest.

  23. Length of Day / Duration

  24. Radiative Balance • Radiative balance exists when a substance gains the same amount of radiation as it gives off. • The Earth continuously receives insolation and radiates infrared energy from its surface.

  25. Maximum and Minimum Temperatures • Maximum radiative energy reaches the Earth when the angle and intensity of insolation are the greatest. • On a daily basis this is at solar noon (when the Sun’s rays are most direct). • Highest temperatures are after this time. • Earth begins to receive more energy than it gives off (reradiates). • Highest temperatures occur mid-afternoon. • Lowest temperatures occur just after sunrise.

  26. Time of Year • In the Northern Hemisphere the hottest time of year is afterJune 21 (greatest angle and duration of insolation). • Hottest time of year is in August when the amounts of incoming and outgoing energy are in radiative balance. • Coldest time of year is afterDec 21 (least angle and duration) occuring in February.

  27. Duration and Temperature Temperature at the surface is directly related to duration of insolation. The longer the duration the higher the temperature Note: the shortest days also have the lowest angle.

More Related