1 / 9

Understanding Earth's Energy Budget and Its Impact on Climate Dynamics

This article explores the intricacies of Earth's energy budget, highlighting the role of albedo, surface cover, and insolation in seasonal and geographical variations. It examines how high albedo surfaces like snow and ice affect energy absorption, the influences of aerosols, and the unequal distribution of solar radiation due to Earth's axial tilt. The latitudinal energy gradient is also discussed, along with convection cells and their role in regulating climate. Additionally, the article delves into wind patterns, the Coriolis effect, and the significance of ocean temperature in shaping atmospheric dynamics.

zarifa
Télécharger la présentation

Understanding Earth's Energy Budget and Its Impact on Climate Dynamics

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. Energy Budget

  2. Atmosphere: Energy budget Albedo varies with season and geography Surface cover that has a high albedo Snow & ice Cloud cover Aerosols

  3. Insolation is unequal in distribution

  4. Tilt of the earth’s axis Absorbed solar radiation is greater than OLR in the tropics and sub-tropics Middle to polar latitudes net cooling Latitudinal energy gradient drives atmosphere and ocean currents Earth’s tilt and seasons

  5. Convection Cells • Convection cells • Transfer energy • Regulate climate

  6. Wind patterns and Coriolis effect • Northern hemisphere objects in flight move to the right • Coriolis Effect in different hemispheres.

  7. Hurricanes are formed in areas of low pressure

  8. Ocean temperatures & Atmosphere

  9. Great Ocean Conveyor Belt • Salty water is more dense than fresh water • Cold water is more dense than warm water • As warm water loses heat, it begins to sink. • .

More Related