Lecture Description
The circulation in the atmosphere is composed of three circulation cells in the northern and southern hemispheres. These cells are caused by the rotation of the Earth which creates the Coriolis force. The Coriolis force deflects northern hemisphere motion to the right and southern hemisphere motion to the left. The majority of large-scale motion in the atmosphere is in geostrophic balance, meaning the Coriolis force acting on the motion is balanced by a pressure gradient force. The rotation of cyclones and anticyclones in the northern and southern hemispheres is controlled by this geostrophic balance.
Course Index
- Introduction to Atmospheres
- Retaining an Atmosphere
- The Perfect Gas Law
- Vertical Structure of the Atmosphere; Residence Time
- Earth Systems Analysis (Tank Experiment)
- Greenhouse Effect, Habitability
- Hydrostatic Balance
- Horizontal Transport
- Water in the Atmosphere I
- Water in the Atmosphere II
- Clouds and Precipitation (Cloud Chamber Experiment)
- Circulation of the Atmosphere (Exam I review)
- Global Climate and the Coriolis Force
- Coriolis Force and Storms
- Convective Storms
- Frontal Cyclones
- Seasons and Climate
- Seasons and Climate Classification
- Ocean Bathymetry and Water Properties
- Ocean Bathymetry and Water Properties
- Ocean Water Density and Atmospheric Forcing
- Ocean Currents
- Ocean Currents and Productivity
- El Niño
- Ice in the Climate System
- Ice and Climate Change
- Isotope Evidence for Climate Change
- Global Warming
- Global Warming II
- Global Warming III
- Climate Sensitivity and Human Population
- The Two Ozone Problems
- The Ozone Layer
- Energy Resources, Renewable Energy
- Renewable Energy
- Review and Overview
- Lab - Quinnipiac River Field Trip
Course Description
This course explores the physical processes that control Earth's atmosphere, ocean, and climate. Quantitative methods for constructing mass and energy budgets. Topics include clouds, rain, severe storms, regional climate, the ozone layer, air pollution, ocean currents and productivity, the seasons, El Niño, the history of Earth's climate, global warming, energy, and water resources.