The atmosphere operates as a global system transferring heat and energy, focusing on the features of global atmospheric circulation and the role of circula
Topic Synopsis
The atmosphere operates as a global system transferring heat and energy, focusing on the features of global atmospheric circulation and the role of circulation cells and ocean currents in redistributing heat energy across the Earth.
Key Concepts & Core Principles
- Global atmospheric circulation: The three-cell model (Hadley, Ferrel, Polar) that redistributes heat from the equator to the poles.
- Pressure belts: High and low pressure zones (e.g., ITCZ, subtropical highs) that drive wind patterns and precipitation.
- Coriolis effect: The deflection of winds due to Earth's rotation, creating prevailing winds like trade winds and westerlies.
- Energy transfer: Latent heat from evaporation and condensation, and sensible heat through convection and advection.
- Ocean currents: Surface currents driven by winds (e.g., Gulf Stream) that transport warm/cold water, affecting coastal climates.
Examiner Marking Points
- Features of global atmospheric circulation
- Role of circulation cells in heat transfer
- Role of ocean currents in heat transfer