Continental Boundaries: The shape and location of continents play a significant role in determining the path of ocean currents. Large landmasses can deflect currents and create unique circulation patterns.
Ocean currents can be broadly classified into two main types: surface currents and deep currents.
Surface Currents: These currents are driven primarily by wind and are located in the top 400 meters of the ocean. They play a crucial role in distributing heat around the globe and can have a significant impact on regional climates.
Deep Currents: Also known as thermohaline currents, these currents are driven by differences in waterdensity, which are influenced by temperature and salinity. Deep currents can circulate water throughout the ocean basins, playing a key role in the global conveyer belt of oceancirculation.
By mastering these concepts, you will gain a comprehensive understanding of oceancirculation and its significance in the broader context of Earth's systems.
[Ocean Circulation] Related Worksheets and Study Guides:
Create a computational model to calculate the change in the energy of one component in a system when the change in energy of the other component(s) and energy flows in and out of the system are known.
Develop and use models to illustrate that energy at the macroscopic scale can be accounted for as either motions of particles or energy stored in fields.