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.
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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.