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:
Science Process Skills: Scientific Inquiry and Critical Thinking Skills
Making Observations and Asking Questions: Students will apply skills from previous grades and make measurements and observations about a variety of events and phenomena, including those that occur during very small and very large time frames.