Why in News?
Recent studies have shown that tectonically driven changes in the ocean gateways had a considerable impact on the global overturning circulations.
Key Findings-
- Studies indicate that changes in ocean routes caused by tectonics, like the closing of the Central American Seaway, had a big effect on ocean circulation.
- Central American Seaway (CAS) is a body of water that once separated North America from South America,
- These changes may have led to the formation of two distinct water bodies-
- Northern component water in the North Atlantic Ocean.
- Antarctic Bottom Water (AABW) in the Southern Ocean.
- Therefore, it is also hypothesised that there would have been extensive changes in the Deep-Water Circulation (DWC) in the oceans across the world, impacting global climate and heat exchanges.
About Deep Water Circulation (DWC)-
- DWC refers to the movement of water in the deep ocean. It is driven by the density differences between water masses caused by variations in temperature and salinity.
- In the Earth’s polar regions ocean water gets very cold, forming sea ice. Thus, the surrounding seawater becomes saltier, because when sea ice forms, the salt is remained behind.
- As the seawater gets saltier, its density increases, and it begins to sink. Surface water is pulled in to replace the sinking water, which in turn finally becomes cold and salty enough to sink.
- This forms a circulation pattern that is known as the thermohaline circulation.
Significance-
- Heat Distribution- It supports to distribute heat around the globe, which helps to regulate the Earth’s temperature and keep different regions from becoming too hot or too cold.
- Maintaining Carbon Dioxide Levels- It plays a crucial role in controlling atmospheric carbon dioxide levels by helping to transport carbon from the surface to the deep ocean, where it can be stored for long periods of time.
- Shaping Ocean Currents- It is accountable for shaping the ocean’s currents and the circulation patterns of the world’s oceans.
- These currents in turn influence the marine ecosystem, weather patterns, and coastal regions.
- Maintaining Sea level- It also has an impact on sea level, as warm water is less dense than cold water, thus it can also affect sea level by redistributing heat and thermal expansion.
Deep-Water Circulations of the Indian Ocean-
- The Indian Ocean does not create its own deep water, it only gets it from other sources like the North Atlantic and Antarctic.
- The northern part of the Indian Ocean is situated far away from the areas where deep water is formed and ocean routes, making it a better place to study the impact of ocean circulation changes.
- Studies have been conducted in the Indian Ocean to understand past deepwater circulation using records from iron-manganese crusts and authigenic neodymium isotope composition of sediment cores.
- These records have some limitations-
- Iron-manganese crusts are found at deeper depths and are only bathed by Antarctic Bottom Water (AABW), so they can only give information about the history of AABW.
- Authigenic neodymium isotope records are only available from the Bay of Bengal part, but they are also not accurate as the Himalayan rivers that flow into the Bay bring in a lot of neodymium particulates which can intervene with the results.
- Though, recently Scientists have generated an authigenic neodymium isotope record from the Arabian Sea and reconstructed the DWC record of the Indian Ocean for the period from 11.3 million years ago (Miocene era) to 1.98 million years ago (Pleistocene era).