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Cocoa Beach Pier, built in 1962, extends into the Atlantic Ocean. According to the United States Census Bureau, the city has a total area of 15.0 square miles (39 km 2). 4.9 square miles (13 km 2) of it is land and 10.1 square miles (26 km 2) of it (67.49%) is water.
To the east the island is connected to Cape Canaveral by the Crawlerway, and by causeways to Cocoa Beach and Satellite Beach. According to the United States Census Bureau, the CDP has a total area of 122.2 km 2 (47.2 sq mi), of which 45.4 km 2 (17.5 sq mi) is land and 76.8 km 2 (29.7 sq mi), or 62.88%, is water. [21]
Fisheries are affected by climate change in many ways: marine aquatic ecosystems are being affected by rising ocean temperatures, [100] ocean acidification [101] and ocean deoxygenation, while freshwater ecosystems are being impacted by changes in water temperature, water flow, and fish habitat loss. [102]
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The increase of both ocean surface temperature and deeper ocean temperature is an important effect of climate change on oceans. [11] Deep ocean water is the name for cold, salty water found deep below the surface of Earth's oceans. Deep ocean water makes up about 90% of the volume of the oceans. Deep ocean water has a very uniform temperature ...
The WOA consists of a climatology of fields of in situ ocean properties for the World Ocean. It was first produced in 1994 [ 2 ] (based on the earlier Climatological Atlas of the World Ocean , 1982 [ 3 ] ), with later editions at roughly four year intervals in 1998, 2001, 2005, 2009, 2013, 2018, and 2023.
Surface temperatures in the western North Atlantic: Most of the North American landmass is black and dark blue (cold), while the Gulf Stream is red (warm). Source: NASA The Gulf Stream is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and flows through the Straits of Florida and up the eastern coastline of the United States, then veers east near 36°N latitude ...
The extent of the ocean surface down into the ocean is influenced by the amount of mixing that takes place between the surface water and the deeper water. This depends on the temperature: in the tropics the warm surface layer of about 100 m is quite stable and does not mix much with deeper water, while near the poles winter cooling and storms makes the surface layer denser and it mixes to ...
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