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The Frying Pan Tower™ rises 135' above the Atlantic Ocean is being restored by volunteers through FPTower Inc., a 501(c)3 nonprofit whose mission is to help provide safety to mariners and the local sea life as well as providing an on-site facility for environmental research, and to live stream cameras of above and below the ocean. Several ...
Marine stratocumulus clouds are common in particular regions, specifically the eastern Pacific Ocean and the eastern South Atlantic Ocean. A typical finding among simulation studies was a persistent cooling of the Pacific, similar to the “La Niña” phenomenon, and, despite the localized nature of the albedo change, an increase in polar sea ice.
Live web cameras around the Myrtle Beach area allow people to watch the beach as Hurricane Ian approaches S.C.
National Geographic's Crittercam is a research tool designed to be worn by wild animals. It combines video and audio recording with collection of environmental data such as depth, temperature, and acceleration. [1] The live feeds help scientists experience an animal's daily routines.
Mist is a phenomenon caused by small droplets of water suspended in the cold air, usually by condensation. Physically, it is an example of a dispersion . It is most commonly seen where water vapor in warm, moist air meets sudden cooling, such as in exhaled air in the winter, or when throwing water onto the hot stove of a sauna .
NOAA video on hydrothermal vents Hydrothermal vents in the deep ocean typically form along the mid-ocean ridges , such as the East Pacific Rise and the Mid-Atlantic Ridge . These are locations where two tectonic plates are diverging and new crust is being formed.
By definition, fog reduces visibility to less than 1 km (0.62 mi), whereas mist causes lesser impairment of visibility. [4] For aviation purposes in the United Kingdom, a visibility of less than 5 km (3.1 mi) but greater than 999 m (3,278 ft) is considered to be mist if the relative humidity is 95% or greater; below 95%, haze is reported.
Computer models of ocean circulation increasingly place most of the deep upwelling in the Southern Ocean, associated with the strong winds in the open latitudes between South America and Antarctica. [28] Direct estimates of the strength of the thermohaline circulation have also been made at 26.5°N in the North Atlantic, by the UK-US RAPID ...