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Map of the Pacific Ocean during European Exploration, circa 1702–1707. ... Surface water temperatures in the Pacific can vary from −1.4 °C (29.5 °F), ...
Sea surface temperature since 1979 in the extrapolar region (between 60 degrees south and 60 degrees north latitude). [9] Sea surface temperature (or ocean surface temperature) is the temperature of ocean water close to the surface.
As a result, ocean surf temperatures are much colder in summer long the Pacific coast than the Atlantic coast at the same latitude. For example, the average July SST ( sea surface temperature ) at New York City at 40.7°N is 73 °F (23 °C), while at the same latitude in Eureka, CA is 57 °F (14 °C).
Global map of sea surface temperature, showing warmer areas around the equator and colder areas around the poles (20 December 2013 at 1-km resolution). Sea surface temperature (SST), or ocean surface temperature, is the water temperature close to the ocean's surface.
The temperature of the water in the gulf generally experiences lows of 16 °C (61 °F) in winter and highs of 24 °C (75 °F) in summer. But temperatures can vary greatly in the gulf, and the water is almost always warmer by the coast than the open ocean.
El Niño is strictly related to water temperatures near the equator in the eastern Pacific Ocean. In April, NOAA issued an El Niño watch, saying there is a 62% chance of the phenomenon developing ...
Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found. An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with ...
The temperature range of the sinking North Pacific Subtropical Mode Waters characteristically falls between 16 °C and 19 °C, however exact temperatures and depths to which these waters sink varies annually depending on the efficiency of water transportation by the extension, which is a function of atmospheric and mesoscale eddy conditions. [56]