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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 ...
As a result, ocean surf temperatures are much colder along the Pacific coast than the Atlantic coast. 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). As such, ocean surf temperatures are rarely above 70 °F (21 °C) during ...
A wet-bulb temperature at 500 hPa in a tropical atmosphere of −13.2 °C (8.2 °F) is required to initiate convection if the water temperature is 26.5 °C (79.7 °F), and this temperature requirement increases or decreases proportionally by 1 °C in the sea surface temperature for each 1 °C change at 500 hpa.
Since the track of most hurricanes is well to the south of San Diego, and the cold California Current (normally sea temperatures are only in the upper 60's F off the CA coast) keeps ocean water significantly colder than in the Gulf of Mexico and western Atlantic (often sea temperatures over 82 F), tropical cyclones rarely impact San Diego. Most ...
A thermocline (also known as the thermal layer or the metalimnion in lakes) is a distinct layer based on temperature within a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) with a high gradient of distinct temperature differences associated with depth.
The water temperature is often a little colder than the average San Diego beach. While the beach has only a small dry sand area at high tide, during very low tides, tide pools are revealed at the cove. California sea lions can be found in the waters of the cove and hauling out, temporarily leaving the water to rest on its beaches, cliffs, and ...
The ocean skin temperature is defined as the temperature of the water at 20 μm depth. This means that the SST skin is very dependent on the heat flux from the ocean to the atmosphere. This results in diurnal warming of the sea surface, high temperatures occur during the day and low temperatures during the night (especially with clear skies and ...
Anomalies in sea surface temperature can be used to forecast the length and intensity of the June Gloom phenomenon in a given season. [2] Years with warmer ocean temperatures, referred to as El Niño, may result in fewer gray days in May and June. [6] Cooler ocean temperatures, associated with La Niña, usually foretell a more gray period.