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Efforts to involve sea surface temperature in model initialization began in 1972 due to its role in modulating weather in higher latitudes of the Pacific.
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One such variation is the Pacific Decadal Oscillation (PDO), also referred to as the Pacific Decadal Variability (PDV), which involves changing sea surface temperatures (SSTs) in the North Pacific Ocean.
El Niño is a weather phenomenon that involves warming sea-surface temperatures and a change in wind that alters weather patterns in the atmosphere worldwide.
Here, we show that photosensitized reactions involving the sea-surface microlayer lead to the production of significant amounts of isoprene.
Solving these modeling problems will help clarify the mechanism involved in typhoon-induced sea surface cooling.
In situ observations underneath a TC are, therefore, needed to allow the mechanisms involved in TC-induced sea surface cooling to be determined.
It can be seen that the mechanisms involved in TC-induced sea surface cooling are complex and depend on various factors, such as the TC intensity, translation speed, and size, and on pre-existing oceanic conditions such as the depth of the mixed layer and the temperature gradient within the underlying seasonal thermocline.
Deployment involved releasing the OBS on the sea surface and allowing it to sink freely to the seafloor.
Investigation of the World Ocean processes involves the determination of space-time changes of sea surface temperature (SST).
In this paper we described the problems involved in the automatic detection of small floating targets on the sea surface, and this in the context of the detection of drifting mines.
Another difference between tsunamis and wind-driven storm waves is that the entire column of water from the sea surface to the sea floor, perhaps several kilometres high, is involved in the wave motion.
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