The ocean smuggles some heat

Oceanographers have long known that the Atlantic and southern oceans are more efficient in storing heat than the Pacific Ocean. In contrast, the north of Atlantic heat is part of the powerful current system of the Atlantic thermohaline circulation.
Through it arrives at the distant North Atlantic Ocean with dense, salty cold water. It will retain some of the heat it accumulates on the surface. Researchers have determined that the intensity of the multi-decadal fluctuations they see is driven by changes in the salinity of water. Freshwater is more active than the corresponding salty, so when the water is injected with new vitality, it will change into rainfall or snowfall patterns. These reasons are due to the melting of Arctic ice or the slowing down of the circulation.
Dr. Dong and Chen pointed out that in the middle of the 20th century, the slight cooling of the global average temperature just met the rapid phase of the Atlantic's thermohaline circulation. Their conclusions no longer emphasize the role of the area because he and his partners focus on testing rather than mixing in model or model measurements. Other studies have confirmed the important role of heat sinks in the Atlantic Ocean and the Southern Ocean. Researchers at the National Center for Atmospheric Research in Boulder, Colorado, pointed out that heat is being driven out of the ocean to a depth of 2,300 feet or less.
Despite this, Dr. Jobs's research team concluded that the Pacific has always been the center of the radiator's action, to a large extent due to the natural climate swing. At the time of the breach, it has been exacerbating the trade winds moving westward across the Pacific Ocean.

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