A new study has given insight to the idea that the oceans are taking up some of the excess heat.

Study co-author Braddock Linsley, a climate scientist at Columbia University's Lamont-Doherty Earth Observatory,s adi that they're experimenting by putting all this heat in the ocean without quite knowing how it's going to come back out and affect climate.
He said that it's not so much the magnitude of the change, but the rate of change.
Ocean heat is typically measured from buoys dispersed throughout the ocean, and with instruments lowered from ships, with reliable records at least in some places going back to the 1960s.
To look back farther in time, scientists have developed ways to analyze the chemistry of ancient marine life to reconstruct the climates in which they lived. In a 2003 expedition to Indonesia, the researchers collected cores of sediment from the seas where water from the Pacific flows into the Indian Ocean.
By measuring the levels of magnesium to calcium in the shells of Hyalinea balthica, a one-celled organism buried in those sediments, the researchers estimated the temperature of the middle-depth waters where H. Balthica lived, from about 1,500 to 3,000 feet down.
Over the last 60 years, water column temperatures, averaged from the surface to 2,200 feet, increased 0.18 degrees C, or .32 degrees F.
The study has been published in the journal Science.
Source-ANI
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