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Булгаков, Н. П. Влияние перехода к голоцену на положение главного термоклина [] !Otitkn.pft: FILE NOT FOUND! !oizd.pft: FILE NOT FOUND! !ospec.pft: FILE NOT FOUND! !oistaspk_H.pft: FILE NOT FOUND! Рубрикатор НБУВ: Тематичні рубрики:
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Анотація: By numerical solution of the heat conduction equation, it is shown that the signal about a climate warming at the Holocene beginning would reach the depth 500 - 1 000 m till now without turbulent mixing. As a result, the temperature vertical distribution in the ocean is formed that is like to a real ocean thermocline. This effect affects stronger the temperature profile into the 1 km top layer of the Earth core. That is why the measurements of the thermal flux give data that are less by 30 % than the real geothermal flux. !oprip481_H.pft: FILE NOT FOUND! Дод. точки доступу: Дегтерев, А. Х.
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