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Evidence of strong ocean heating during glacial periods. Causes of ocean heating. Part 2.
2025-07-30

We have developed the model of World Ocean thermo-haline circulation which shows that Pleistocene glacial-interglacial cycles are connected with change in interior ocean temperature. During glaciations haline circulation dominated – warm and salty isotopically heavy water from Red sea filled the ocean interior, which led to strong freshening of ocean surface and its stratification. Additionally, interior ocean water was heated by geothermal heat flux and heat released at decomposition of organic rain. Due to increased temperature, density of water on the ocean floor declined and strong thermo circulation started. This resulted in new interglacial period. Ocean quickly released heat accumulated during the glaciation.

Ссылка для цитирования:

Зимов С. А., Зимов Н. С. 2025. Evidence of strong ocean heating during glacial periods. Causes of ocean heating. Part 2. PREPRINTS.RU. https://doi.org/10.24108/preprints-3113642

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