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All temperature data collected from deep boreholes drilled throughout the World’s Ocean show strong heat flow decreases with depth (a minimum of 40 mW/m2). Sharp shifts in heat flow are seen within boreholes at depths crossing gas hydrate bottom. This means that during the last glacial bottom water temperature there was on 25-30 degrees of C warmer. Conversely, in isolated and shallow seas, heat flow in the sediments show little change with depth. This means that bottom temperatures were rather stable there. Taking into account all these, average heat flow through ocean crust does not exceed 35 mW/m2, that is 3 times less existing estimate.
Зимов С. А., Зимов Н. С. 2025. Evidence of strong ocean heating during glacial periods. Causes of ocean heating. Part 1. PREPRINTS.RU. https://doi.org/10.24108/preprints-3113646
