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The 26 pages that link to Ocean heat content, each with the reason it gives.

• Climate changeRelated: The oceans absorb most of the excess heat trapped by human-caused warming.

• Sea level riseRelated: It tracks the heat uptake that drives much of seawater’s expansion.

• Marine heatwaveRelated: Changes in stored heat can sustain unusually warm surface conditions.

• Specific heat capacityRelated: The ocean’s large heat capacity lets it absorb substantial energy with modest temperature change.

• Heat capacityRelated: Water's large heat capacity lets the ocean store substantial climate-system energy.

• Global warmingRelated: Ocean uptake delays surface warming while recording the climate system’s accumulating heat.

• Earth's energy budgetBroader topic: The oceans absorb most of the excess energy when Earth gains heat.

• Sea surface temperatureRelated: SST samples the surface, while heat content reveals how much warmth lies beneath it.

• Sea-level changeCompared with: It is a measure of stored energy, not sea-surface height, though warming can raise sea level.

• Ocean stratificationRelated: Layering governs how surface heat is stored, redistributed, and mixed downward.

• ThermoclineRelated: Thermocline position influences how much heat is stored near the surface versus at depth.

• Climate variabilityRelated: The ocean stores and releases heat, helping sustain climate fluctuations across years and decades.

• Thermal inertiaRelated: The ocean’s large heat capacity gives it substantial inertia in climate change.

• Ocean heat transportRelated: Transport changes where heat is stored, while heat content measures the resulting inventory.

• StratificationRelated: Stratification affects how heat is distributed and stored below the surface.

• Ocean warmingBroader topic: It measures accumulated ocean warming more reliably than surface temperature alone.

• ArgoRelated: Argo observations reveal how much heat the upper ocean absorbs and stores.

• HaloclineRelated: A halocline can inhibit upward mixing of deep heat, affecting surface conditions and ice.

• Air–sea gas exchangeCompared with: Heat crosses the same broad boundary, but through distinct mechanisms rather than gas transfer.

• Tropical cyclogenesisRelated: Deep warm water supplies energy without cooling rapidly under storm-driven mixing.

• Physical oceanographyRelated: Tracking it reveals how the ocean absorbs and transports climate-system heat.

• Effects of climate changeRelated: Ocean heat drives expansion, affects marine ecosystems, and fuels some storms.

• Effects of climate change on oceansRelated: The ocean absorbs most of the excess heat trapped by human greenhouse gas emissions.

• Effects of climate change on small island countriesRelated: Ocean warming expands seawater and contributes to global sea-level rise around islands.

• History of climate change scienceRelated: Ocean measurements showed that much of the excess energy from warming enters the sea.

• Ocean temperatureRelated: It combines temperature measurements with depth to track the ocean’s accumulated warming.