claim: Surface temperatures can show short-term cooling when heat is exchanged between the atmosphere and the ocean, which has a much greater heat capacity than the air.
evidences.evidence_id: Convection:43
evidences.article: Convection
evidences.evidence: Longitudinal circulation, on the other hand, comes about because the ocean has a higher specific heat capacity than land (and also thermal conductivity, allowing the heat to penetrate further beneath the surface ) and thereby absorbs and releases more heat, but the temperature changes less than land.
evidences.votes: SUPPORTS SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Global warming:32
evidences.article: Global warming
evidences.evidence: This is due to the larger heat capacity of oceans and because oceans lose more heat by evaporation.
evidences.votes: REFUTES SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Global warming:94
evidences.article: Global warming
evidences.evidence: When soot is suspended in the atmosphere, it directly absorbs solar radiation, heating the atmosphere and cooling the surface.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO NOT_ENOUGH_INFO
evidences.evidence_id: Tropical cyclone:133
evidences.article: Tropical cyclone
evidences.evidence: This cooling is primarily caused by wind-driven mixing of cold water from deeper in the ocean with the warm surface waters.
evidences.votes: SUPPORTS SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Tropical cyclone:74
evidences.article: Tropical cyclone
evidences.evidence: latent heat) at the temperature of the warm ocean surface (during evaporation, the ocean cools and the air warms).
evidences.votes: SUPPORTS SUPPORTS NOT_ENOUGH_INFO