claim: But as that upper layer warms up, the oxygen-rich waters are less likely to mix down into cooler layers of the ocean because the warm waters are less dense and do not sink as readily.
evidences.evidence_id: Anoxic event:88
evidences.article: Anoxic event
evidences.evidence: If the high latitude waters are below 5 °C (41 °F), they will be dense enough to sink; as they are cool, oxygen is highly soluble in their waters, and the deep ocean will be oxygenated.
evidences.votes: REFUTES SUPPORTS
evidences.evidence_id: Anoxic event:89
evidences.article: Anoxic event
evidences.evidence: If high latitude waters are warmer than 5 °C (41 °F), their density is too low for them to sink below the cooler deep waters.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Lake ecosystem:28
evidences.article: Lake ecosystem
evidences.evidence: As the season progresses, the warmer air temperatures heat the surface waters, making them less dense.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Marine habitats:49
evidences.article: Marine habitats
evidences.evidence: Water that is saltier or cooler will be denser, and will sink in relation to the surrounding water.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Sea:56
evidences.article: Sea
evidences.evidence: Warm surface currents cool as they move away from the tropics, and the water becomes denser and sinks.
evidences.votes: REFUTES SUPPORTS