claim: Early estimates of ocean heat from the Argo showed a cooling bias due to pressure sensor issues.
evidences.evidence_id: Argo (oceanography):5
evidences.article: Argo (oceanography)
evidences.evidence: In most cases probes drift at a depth of 1000 metres (the so-called parking depth) and, every 10 days, by changing their buoyancy, dive to a depth of 2000 metres and then move to the sea-surface, measuring conductivity and temperature profiles as well as pressure.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS
evidences.evidence_id: Argo (oceanography):56
evidences.article: Argo (oceanography)
evidences.evidence: Such measurements are important for developing a comprehensive understanding of the ocean, such as trends in heat content.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS
evidences.evidence_id: Argo (oceanography):95
evidences.article: Argo (oceanography)
evidences.evidence: David Morrison reports that "[b]oth of these data sets show clear signatures of heat deposition in the ocean, from the temperature changes in the top 2 km of water and from the expansion of the ocean water due to heating.
evidences.votes: NOT_ENOUGH_INFO REFUTES
evidences.evidence_id: Ocean heat content:11
evidences.article: Ocean heat content
evidences.evidence: Ocean heat content can be estimated using temperature measurements obtained by a Nansen bottle, an ARGO float, or ocean acoustic tomography.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Shutdown of thermohaline circulation:58
evidences.article: Shutdown of thermohaline circulation
evidences.evidence: Based on coupled Atmosphere-Ocean General Circulation Models from 2001, the THC tends to weaken somewhat rather than stop, and the warming effects outweigh the cooling, even over Europe.
evidences.votes: NOT_ENOUGH_INFO REFUTES