claim: The first adjustment changed how the temperature of the ocean surface is calculated, by replacing satellite data with drifting buoys and temperatures in ships’ water intake.
evidences.evidence_id: Instrumental temperature record:62
evidences.article: Instrumental temperature record
evidences.evidence: The sea record consists of surface ships taking sea temperature measurements from engine inlets or buckets.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Sea level:39
evidences.article: Sea level
evidences.evidence: It varies globally in a range of ± 2 m. Historically, adjustments were made to sea-level measurements to take into account the effects of the 235 lunar month Metonic cycle and the 223-month eclipse cycle on the tides.
evidences.votes: REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: Sea surface temperature:21
evidences.article: Sea surface temperature
evidences.evidence: The first automated technique for determining SST was accomplished by measuring the temperature of water in the intake port of large ships, which was underway by 1963.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Weather buoy:29
evidences.article: Weather buoy
evidences.evidence: Both moored buoys and drifting buoys (drifting in the open ocean currents) are used.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Weather station:4
evidences.article: Weather station
evidences.evidence: Weather conditions out at sea are taken by ships and buoys, which measure slightly different meteorological quantities such as sea surface temperature (SST), wave height, and wave period.
evidences.votes: SUPPORTS SUPPORTS