claim: Short term cooling over the last few years is largely due to a strong La Nina phase in the Pacific Ocean and a prolonged solar minimum.
evidences.evidence_id: El Niño:1
evidences.article: El Niño
evidences.evidence: The ENSO is the cycle of warm and cold sea surface temperature (SST) of the tropical central and eastern Pacific Ocean.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: El Niño–Southern Oscillation:0
evidences.article: El Niño–Southern Oscillation
evidences.evidence: El Niño–Southern Oscillation (ENSO) is an irregularly periodic variation in winds and sea surface temperatures over the tropical eastern Pacific Ocean, affecting the climate of much of the tropics and subtropics.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: El Niño–Southern Oscillation:51
evidences.article: El Niño–Southern Oscillation
evidences.evidence: An especially strong Walker circulation causes La Niña, resulting in cooler ocean temperatures in the central and eastern tropical Pacific Ocean due to increased upwelling.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO SUPPORTS SUPPORTS
evidences.evidence_id: La Niña:3
evidences.article: La Niña
evidences.evidence: During a period of La Niña, the sea surface temperature across the equatorial Eastern Central Pacific Ocean will be lower than normal by 3 to 5°C (5.4 to 9°F).
evidences.votes: SUPPORTS NOT_ENOUGH_INFO SUPPORTS SUPPORTS
evidences.evidence_id: La Niña:6
evidences.article: La Niña
evidences.evidence: La Niña is the positive and cold phase of the El Niño–Southern Oscillation, and is associated with cooler-than-average sea surface temperatures in the central and eastern tropical Pacific Ocean.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO SUPPORTS SUPPORTS