claim: Often the compensatory cooling, known as La Niña, is larger than the El Niño warming.”
evidences.evidence_id: El Niño:5
evidences.article: El Niño
evidences.evidence: The cool phase of ENSO is La Niña, with SSTs in the eastern Pacific below average, and air pressure high in the eastern Pacific and low in the western Pacific.
evidences.votes: REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: El Niño:96
evidences.article: El Niño
evidences.evidence: The exact opposite heating and atmospheric pressure anomalies occur during La Niña.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: El Niño–Southern Oscillation:1
evidences.article: El Niño–Southern Oscillation
evidences.evidence: The warming phase of the sea temperature is known as El Niño and the cooling phase as La Niña.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: La Niña:0
evidences.article: La Niña
evidences.evidence: La Niña (/lɑːˈniːnjə/, Spanish pronunciation: [la ˈniɲa]) is a coupled ocean-atmosphere phenomenon that is the colder counterpart of El Niño, as part of the broader El Niño–Southern Oscillation climate pattern.
evidences.votes: SUPPORTS NOT_ENOUGH_INFO
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