claim: Most of the atmospheric moisture originates in the tropical ocean, and the difference between surface and upper atmospheric temperature determines how much of the moisture rises into the atmosphere.
evidences.evidence_id: Extratropical cyclone:40
evidences.article: Extratropical cyclone
evidences.evidence: The peak time of subtropical cyclogenesis (the midpoint of this transition) in the North Atlantic is in the months of September and October, when the difference between the temperature of the air aloft and the sea surface temperature is the greatest, leading to the greatest potential for instability.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS
evidences.evidence_id: Low-pressure area:75
evidences.article: Low-pressure area
evidences.evidence: Worldwide, tropical cyclone activity peaks in late summer, when the difference between temperatures aloft and sea surface temperatures is the greatest.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Monsoon of South Asia:57
evidences.article: Monsoon of South Asia
evidences.evidence: Consequently, the air above coastal lands heats up faster than the air above seas.
evidences.votes: REFUTES REFUTES
evidences.evidence_id: Water vapor:113
evidences.article: Water vapor
evidences.evidence: The upper temperature level is given by the soil or water surface of the earth, which absorbs the incoming sun radiation and warms up, evaporating water.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Water vapor:75
evidences.article: Water vapor
evidences.evidence: The increase in buoyancy can have a significant atmospheric impact, giving rise to powerful, moisture rich, upward air currents when the air temperature and sea temperature reaches 25 °C or above.
evidences.votes: SUPPORTS SUPPORTS