claim: The warm and cool regions roughly balance each other out with little impact on global temperature.
evidences.evidence_id: Global warming:106
evidences.article: Global warming
evidences.evidence: The main balancing feedback to global temperature change is radiative cooling to space as infrared radiation, which increases strongly with increasing temperature.
evidences.votes: REFUTES REFUTES
evidences.evidence_id: Global warming:172
evidences.article: Global warming
evidences.evidence: This could trigger cooling in the North Atlantic, Europe, and North America.
evidences.votes: NOT_ENOUGH_INFO REFUTES
evidences.evidence_id: Global warming:79
evidences.article: Global warming
evidences.evidence: Globally, these effects are estimated to have led to a slight cooling, dominated by an increase in surface albedo.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Global warming:81
evidences.article: Global warming
evidences.evidence: In the tropics the net effect is to produce a significant warming, while at latitudes closer to the poles a loss of albedo leads to an overall cooling effect.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Terraforming of Venus:138
evidences.article: Terraforming of Venus
evidences.evidence: This in turn would raise planetary albedo and act to cool the global temperature to Earth-like levels, despite the greater proximity to the Sun.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS