claim: The long term trend from albedo is of cooling.
evidences.evidence_id: Albedo:114
evidences.article: Albedo
evidences.evidence: The scattering of radiation causes atmospheric cooling, whereas absorption can cause atmospheric warming.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Albedo:53
evidences.article: Albedo
evidences.evidence: [citation needed] Arctic regions notably release more heat back into space than what they absorb, effectively cooling the Earth.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Albedo:59
evidences.article: Albedo
evidences.evidence: A layer of snowfall increases local albedo, reflecting away sunlight, leading to local cooling.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Ice age:0
evidences.article: Ice age
evidences.evidence: An ice age is a long period of reduction in the temperature of the Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS
evidences.evidence_id: Little Ice Age:162
evidences.article: Little Ice Age
evidences.evidence: Orbital forcing from cycles in the earth's orbit around the sun has, for the past 2,000 years, caused a long-term northern hemisphere cooling trend that continued through the Middle Ages and the Little Ice Age.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO