claim: Climate sensitivity can be calculated empirically by comparing past temperature change to natural forcings at the time.
evidences.evidence_id: Climate sensitivity:0
evidences.article: Climate sensitivity
evidences.evidence: Climate sensitivity is the globally averaged temperature change in response to changes in radiative forcing, which can occur, for instance, due to increased levels of carbon dioxide (CO 2).
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Climate sensitivity:109
evidences.article: Climate sensitivity
evidences.evidence: One way is to use estimates of global radiative forcing and temperature directly.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Climate sensitivity:41
evidences.article: Climate sensitivity
evidences.evidence: Ignoring these factors causes lower estimates of climate sensitivity when using radiative forcing and temperature records from the historical period.
evidences.votes: REFUTES SUPPORTS
evidences.evidence_id: Climate sensitivity:77
evidences.article: Climate sensitivity
evidences.evidence: Climate sensitivity can be estimated using observed temperature rise, observed ocean heat uptake, and modeled or observed radiative forcing.
evidences.votes: SUPPORTS SUPPORTS
evidences.evidence_id: Climate sensitivity:9
evidences.article: Climate sensitivity
evidences.evidence: Climate sensitivity is typically estimated in three ways; by using observations taken during the industrial age, by using temperature and other data from the Earth's past and by modelling the climate system in computers.
evidences.votes: SUPPORTS SUPPORTS