claim: We now know that the planetary energy balance is determined by the upper levels of the troposphere and that the saturation of the absorption at the central frequency does not preclude the possibility to absorb more energy.
evidences.evidence_id: Carbon dioxide:191
evidences.article: Carbon dioxide
evidences.evidence: Less energy reaches the upper atmosphere, which is therefore cooler because of this absorption.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO NOT_ENOUGH_INFO
evidences.evidence_id: Heat transfer:223
evidences.article: Heat transfer
evidences.evidence: In the case of the Earth-atmosphere system, it refers to the process by which long-wave (infrared) radiation is emitted to balance the absorption of short-wave (visible) energy from the Sun.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Ionosphere:64
evidences.article: Ionosphere
evidences.evidence: This is the main reason for absorption of HF radio waves, particularly at 10 MHz and below, with progressively less absorption at higher frequencies.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS NOT_ENOUGH_INFO
evidences.evidence_id: Troposphere:25
evidences.article: Troposphere
evidences.evidence: The reason for this temperature difference is that the ground absorbs most of the sun's energy, which then heats the lower levels of the atmosphere with which it is in contact.
evidences.votes: NOT_ENOUGH_INFO NOT_ENOUGH_INFO NOT_ENOUGH_INFO
evidences.evidence_id: Troposphere:74
evidences.article: Troposphere
evidences.evidence: Its fundamental principle is that of balance – the energy that the Earth absorbs from the sun each year is equal to that which it loses to space by radiation.
evidences.votes: NOT_ENOUGH_INFO SUPPORTS NOT_ENOUGH_INFO