claim: (2009) have demonstrated recently  – the upper troposphere (the only place where adding CO2 to the  atmosphere could make any difference to temperature) is considerably  drier than the models are tuned to expect."
evidences.evidence_id: Atmosphere of Jupiter:248
evidences.article: Atmosphere of Jupiter
evidences.evidence: In 2010, astronomers imaged the GRS in the far infrared (from 8.5 to 24 μm) with a spatial resolution higher than ever before and found that its central, reddest region is warmer than its surroundings by between 3–4 K. The warm airmass is located in the upper troposphere in the pressure range of 200–500 mbar.
evidences.votes: NOT_ENOUGH_INFO REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: Sea surface temperature:84
evidences.article: Sea surface temperature
evidences.evidence: At the 500 hPa level, the air temperature averages −7 °C (18 °F) within the tropics, but air in the tropics is normally dry at this height, giving the air room to wet-bulb, or cool as it moistens, to a more favorable temperature that can then support convection.
evidences.votes: NOT_ENOUGH_INFO REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: Troposphere:46
evidences.article: Troposphere
evidences.evidence: If the upper air is warmer than predicted by the adiabatic lapse rate ( d S / d z > 0 {\displaystyle dS/dz>0} ), then when a parcel of air rises and expands, it will arrive at the new height at a lower temperature than its surroundings.
evidences.votes: NOT_ENOUGH_INFO REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: Troposphere:48
evidences.article: Troposphere
evidences.evidence: If, on the contrary, the upper air is cooler than predicted by the adiabatic lapse rate, then when the air parcel rises to its new height it will have a higher temperature and a lower density than its surroundings, and will continue to accelerate upward.
evidences.votes: NOT_ENOUGH_INFO REFUTES NOT_ENOUGH_INFO
evidences.evidence_id: Uranus:162
evidences.article: Uranus
evidences.evidence: The temperatures in the coldest upper region of the troposphere (the tropopause) actually vary in the range between 49 and 57 K (−224 and −216 °C; −371 and −357 °F) depending on planetary latitude.
evidences.votes: NOT_ENOUGH_INFO REFUTES NOT_ENOUGH_INFO