Arctic winter warming amplified by the thermal inversion and consequent low infrared cooling to space

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Surface radiation climatology for Ny-Ålesund, Svalbard (78.9° N), basic observations for trend detection (2015, background): “Another parameter potentially influencing the winter downward longwave radiation are thermal inversions in the vertical temperature profile (Bintanja et al. 2011) that are frequently observed in the planetary boundary layer above Ny-Ålesund.”
EC-Earth V2.2: description and validation of a new seamless earth system prediction model (2012, methodology): “planetary boundary layer is highlighted in a recent study by Bintanja et al. (2011) and in an extension of that study by Bintanja et al.”
Response of the large‐scale structure of the atmosphere to global warming (2015, background): “Winton, 2006; Screen and Simmonds, 2010; Bintanja et al., 2011). The spatial pattern of temperature increase is shown in Figure 3, which shows the ensemble mean surface temperature trend (in degrees per decade) from the 1% integrations as a function of latitude and longitude. That land warms more re”