Figure 3
From: Vertical Feedback Mechanism of Winter Arctic Amplification and Sea Ice Loss
Winter average pattern of sea ice loss mode in the Barents and Kara Seas: (a) sea ice reduction (%, shading), 2 m air temperature (red contour) and 850 hPa temperature (black contour), (b) upward longwave radiation (red contour) and downward longwave radiation (black contour), (c) sensible heat flux (red contour) and latent heat flux (black contour), and (d) net energy balance (sensible heat flux + latent heat flux + upward longwave radiation – downward longwave radiation). Figures were created with GrADS 2.1.0 (http://cola.gmu.edu/grads/).
