Fig. 7: Cloud observations during the warm intrusion event.
From: A central arctic extreme aerosol event triggered by a warm air-mass intrusion
(A) Radar reflectivity showing the cloud base height, (B) Equivalent potential temperature showing the vertical temperature profile, (C) Liquid water path (D) Upwelling (blue) and downwelling (pink) longwave radiation and (E) the net longwave radiation. The unshaded area marks the warm air mass intrusion, the focus of this study.
