|Title||Unique manifestations of mixed-phase cloud microphysics over Ross Island and the Ross Ice Shelf, Antarctica|
|Publication Type||Journal Article|
|Year of Publication||2016|
|Authors||Scott R.C, Lubin D.|
|Journal||Geophysical Research Letters|
|Type of Article||Article|
|Keywords||antarctica; Arctic; climate; Cloud microphysics; greenland; ice nucleation; McMurdo; north slope; nuclei; ocean; orographic; peninsula; precipitation; regimes; Ross Island; water; west antarctica|
Spaceborne radar and lidar observations from the CloudSat and CALIPSO satellites are used to compare seasonal variations in the microphysical and radiative properties of clouds over Ross Island, Antarctica, with two contrasting Arctic atmospheric observatories located in Barrow, Alaska, and Summit, Greenland. At Ross Island, downstream from recurrent intrusions of marine air over the West Antarctic Ice Sheet and eastern Ross Ice Shelf, clouds exhibit a tendency toward the greatest geometrical thickness and coldest temperatures in summer, the largest average ice water content, IWC, at low altitude during summer and autumn, the most abundant IWC at cold mixed-phase temperatures (-40 degrees C).