Atmospheric conditions during the Arctic Clouds in Summer Experiment (ACSE): Contrasting open-water and sea-ice surfaces during melt and freeze-up seasons

The Arctic Clouds in Summer Experiment (ACSE) was conducted during summer and early autumn 2014, providing a detailed view of the seasonal transition from ice melt into freeze-up. Measurements were taken over both ice-free and ice-covered surfaces near the ice edge, offering insight into the role of...

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Bibliographic Details
Published in:Journal of Climate
Main Authors: Sotiropoulou, G, Tjernström, M, Sedlar, J, Achtert, P, Brooks, BJ, Brooks, IM, Persson, POG, Prytherch, J, Salisbury, DJ, Shupe, MD, Johnston, PE, Wolfe, D
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2016
Subjects:
Arctic
ice pack
Sea ice
Online Access:https://eprints.whiterose.ac.uk/105170/
https://eprints.whiterose.ac.uk/105170/8/jcli-d-16-0211.1.pdf
https://doi.org/10.1175/JCLI-D-16-0211.1
Description
Summary:The Arctic Clouds in Summer Experiment (ACSE) was conducted during summer and early autumn 2014, providing a detailed view of the seasonal transition from ice melt into freeze-up. Measurements were taken over both ice-free and ice-covered surfaces near the ice edge, offering insight into the role of the surface state in shaping the atmospheric conditions. The initiation of the autumn freeze-up was related to a change in air mass, rather than to changes in solar radiation alone; the lower atmosphere cooled abruptly, leading to a surface heat loss. During melt season, strong surface inversions persisted over the ice, while elevated inversions were more frequent over open water. These differences disappeared during autumn freeze-up, when elevated inversions persisted over both ice-free and ice-covered conditions. These results are in contrast to previous studies that found a well-mixed boundary layer persisting in summer and an increased frequency of surface-based inversions in autumn, suggesting that knowledge derived from measurements taken within the pan-Arctic area and on the central ice pack does not necessarily apply closer to the ice edge. This study offers an insight into the atmospheric processes that occur during a crucial period of the year; understanding and accurately modeling these processes is essential for the improvement of ice-extent predictions and future Arctic climate projections.

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