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  • Author or Editor: D. Wylie x
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J. A. Curry
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M. D. King
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D. A. Randall
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A. G. Williams
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D. Wylie

An overview is given of the First ISCCP Regional Experiment Arctic Clouds Experiment that was conducted during April–July 1998. The principal goal of the field experiment was to gather the data needed to examine the impact of arctic clouds on the radiation exchange between the surface, atmosphere, and space, and to study how the surface influences the evolution of boundary layer clouds. The observations will be used to evaluate and improve climate model parameterizations of cloud and radiation processes, satellite remote sensing of cloud and surface characteristics, and understanding of cloud–radiation feedbacks in the Arctic. The experiment utilized four research aircraft that flew over surface-based observational sites in the Arctic Ocean and at Barrow, Alaska. This paper describes the programmatic and scientific objectives of the project, the experimental design (including research platforms and instrumentation), the conditions that were encountered during the field experiment, and some highlights of preliminary observations, modeling, and satellite remote sensing studies.

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Taneil Uttal
,
Judith A. Curry
,
Miles G. McPhee
,
Donald K. Perovich
,
Richard E. Moritz
,
James A. Maslanik
,
Peter S. Guest
,
Harry L. Stern
,
James A. Moore
,
Rene Turenne
,
Andreas Heiberg
,
Mark. C. Serreze
,
Donald P. Wylie
,
Ola G. Persson
,
Clayton A. Paulson
,
Christopher Halle
,
James H. Morison
,
Patricia A. Wheeler
,
Alexander Makshtas
,
Harold Welch
,
Matthew D. Shupe
,
Janet M. Intrieri
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Knut Stamnes
,
Ronald W. Lindsey
,
Robert Pinkel
,
W. Scott Pegau
,
Timothy P. Stanton
, and
Thomas C. Grenfeld

A summary is presented of the Surface Heat Budget of the Arctic Ocean (SHEBA) project, with a focus on the field experiment that was conducted from October 1997 to October 1998. The primary objective of the field work was to collect ocean, ice, and atmospheric datasets over a full annual cycle that could be used to understand the processes controlling surface heat exchanges—in particular, the ice–albedo feedback and cloud–radiation feedback. This information is being used to improve formulations of arctic ice–ocean–atmosphere processes in climate models and thereby improve simulations of present and future arctic climate. The experiment was deployed from an ice breaker that was frozen into the ice pack and allowed to drift for the duration of the experiment. This research platform allowed the use of an extensive suite of instruments that directly measured ocean, atmosphere, and ice properties from both the ship and the ice pack in the immediate vicinity of the ship. This summary describes the project goals, experimental design, instrumentation, and the resulting datasets. Examples of various data products available from the SHEBA project are presented.

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