Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations

<p>In recent decades, Arctic sea ice has shifted toward a younger, thinner, seasonal ice regime. Studying and understanding this “new” Arctic will be the focus of a year-long ship campaign beginning in autumn 2019. Lagrangian tracking of sea ice floes in the Community Earth System Model Large...

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Main Authors: A. K. DuVivier, P. DeRepentigny, M. M. Holland, M. Webster, J. E. Kay, D. Perovich
Format: Article
Language:English
Published: Copernicus Publications 2020-04-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/14/1259/2020/tc-14-1259-2020.pdf
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spelling doaj-fb87d4865668489e9d24fa8d5acf5a792020-11-25T02:27:49ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242020-04-01141259127110.5194/tc-14-1259-2020Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observationsA. K. DuVivier0P. DeRepentigny1P. DeRepentigny2M. M. Holland3M. Webster4J. E. Kay5J. E. Kay6D. Perovich7National Center for Atmospheric Research, Boulder, CO, USADepartment of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO, USAInstitute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USANational Center for Atmospheric Research, Boulder, CO, USAGeophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USADepartment of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO, USACooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USAThayer School of Engineering, Dartmouth College, Hanover, NH, USA<p>In recent decades, Arctic sea ice has shifted toward a younger, thinner, seasonal ice regime. Studying and understanding this “new” Arctic will be the focus of a year-long ship campaign beginning in autumn 2019. Lagrangian tracking of sea ice floes in the Community Earth System Model Large Ensemble (CESM-LE) during representative “perennial” and “seasonal” time periods allows for understanding of the conditions that a floe could experience throughout the calendar year. These model tracks, put into context a single year of observations, provide guidance on how observations can optimally shape model development, and how climate models could be used in future campaign planning. The modeled floe tracks show a range of possible trajectories, though a Transpolar Drift trajectory is most likely. There is also a small but emerging possibility of high-risk tracks, including possible melt of the floe before the end of a calendar year. We find that a Lagrangian approach is essential in order to correctly compare the seasonal cycle of sea ice conditions between point-based observations and a model. Because of high variability in the melt season sea ice conditions, we recommend in situ sampling over a large range of ice conditions for a more complete understanding of how ice type and surface conditions affect the observed processes. We find that sea ice predictability emerges rapidly during the autumn freeze-up and anticipate that process-based observations during this period may help elucidate the processes leading to this change in predictability.</p>https://www.the-cryosphere.net/14/1259/2020/tc-14-1259-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. K. DuVivier
P. DeRepentigny
P. DeRepentigny
M. M. Holland
M. Webster
J. E. Kay
J. E. Kay
D. Perovich
spellingShingle A. K. DuVivier
P. DeRepentigny
P. DeRepentigny
M. M. Holland
M. Webster
J. E. Kay
J. E. Kay
D. Perovich
Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
The Cryosphere
author_facet A. K. DuVivier
P. DeRepentigny
P. DeRepentigny
M. M. Holland
M. Webster
J. E. Kay
J. E. Kay
D. Perovich
author_sort A. K. DuVivier
title Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
title_short Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
title_full Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
title_fullStr Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
title_full_unstemmed Going with the floe: tracking CESM Large Ensemble sea ice in the Arctic provides context for ship-based observations
title_sort going with the floe: tracking cesm large ensemble sea ice in the arctic provides context for ship-based observations
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2020-04-01
description <p>In recent decades, Arctic sea ice has shifted toward a younger, thinner, seasonal ice regime. Studying and understanding this “new” Arctic will be the focus of a year-long ship campaign beginning in autumn 2019. Lagrangian tracking of sea ice floes in the Community Earth System Model Large Ensemble (CESM-LE) during representative “perennial” and “seasonal” time periods allows for understanding of the conditions that a floe could experience throughout the calendar year. These model tracks, put into context a single year of observations, provide guidance on how observations can optimally shape model development, and how climate models could be used in future campaign planning. The modeled floe tracks show a range of possible trajectories, though a Transpolar Drift trajectory is most likely. There is also a small but emerging possibility of high-risk tracks, including possible melt of the floe before the end of a calendar year. We find that a Lagrangian approach is essential in order to correctly compare the seasonal cycle of sea ice conditions between point-based observations and a model. Because of high variability in the melt season sea ice conditions, we recommend in situ sampling over a large range of ice conditions for a more complete understanding of how ice type and surface conditions affect the observed processes. We find that sea ice predictability emerges rapidly during the autumn freeze-up and anticipate that process-based observations during this period may help elucidate the processes leading to this change in predictability.</p>
url https://www.the-cryosphere.net/14/1259/2020/tc-14-1259-2020.pdf
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