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...
Main Authors: | , , , , , |
---|---|
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 |
id |
doaj-fb87d4865668489e9d24fa8d5acf5a79 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT akduvivier goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT pderepentigny goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT pderepentigny goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT mmholland goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT mwebster goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT jekay goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT jekay goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations AT dperovich goingwiththefloetrackingcesmlargeensembleseaiceinthearcticprovidescontextforshipbasedobservations |
_version_ |
1724840679725596672 |