Arctic sea-ice evolution as modeled by Max Planck Institute for Meteorology’s Earth system model

Metadata Label Value
Author(s) Notz, Dirk, Haumann, F. Alexander, Haak, Helmuth, Jungclaus, Johann H., Marotzke, Jochem
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley Log in to provide feedback

Detailed Information

Metadata Field Content
Title Arctic sea-ice evolution as modeled by Max Planck Institute for Meteorology’s Earth system model
Author(s) Notz, Dirk
Haumann, F. Alexander
Haak, Helmuth
Jungclaus, Johann H.
Marotzke, Jochem
Journal or Series Title Journal of advances in modeling earth systems
Volume Number 5
Issue Number 2
Start Page 173
End Page 194
ISSN 1942-2466
Publisher Wiley
Publication Place S.l.
Publication Date 2013-06
Abstract We describe the evolution of Arctic sea ice as modeled by the Max Planck Institute for Meteorology's Earth System Model (MPI-ESM). The modeled spatial distribution and interannual variability of the sea-ice cover agree well with satellite observations and are improved relative to the model's predecessor ECHAM5/MPIOM. An evaluation of modeled sea-ice coverage based on sea-ice area gives, however, conflicting results compared to an evaluation based on sea-ice extent and is additionally hindered by uncertainties in the observational record. Simulated trends in sea-ice coverage for the satellite period range from more strongly negative than observed to positive. The observed evolution of Arctic sea ice is incompatible with modeled internal variability and probably caused by external forcing. Simulated drift patterns agree well with observations, but simulated drift speed is generally too high. Simulated sea-ice volume agrees well with volume estimates of the PIOMAS reanalysis for the past few years. However, a preceding Arctic wide decrease in sea-ice volume starts much earlier in MPI-ESM than in PIOMAS. Analyzing this behavior in MPI-ESM's ocean model MPIOM, we find that the modeled volume trend depends crucially on the specific choice of atmospheric reanalysis forcing, which casts some doubt on the reliability of estimates of volume trends. In our CMIP5 scenario simulations, we find a substantial delay in sea-ice response to increasing CO2 concentration; a seasonally ice-free Arctic can result for a CO2 concentration of around 500 ppm. Simulated winter sea-ice coverage drops rapidly to near ice-free conditions once the mean Arctic winter temperature exceeds −5°C.
DOI 10.1002/jame.20016
Additional Notes Received 27 July 2012, Revised 10 December 2012, Accepted 8 January 2013, Published online 18 April 2013
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 007616648
Source Database ID FORM-1384435261
SCOPUS-84880779380
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

@article{Ntz2013,
  author = "Notz, Dirk and Haumann, F. Alexander and Haak, Helmuth and Jungclaus, Johann H. and Marotzke, Jochem",
  title = "{A}rctic sea-ice evolution as modeled by {M}ax {P}lanck {I}nstitute for {M}eteorology{\textquoteright}s {E}arth system model",
  journal = "Journal of advances in modeling earth systems",
  year = 2013,
  volume = "5",
  number = "2",
  pages = "173--194",
  month = jun,
}


E-Citations record created: Thu, 14 Nov 2013, 13:21:30 CET