Polynyas in a dynamic-thermodynamic sea-ice model

5Citations
Citations of this article
30Readers
Mendeley users who have this article in their library.

Abstract

The representation of polynyas in viscous-plastic dynamic-thermodynamic sea-ice models is studied in a simplified test domain, in order to give recommendations about parametrisation choices. Bjornsson et al. (2001) validated their dynamic-thermodynamic model against a polynya flux model in a similar setup and we expand on that work here, testing more sea-ice rheologies and new-ice thickness formulations. The two additional rheologies tested give nearly identical results whereas the two new-ice thickness parametrisations tested give widely different results. Based on our results we argue for using the new-ice thickness parametrisation of Hibler (1979). We also implement a new parametrisation for the parameter h0 from Hibler's scheme, based on ideas from a collection depth parametrisation for flux polynya models. © Author(s) 2010.

Cite

CITATION STYLE

APA

Ólason, E. Ö., & Harms, I. (2010). Polynyas in a dynamic-thermodynamic sea-ice model. Cryosphere, 4(2), 147–160. https://doi.org/10.5194/tc-4-147-2010

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free