Ice shelf response to the change in ocean temperature

O. V. Nagornov, O. V. Sergienko

Research output: Contribution to conferencePaperpeer-review

1 Scopus citations

Abstract

Ice Shelf response to Global Ocean temperature change is examined. The thermohaline circulation forced by the mass and energy exchange at the ice-ocean boundary is studied with a two-dimensional model. The melting/freezing rate has been estimated. Different boundary conditions are considered. Maximum melting rate is 2 m/y, it is reached at the grounding line. Accumulation of ice takes place at the ice shelf edge with rate on the order of 0.1 m/y. If the underlying water warm by 0.001 °C/y the melting rate would increase to 2.2 m/y and the freezing rate would change by 0.01 m/y. The dimension of the region with supercooled water has been estimated.

Original languageEnglish (US)
Pages281-295
Number of pages15
StatePublished - 1998
Externally publishedYes
EventProceedings of the 1998 7th International Conference on Development and Application of Computer Techniques to Environmental Studies, ENVIROSOFT VII - Las Vegas, NV, USA
Duration: Nov 10 1998Nov 12 1998

Conference

ConferenceProceedings of the 1998 7th International Conference on Development and Application of Computer Techniques to Environmental Studies, ENVIROSOFT VII
CityLas Vegas, NV, USA
Period11/10/9811/12/98

All Science Journal Classification (ASJC) codes

  • General Engineering

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