File(s) under permanent embargo
Melting of Ice and Sea Ice into Seawater and Frazil Ice Formation
journal contribution
posted on 2023-05-18, 03:06 authored by McDougall, TJ, Barker, PM, Feistel, R, Benjamin Galton-FenziBenjamin Galton-FenziThe thermodynamic consequences of the melting of ice and sea ice into seawater are considered. The International Thermodynamic Equation Of Seawater—2010 (TEOS-10) is used to derive the changes in the Conservative Temperature and Absolute Salinity of seawater that occurs as a consequence of the melting of ice and sea ice into seawater. Also, a study of the thermodynamic relationships involved in the formation of frazil ice enables the calculation of the magnitudes of the Conservative Temperature and Absolute Salinity changes with pressure when frazil ice is present in a seawater parcel, assuming that the frazil ice crystals are sufficiently small that their relative vertical velocity can be ignored. The main results of this paper are the equations that describe the changes to these quantities when ice and seawater interact, and these equations can be evaluated using computer software that the authors have developed and is publicly available in the Gibbs SeaWater (GSW) Oceanographic Toolbox of TEOS-10.
History
Publication title
Journal of Physical OceanographyVolume
44Issue
7Pagination
1751-1775ISSN
0022-3670Department/School
Institute for Marine and Antarctic StudiesPublisher
Amer Meteorological SocPlace of publication
45 Beacon St, Boston, USA, Ma, 02108-3693Rights statement
Copyright 2014 American Meteorological SocietyRepository Status
- Restricted