sea_ice_temperature_expressed_as_heat_content

The quantity with standard name sea_ice_temperature_expressed_as_heat_content is calculated relative to the heat content of ice at zero degrees Celsius, which is assumed to have a heat content of zero Joules. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea ice multiplied by the temperature of the sea ice in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea ice the integral is assumed to be calculated over the full depth of the ice. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs.
  • List containing this term version: CF (56) CF (57) CF (58) CF (59) CF (60) CF (61) CF (62) CF (63) CF (64) CF (65) CF (66) CF (67) CF (68) CF (69) CF (70) CF (71) CF (72) CF (73) CF (74) CF (75) CF (76) CF (77) CF (78) CF (79) CF (80) CF (81) CF (82) CF (83) CF (84) CF (85) CF (86)
  • Proposls with this term version:
  • Proposal: Martin Juckes [tendency_of_sea_water_conservative_tempe]

  • Aliases for this term

    integral_of_sea_ice_temperature_wrt_depth_expressed_as_heat_content

    "Content" indicates a quantity per unit area. Depth is the vertical distance below the surface. The quantity with standard name integral_of_sea_ice_temperature_wrt_depth_expressed_as_heat_content is calculated relative to the heat content of ice at zero degrees Celsius, which is assumed to have a heat content of zero Joules. "integral_of_Y_wrt_X" means int Y dX. The data variable should have an axis for X specifying the limits of the integral as bounds. "wrt" means with respect to.
  • List containing this term version: CF (16) CF (17) CF (18) CF (19) CF (20) CF (21) CF (25) CF (22) CF (27) CF (23) CF (24) CF (26) CF (28) CF (29) CF (30) CF (31) CF (32) CF (33) CF (34) CF (35) CF (36) CF (37) CF (38) CF (39) CF (40) CF (41) CF (42) CF (43) CF (44) CF (45) CF (46) CF (47)
  • Proposls with this term version:
  • Proposal: Jonathan Gregory / Stephen Griffies / Alison Pamment [New standard names for OMIP: physics]

  • This term is alaised by

    sea_ice_temperature_expressed_as_heat_content

    The quantity with standard name integral_wrt_depth_of_sea_ice_temperature_expressed_as_heat_content is calculated relative to the heat content of ice at zero degrees Celsius, which is assumed to have a heat content of zero Joules.
  • List containing this term version:
  • Proposls with this term version:
  • Proposal: Martin Juckes [tendency_of_sea_water_conservative_tempe]
  • sea_ice_temperature_expressed_as_heat_content

    The quantity with standard name integral_wrt_depth_of_sea_ice_temperature_expressed_as_heat_content is calculated relative to the heat content of ice at zero degrees Celsius, which is assumed to have a heat content of zero Joules. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs.
  • List containing this term version:
  • Proposls with this term version:
  • Proposal: Martin Juckes [tendency_of_sea_water_conservative_tempe]
  • sea_ice_temperature_expressed_as_heat_content

    The quantity with standard name sea_ice_temperature_expressed_as_heat_content is calculated relative to the heat content of ice at zero degrees Celsius, which is assumed to have a heat content of zero Joules. The phrase "expressed_as_heat_content" means that this quantity is calculated as the specific heat capacity times density of sea ice multiplied by the temperature of the sea ice in the grid cell and integrated over depth. If used for a layer heat content, coordinate bounds should be used to define the extent of the layers. If no coordinate bounds are specified, it is assumed that the integral is calculated over the entire vertical extent of the medium, e.g, if the medium is sea ice the integral is assumed to be calculated over the full depth of the ice. "Sea ice" means all ice floating in the sea which has formed from freezing sea water, rather than by other processes such as calving of land ice to form icebergs.
  • List containing this term version: CF (56) CF (57) CF (58) CF (59) CF (60) CF (61) CF (62) CF (63) CF (64) CF (65) CF (66) CF (67) CF (68) CF (69) CF (70) CF (71) CF (72) CF (73) CF (74) CF (75) CF (76) CF (77) CF (78) CF (79) CF (80) CF (81) CF (82) CF (83) CF (84) CF (85) CF (86)
  • Proposls with this term version:
  • Proposal: Martin Juckes [tendency_of_sea_water_conservative_tempe]