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Each Output variable record corresponds to a physical parameter specification.
Attribute | Value |
---|---|
branded_variable_name | sicompstren_tavg-u-hxy-si |
cell_measures | area: areacello |
cell_methods | amnsi-twm (Weighted Time Mean on Sea-Ice) |
cmip6_frequency | mon |
cmip6_tables_identifier | SImon (Monthly sea-ice data) |
cmip7_compound_name | seaIce.mon.sicompstren_tavg-u-hxy-si |
cmip7_frequency | mon |
description | Computed strength of the ice pack, defined as the energy (J m-2) dissipated per unit area removed from the ice pack under compression, and assumed proportional to the change in potential energy caused by ridging. For Hibler-type models, this is P = P\* h exp(-C(1-A)) where P\* is compressive strength, h is ice thickness, A is compactness and C is strength reduction constant. |
dimensions | longitude, latitude, time |
flag_-_variable_change_since_cmip6 | True |
modelling_realm | Sea Ice |
name | SImon.sicompstren |
physical_parameter | sicompstren (Compressive Sea Ice Strength) |
processing_note | Note that SIMIP requests the area-weighted average for all intensive variables (i.e., variables that are not proportional to area fraction such as albedo, temperature, or heat flux). Hence, all time samples with non-zero sea-ice fraction are first multiplied by area fraction, then summed, and then divided by the sum of the area fractions. See Appendix C of Notz et al. (2016) for more detail. CHANGE SINCE CMIP6 in Cell Methods - CMIP6:area: time: mean where sea_ice (comment: mask=siconc) CMIP7:area: time: mean where sea_ice (mask=siconc), |
provenance | SIMIP [seaicemon] |
spatial_shape | XY-na (Global field (single level)) |
temporal_shape | time-intv (Temporal Interval) |
title | Compressive Sea Ice Strength |
type | real |
uid | 71166880-faa7-11e6-bfb7-ac72891c3257 |