Table 1 in New insight in the determination of thermodynamic equilibrium thickness using heat budget over Barents Sea

Table 1 — Validation of atmospheric variables with their R, biases and RMSE VariableRetrieved fromValidation with *RBiasRMSETemperature (K)ERA-5N-ICE2015 (ref. 30)0.96+3.405.30DAMOCLES (ref. 31)0.74+0.512.61Specific humidity (kg kg- 1)N-ICE 2015 (ref. 30)0.980.000.50DAMOCLES (ref. 31)0.56+0.400.75V-wind (ms- 1)N-ICE 2015 (ref. 30)0.92+0.401.40DAMOCLES (ref. 31)0.71+0.431.80Pressure (hPa)RAOBCORE (ref. 32)N. A+1.66N. ANet radiation at the top of the atmosphere (Wm- 2)CERES and CAVE (ref. 33)0.94-18.5226.95Net heat flux at the Earth’s surface (Wm- 2)N-ICE 2015 (ref. 30)0.32-14.0032.00Top net thermal radiation (Wm- 2)MERRA – 2 (ref. 34)0.70+5.00N. ATop net solar radiation (Wm- 2)NIBIO - CMP11 or CMP13 pyranometers (ref. 35)0.99+4.1010.20Ocean heat content (J)NOAAIn-situ observation (2006 - 2015) (ref. 36)N. A±0.100.61CERES EBAF EEI (ref. 37)0.44N. A0.40 *N-ICE2015 - Norwegian Young Sea-ice cruise, DAMOCLES - Developing Arctic Modeling and Observing Capabilities for Long-term Environmental Studies, RAOBCORE - RAdiosone OBservation COrrection using Reanalyses, CERES - Clouds and the Earth’s Radiant Energy System, CAVE - CERES ARM Validation Experiment, MERRA - Modern Era Retrospective-Analysis for Research and Applications, NIBIO - Norwegian Institute of Bioeconomy Research, CMP11 or CMP13 - Kyoto Protocol, EBAF - Energy Balanced and Filled, and EEI - Earth's energy imbalance