Processing Steps |
- Data Type: cloud_area_fraction (measured); Units: dimensionless; Observation Type: in situ; Sampling Instrument: human eye; Sampling and Analyzing Method: The "cloud_area_fraction" was reported once per hour by surface observers. Those values were linearly interpolated to the one-minute resolution of the observed surface data before being used to estimate longwave radiation. The one-minute values were averaged to one-hour resolution for this data set.; Data Quality Information:
- Data Type: downwelling_longwave_flux_in_air_assuming_clear_sky (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: Calculated by the RRTMv3.3 algorithm, described in Mlawer et al. (1997, 10.1029/97JD00237), from atmospheric soundings collected during the cruise and profiles of the 7 most significant radiatively active gases: H2O, CO2, O3, N2O, CO, CH4 and O2. H2O came from the same radiosonde profile as the temperature. Surface CO2 was set to 398.4 ppm and distributed using a constant mixing ratio at all heights. Other gas profiles were taken from the US Standard Atmosphere tropical profile. The reported value is referenced to 3.8 m ASL.; Data Quality Information:
- Data Type: downwelling_longwave_flux_in_air (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: Calculated from "downwelling_longwave_flux_in_air_assuming_clear_sky" and an estimate of the longwave cloud radiative effect with a hypothetical optically thick cloud at 1 km ASL that was scaled by cloud_area_fraction. We used RRTMv3.3 coupled with the DISORT algorithm, described in Stamnes et al. (1988, doi:10.1364/AO.27.002502), and considered absorption but not scattering. The reported value is referenced to 3.8 m ASL.; Data Quality Information:
- Data Type: surface_upwelling_longwave_flux_in_air (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: Calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1), assuming a surface emissivity of 0.97. The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: downwelling_shortwave_flux_in_air (measured); Units: W/m^2; Observation Type: in situ; Sampling Instrument: IMET Eppley PSP; Sampling and Analyzing Method: Downwelling shortwave radiation was measured at 11.2 m ASL, logged at 1 Hz, and averaged to 1 minute, then averaged to 1 hour for input to coare35vnWarm.; Data Quality Information:
- Data Type: surface_upwelling_shortwave_flux_in_air (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: Calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1), assuming a surface albedo of 0.945. The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: surface_upward_latent_heat_flux (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The bulk latent heat flux out of the ocean was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: surface_upward_sensible_heat_flux (calculated); Units: W/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The bulk sensible heat flux out of the ocean was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Bulk buoyancy flux into ocean (calculated); Units: m^2/s^3; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The bulk buoyancy flux into the ocean was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Friction velocity (calculated); Units: m/s; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The friction velocity, u*, which includes gustiness, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Wind stress (calculated); Units: N/m^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The wind stress, tau, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Temperature scaling parameter (calculated); Units: K; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The temperature scaling parameter, t*, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Specific humidity scaling parameter (calculated); Units: g/kg^2; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The specific humidity scaling parameter, q*, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Thermal roughness length (calculated); Units: m; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The thermal roughness length, z0t, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Moisture roughness length (calculated); Units: m; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The moisture roughness length, z0q, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Wind stress transfer coefficient at height=zu (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The drag coefficient, Cd, is valid at the height of the radiosonde ground station, zu = 3.8 m ASL. It was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Sensible heat transfer coefficient at height=zu (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The sensible heat transfer coefficient (Stanton number), Ch, is valid at the height of the radiosonde ground station, zu = 3.8 m ASL. It was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Latent heat transfer coefficient at height=zu (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The latent heat transfer coefficient (Dalton number), Ce, is valid at the height of the radiosonde ground station, zu = 3.8 m ASL. It was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Obukhov length scale (calculated); Units: m; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The Obukhov length scale, L, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Monin-Obukhov stability parameter (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The Monin-Obukhov stability parameter, zu/L, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: wind_speed at height=10m (calculated); Units: m/s; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The wind speed at height=10m, U10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: air_temperature at height=10m (calculated); Units: C; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The air temperature at height=10m, T10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: specific_humidity at height=10m (calculated); Units: g/kg; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The specific_humidity at height=10m, Q10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: relative_humidity at height=10m (calculated); Units: %; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The relative_humidity at height=10m, RH10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Neutral value of wind speed at height=zu (calculated); Units: m/s; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The wind speed at height=zu valid under conditions of neutral static stability, UN, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Neutral value of wind speed at height=10m (calculated); Units: m/s; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The wind speed at height=10m valid under conditions of neutral static stability, UN10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Neutral value of drag coefficient at height=10m (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The drag coefficient at height=10m valid under conditions of neutral static stability, CdN_10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Neutral value of Stanton number at height=10m (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The Stanton number at height=10m valid under conditions of neutral static stability, ChN_10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Neutral value of Dalton number at height=10m (calculated); Units: dimensionless; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The Dalton number at height=10m valid under conditions of neutral static stability, CeN_10, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: sea_surface_temperature (calculated); Units: C; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The SST was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Cool-skin temperature depression (calculated); Units: C; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The cool-skin temperature depression, dter, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Surface saturation specific humidity (calculated); Units: g/kg; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The surface saturation specific humidity, Qs, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Latent heat of vaporization (calculated); Units: J/kg; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The latent heat of vaporization, Le, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
- Data Type: Evaporation rate (calculated); Units: mm/hour; Observation Type: model output; Sampling Instrument: Not applicable; Sampling and Analyzing Method: The evaporation rate, Evap, was calculated by the "coare35vnWarm" version of the COARE flux algorithm, described in Edson et al. (2013, doi:10.1175/jpo-d-12-0173.1). The following measured quantities were used as input to coare35vnWarm: time, pressure, air temperature, wind, bulk ocean temperature, and solar radiation. Estimated longwave radiation was also used as input. The input winds were valid at the height of the radiosonde ground station, zu = 3.8 m ASL. We had a bulk ocean temperature rather than a true ocean skin temperature, so coare35vnWarm did a cool-skin calculation to get SST.; Data Quality Information:
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