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Combining Argo data with other hydrographic data to generate climatologies and nowcasts of physical properties. C. Schmid NOAA/AOML. Topics. Data sets and methods. Mapping of the mixed layer properties. Deriving the heat storage rate. Deriving the oceanic heat transport.
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Combining Argo data with other hydrographic data to generate climatologies and nowcasts of physical properties C. Schmid NOAA/AOML
Topics • Data sets and methods. • Mapping of the mixed layer properties. • Deriving the heat storage rate. • Deriving the oceanic heat transport. • Deriving the heat budget.
Data sets • Hydrographic profiles from Argo and pre-Argo floats (various sources). • Hydrographic profiles from XBTs, CTDs (AOML & NODC). • Velocity from surface drifters (AOML). • Sea surface height from altimetry. • Scatterometer wind. • Reynolds SST. • SST from Remote Sensing Systems microwave TMI. • Surface fluxes from the NCEP reanalysis 1.
Processing of hydrographic data • Remove duplicate profiles. • Apply automatic QC to all profiles. • Combine data sets from different sources, sorted by space and time. • Derive mixed layer properties (T, S, h) using the temperature gradient (limit 0.05ºC/dbar). • Apply statistical QC to mixed layer properties.
QC procedures for profiles • Global range tests (e.g. temperature within range of –2.5 to 40ºC) • Spike, vertical gradient and density inversion tests. • Comparison with Levitus climatology and NCEP ocean reanalysis (GODAS). Rejection if profile outside of 10 standard deviations from both profiles.
QC procedures for mixed layer properties • Separate check of mixed layer thickness and temperature. • Derive median and standard deviation from all values obtained within one month in a box (latitude x longitude: 1.5º x 5º). • Reject values if they are outside of a 2 standard deviation envelop around the median for each month and box (use adjacent boxes if needed).
Heat budget equation for mixed layer where • Terms: • Heat storage rate • Horizontal Advection • entrainment (new) • total surface fluxes • penetrative short-wave radiation (neglect for now) • Diffusive flux at the base of the mixed layer is small • (not shown, neglect).
Deriving the heat storage rate (HSR) • Derive monthly averages of mixed layer properties and positions in each box. • Perform objective analysis with a grid resolution of 1o by 1o. • Interpolate time series over short gaps (< 4 months). • Smooth the time series with a 3-point running mean. • Derive the time derivative of the temperature and the heat storage rate.
Deriving horizontal heat transport • derive v∙T and v´∙ T´ from data set compiled by Rick • Mean velocities are from drifters. • Time variant velocities are from altimetry (geostrophic) and scatterometer winds (Ekman). • Mean temperature is from Reynolds SST. • Time variant temperature comes from Remote Sensing Systems microwave TMI. • Derive cph from monthly mean of mixed layer properties. • Integrate around region to get the transport.
Deriving entrainment of heat into mixed layer • Temperature (T) and velocity (v) fields were provided by Rick (the same data were used to derive the horizontal heat transport). • The mixed layer properties (, cp, h ) are derived from the hydrographic profiles. • Estimate mean for region to get the entrainment.
Foltz et al, 2003 TNA-SE
Foltz et al, 2003 TNA-SE
Foltz et al, 2003 TSA-NE3
Foltz et al, 2003 TSA-NE3