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Decadal-averaged months for all six decades at different depths in the NWARC were compared to each other, and it was found that on the 1/10[degrees] x 1/10[degrees] grid there are identifiable repetitive mesoscale patterns in all decadal climatologies for all months in the upper-1,000-m layer.
To test this hypothesis, we compared NWARC's monthly decadal near-surface temperature to sea surface temperature (SST) from the Coral Reef Temperature Anomaly Database version 5 (CoRTADv5).
Figure 4 shows October decadal temperature from NWARC at 10 m depth for 1985-94, 1995-2004, and 2005-12 (left panels) and decadal October SST assembled from CoRTADv5 (right panels).
(2016) compared the monthly observed high-resolution decadal climatologies from NWARC with the decadal climatologies compiled using the model output from the Nucleus for European Modeling of the Ocean (NEMO) eddyresolving model (Madec 2008; Molines et al.
NWARC salinity climatologies show similar transitions as temperature from coarse to eddy-permitting to eddy-resolving resolutions and likewise may be expected to be useful in climate simulations and satellite data validation.
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