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The static MODAS climatology temperature and salinity fields are at the very least as top quality as similar fields with the Levitus climatology. On the other hand MODAS provides greater horizontal resolution in a few regions. Levitus is 1° globally even though MODAS is ½° in the open up ocean, ¼° in coastal locations, and ⅛° in the vicinity of land.
From the MODAS dynamic climatology, these regressions are immediate linear relationships in between surface area temperature and dynamic height Using the temperature at a specified depth. Synthetic temperature profiles extending to some maximum depth of 1500 m are computed from these regression associations.
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The dynamic climatology shops the interactions, attained from archives of historic temperature and salinity profiles, involving subsurface temperature with steric height anomaly and area temperature. Nonetheless, the typical application constructs artificial temperature profiles, using the saved regression associations, from noticed full SSH anomalies and SST. The SSH and SST values may be from an individual measurement or from interpolated fields. The modas SSH used in the derivation of your MODAS dynamic climatology is steric top anomaly that varies in the ocean as a consequence of deviations in temperature and salinity. Measurements of whole top relative to prescribed indicates, for example from altimeter measurements, have to be interpreted and modified to provide details suitable for use While using the MODAS regression.
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