Joint bivariate locally stationary Gaussian process mapping of two ocean pressure layers reduces global OHC anomaly uncertainties by up to 15% versus independent layer maps.
The Galerkin finite element method for elliptic problems
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Improved Global Ocean Heat Content Estimation by Modeling Vertical Spatio-Temporal Dependence
Joint bivariate locally stationary Gaussian process mapping of two ocean pressure layers reduces global OHC anomaly uncertainties by up to 15% versus independent layer maps.