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The North Atlantic circulation derived from inverse models
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The North Atlantic circulation derived from inverse models
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Building a Scalable Ensemble Data Assimilation System for Coupled Models
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On estimating the circulation in the North Atlantic from altimetry and ARGO data
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Using Altimetry, GRACE and Argo to assess stationary circulation and transports...
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On estimating the circulation in the North Atlantic from altimetry and ARGO data
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Inverse solution for pentadal variability in the North Atlantic
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Inverse Estimate of the North Atlantic Circulation: Influence of the fine resolu...
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Inverse Estimate of the North Atlantic Circulation: Influence of the fine resolu...
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Variability of the North Atlantic circulation from 1950 to 1994 determined by 3D...
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Building a Scalable Ensemble Data Assimilation System for Coupled Models with PD...
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Scalable Coupled Ensemble Data Assimilation with AWI-CM and PDAF
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Initial response of reduced ice albedo and increased greenhouse gas concentratio...
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Sensitivitätsstudien mit dem gekoppelten Klimamodell ECHAM-FESOM zu Gitterauflös...
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Inverse Estimate of the North Atlantic Circulation: Influence of the fine resolu...
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Interannual variability of transports through Fram Strait estimated with a new i...
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FEMSECT: an Inverse Section Model Based on the Finite Element Method
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Filchner-Ronne Ice Shelf basal melting: Sensitivity to sea ice changes and the s...
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Using ARGO, GRACE and altimetry to assess the quasi stationary circulation in th...
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Inverse finite-element ocean circulation model (IFEOM)
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[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
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Atlantic meridional overturning circulation variability
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