4.3 Article

Using Drifter Velocity Measurements to Assess and Constrain Coarse-Resolution Ocean Models

Journal

JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY
Volume 38, Issue 4, Pages 909-919

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JTECH-D-20-0159.1

Keywords

Ocean circulation; Error analysis; Climate models; Data assimilation

Funding

  1. GRACE Follow-On Science Team through NASA [80NSSC20K0728]
  2. NASA Physical Oceanography, Cryospheric Science, and Modeling, Analysis and Prediction programs
  3. National Aeronautics and Space Administration [80NM0018D0004]
  4. NOAA's Global Ocean Monitoring and Observing Program
  5. Atlantic Oceanographic and Meteorological Laboratory

Ask authors/readers for more resources

Fitting ocean models to Global Drifter Program (GDP) measurements can significantly impact the ECCO large-scale time-mean surface circulation. However, the impact on the ECCO time-variable circulation is weaker and mainly limited to low latitudes, with representation errors contributing substantially to degrading the data impacts.
Properly fitting ocean models to observations is crucial for improving model performance and understanding ocean dynamics. Near-surface velocity measurements from the Global Drifter Program (GDP) contain valuable information about upper-ocean circulation and air-sea fluxes on various space and time scales. This study explores whether GDP measurements can be used for usefully constraining the surface circulation from coarse-resolution ocean models, using global solutions produced by the consortium for Estimating the Circulation and Climate of the Ocean (ECCO) as an example. To address this problem, a careful examination of velocity data errors is required. Comparisons between an ECCO model simulation, performed without any data constraints, and GDP and Ocean Surface Current Analyses Real-Time (OSCAR) velocity data, over the period 1992-2017, reveal considerable differences in magnitude and pattern. These comparisons are used to estimate GDP data errors in the context of the time-mean and time-variable surface circulations. Both instrumental errors and errors associated with limitations in model physics and resolution (representation errors) are considered. Given the estimated model-data differences, errors, and signal-to-noise ratios, our results indicate that constraining ocean-state estimates to GDP can have a substantial impact on the ECCO large-scale time-mean surface circulation over extensive areas. Impact of GDP data constraints on the ECCO time-variable circulation would be weaker and mainly limited to low latitudes. Representation errors contribute substantially to degrading the data impacts.

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