Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates

By Carl Wunsch, Patrick Heimbach. 2013

148 citations recorded by the source corpus.

Abstract The World Ocean Circulation Experiment drove the development of estimates of the decadal scale time evolving general circulation that are dynamically and kinematically consistent. A long timescale, and a goal of estimation rather than prediction, preclude the use of meteorological methods called “data assimilation (DA).” Instead, “state estimation” methods are reviewed here and distinguished from DA. Results from the dynamically consistent family of solutions from the project Estimating the Circulation and Climate of the Ocean based upon least-squares Lagrange multipliers (adjoints) are used to discuss the determination of the dominant elements of the circulation in the period since 1992—which marked the beginning of the satellite altimetric record. Significant changes documented in the Arctic in recent decades now mandate consideration of the coupled ocean-cryospheric state.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/55f5d02be223ab0cbb053a9c736cd9707393177c

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In Atmospheric Science

  1. S. Griffies
  2. Robert Hallberg
  3. Gokhan Danabasoglu
  4. Johann Jungclaus
  5. Helmuth Haak
  6. B. Fox‐Kemper
  7. J. Gregory
  8. K. Taylor

In Global and Planetary Change

  1. S. Griffies
  2. Robert Hallberg
  3. Gokhan Danabasoglu
  4. Johann Jungclaus
  5. Helmuth Haak
  6. J. Gregory
  7. B. Fox‐Kemper
  8. K. Taylor

In Oceanography

  1. S. Griffies
  2. Robert Hallberg
  3. Gokhan Danabasoglu
  4. B. Fox‐Kemper
  5. Johann Jungclaus
  6. Helmuth Haak
  7. Alistair Adcroft
  8. A. Nurser

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