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Andy Moore

Andy Moore. Ocean Sciences Department UC Santa Cruz. Research Interests. Ocean and climate dynamics Stochastic systems Physical-biological interactions Data assimilation Prediction Predictability. MesoAmerican Barrier Reef. Current Regions of Interest. CGOA. N Atlantic. CCS. IAS.

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Andy Moore

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  1. Andy Moore Ocean Sciences Department UC Santa Cruz

  2. Research Interests • Ocean and climate dynamics • Stochastic systems • Physical-biological interactions • Data assimilation • Prediction • Predictability

  3. MesoAmerican Barrier Reef Current Regions of Interest CGOA N Atlantic CCS IAS ENSO Southern Ocean

  4. Future drivers: • Adaptive Observations • Observation Sensitivity Ensemble Prediction 4-Dimensional Variational Data Assimilation (4DVAR) Development of Community Tools for the Regional Ocean Modeling System (ROMS) Nonlinear ROMS Tangent Linear (TL) ROMS Finite Amplitude TL ROMS Adjoint ROMS Adjoint Sensitivity Analysis Arango, Cornuelle, DiLorenzo, Miller, Moore, Powell

  5. Science Questions • Factors that limit predictability of ocean (climategyreboundary currentwakes) • Role of stochastic processes on ocean circulation and biology • Information content of observations

  6. Recent Examples • Coupled model data assimilation – ENSO (Moore, Weaver, Harrison) • Data assimilation and ensemble prediction in the IAS (Powell, Moore, Arango, Milliff, DiLorenzo)

  7. Explorer of the Seas (Royal Caribbean CL) Ship of Opportunity

  8. Recent Examples • Coupled model data assimilation – ENSO (Moore, Weaver, Harrison) • Data assimilation and ensemble prediction in the IAS (Powell, Moore, Arango, Milliff, DiLorenzo) • Coupled physical-biological modeling – CCS, CGOA (Edwards, Fiechter, Broquet, Moore, Powell, DiLorenzo)

  9. Coastal Gulf of Alaska (CGOA) ROMS-NEMURO Jerome Fiechter, UCSC

  10. Recent Examples • Coupled model data assimilation – ENSO (Moore, Weaver, Harrison) • Data assimilation and ensemble prediction in the IAS (Powell, Moore, Arango, Milliff, DiLorenzo) • Coupled physical-biological modeling – CCS, CGOA (Edwards, Fiechter, Broquet, Moore, Powell, DiLorenzo) • Influence of NAO on N Atlantic circulation – (Chhak, Moore, Milliff)

  11. NAO Wind Stress Curl (c.i. 5X10-8 N m-3) Wintertime deep ocean rectified circulation in a 1/6 degree QG model (c.i. 0.2 Sv)

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