An Objective Analysis of the POLYMODE Local Dynamics Experiment. Part I: General Formalism and Statistical Model Selection

Abstract

A formalism is presented for making estimates of a variety of mesoscale quantities—streamfunction, potential vorticity, and both linear and nonlinear terms in the dynamical balance equations for heat and potential vorticity—from measurements made during the POLYMODE Local Dynamics Experiment (LDE). The formalism is based upon the dynamical assumptions of geostrophic and hydrostatic balance and the methodology of multivariate optimal estimation theory. A particular novel result is the derivation of optimal estimators for quadratically nonlinear quantities, such as the advection terms in the dynamical balance equations. Two statistical representations are formulated that are appropriate to different subsets of LDE data: a vertical modal representation for spatially extensive estimates of the most energetic mesoscale motion (for use during the two-month intensive phase of LDE), and a vertically local representation for the somewhat smaller scale motions that can be estimated from the thermocline moo... Abstract A formalism is presented for making estimates of a variety of mesoscale quantities—streamfunction, potential vorticity, and both linear and nonlinear terms in the dynamical balance equations for heat and potential vorticity—from measurements made during the POLYMODE Local Dynamics Experiment (LDE). The formalism is based upon the dynamical assumptions of geostrophic and hydrostatic balance and the methodology of multivariate optimal estimation theory. A particular novel result is the derivation of optimal estimators for quadratically nonlinear quantities, such as the advection terms in the dynamical balance equations. Two statistical representations are formulated that are appropriate to different subsets of LDE data: a vertical modal representation for spatially extensive estimates of the most energetic mesoscale motion (for use during the two-month intensive phase of LDE), and a vertically local representation for the somewhat smaller scale motions that can be estimated from the thermocline moo...