Abstract

Data assimilation (DA) in the geophysical sciences remains the cornerstone of robust forecasts from numerical models. Indeed, DA plays a crucial role in the quality of numerical weather prediction, and is a crucial building block that has allowed dramatic improvements in weather forecasting over the past few decades. DA is commonly framed in a variational setting, where one solves an optimization problem within a Bayesian formulation using raw model forecasts as a prior, and observations as likelihood. This leads to a DA objective function that needs to be minimized, where the decision variables are the initial conditions specified to the model. In traditional DA, the forward model is numerically and computationally expensive. Here we replace the forward model with a low-dimensional, data-driven, and differentiable emulator. Consequently, gradients of our DA objective function with respect to the decision variables are obtained rapidly via automatic differentiation. We demonstrate our approach by performing an emulator-assisted DA forecast of geopotential height. Our results indicate that emulator-assisted DA is faster than traditional equation-based DA forecasts by four orders of magnitude, allowing computations to be performed on a workstation rather than a dedicated high-performance computer. In addition, we describe accuracy benefits of emulator-assisted DA when compared to simply using the emulator for forecasting (i.e., without DA). Our overall formulation is denoted AIAEDA (Artificial Intelligence Emulator Assisted Data Assimilation).

Highlights

  • Data assimilation (DA) in the geophysical sciences remains the cornerstone of robust forecasts from numerical models

  • This leads to a DA objective function that needs to be minimized, where the decision variables are the initial conditions specified to the model

  • The data used in this study is a subset of 20 years of output from the regional climate model WRF version 3.3.1, prepared 235 with methods and configurations described by Wang and Kotamarthi (2014)

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Summary

Introduction

15 A physical system can be characterized by our existing knowledge of the system plus a set of observations. Data assimilation (DA) combines existing knowledge of a system, usually in the form of a model, with observations to infer. 20 the best estimate of the system state at a given time Both existing knowledge and observations come with errors that lead to uncertainties about the “true” state of the system being investigated. When combining model results characterizing our knowledge of the system with observations, it is essential to account for these errors and give an appropriate weight to each source of information available. This leads to statistical approaches, which are the basis for state-of-the-art DA methods

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