Abstract

Data assimilation is a crucial aspect of modern oceanography. It allows the future forecasting and backward smoothing of ocean state from the noisy observations. Statistical methods are employed to perform these tasks and are often based on or related to the Kalman filter. Typically Kalman filters assumes that the locations associated with observations are known with certainty. This is reasonable for typical oceanographic measurement methods. Recently, however an alternative and abundant source of data comes from the deployment of ocean sensors on marine animals. This source of data has some attractive properties: unlike traditional oceanographic collection platforms, it is relatively cheap to collect, plentiful, has multiple scientific uses and users, and samples areas of the ocean that are often difficult of costly to sample. However, inherent uncertainty in the location of the observations is a barrier to full utilisation of animal-borne sensor data in data-assimilation schemes. In this article we examine this issue and suggest a simple approximation to explicitly incorporate the location uncertainty, while staying in the scope of Kalman-filter-like methods. The approximation stems from a Taylor-series approximation to elements of the updating equation.

Highlights

  • The process of updating physical ocean models using observations, to obtain accurate estimates of ocean state is referred to as data assimilation (DA) and is used to forecast current and future ocean conditions, as well as for hind-casting of historical states (e.g., [1], [2])

  • In this article we describe some simple adjustments to the Kalman filter algorithm which allow the use of spatially imprecise data in the DA scheme

  • Our motivation for this study was the challenge of utilizing the voluminous amounts of sensor data collected from marine animals for oceanographic data assimilation schemes

Read more

Summary

Introduction

The process of updating physical ocean models using observations, to obtain accurate estimates of ocean state is referred to as data assimilation (DA) and is used to forecast current and future ocean conditions, as well as for hind-casting (backward smoothing) of historical states (e.g., [1], [2]). The ocean and atmosphere are continuously changing, so it is desirable to efficiently update model predictions (forecasts and hind-casts) with new data as it comes online. The DA scheme needs to be able to use a wide variety of different data sources. In this study we consider the use of spatially imprecise measurements in DA schemes – accurate measurements on the observed state variables, with imprecise spatial locations

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call