Estimating the sources of global sea level rise with data assimilation techniques

Material Information

Title:
Estimating the sources of global sea level rise with data assimilation techniques
Series Title:
Proceeding of the National Academy of Sciences
Creator:
Hay, Carling C.
Morrow, Eric
Kopp, Robert E.
Mitrovica, Jerry X.
Publisher:
National Academy of Sciences
Publication Date:
Language:
English

Subjects

Subjects / Keywords:
Climate change ( lcsh )
Ice sheets ( lcsh )
Sea level rise ( lcsh )
Kalman filtering ( lcsh )

Notes

Abstract:
A rapidly melting ice sheet produces a distinctive geometry, or fingerprint, of sea level (SL) change. Thus, a network of SL observationsmay, in principle, be used to infer sources ofmeltwater flux.We outline a formalism, based on amodified Kalman smoother, for using tide gauge observations to estimate the individual sources of global SL change.We also report on a series of detection experiments based on synthetic SL data that explore the feasibility of extracting source information from SL records. The Kalman smoother technique iteratively calculates the maximum-likelihood estimate of Greenland ice sheet (GIS) andWestAntarctic ice sheet (WAIS) melt at each time step, and it accommodates data gaps while also permitting the estimation of nonlinear trends. Our synthetic tests indicate that when all tide gauge records are used in the analysis, it should be possible to estimate GIS and WAIS melt rates greater than ∼0.3 and ∼0.4 mm of equivalent eustatic sea level rise per year, respectively.We have also implemented a multimodel Kalman filter that allows us to account rigorously for additional contributions to SL changes and their associated uncertainty. The multimodel filter uses 72 glacial isostatic adjustment models and 3 ocean dynamic models to estimate the most likely models for these processes given the synthetic observations. We conclude that ourmodified Kalman smoother procedure provides a powerful method for inferring melt rates in a warming world. ( English )

Record Information

Source Institution:
Florida International University
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Sea Level Rise