Víctor Malagón-Santos, A. Slangen, T. Hermans, Sönke Dangendorf, M. Marcos, N. Maher
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Here, we test two pattern recognition methods based on empirical orthogonal functions (EOFs), namely\nsignal-to-noise maximizing EOF pattern filtering and low-frequency component analysis, for their ability to reduce errors in pattern scaling of\nocean dynamic sea-level change. We use the Max Planck Institute Grand Ensemble (MPI-GE) as a test bed for both methods, as it is a type of\ninitial-condition large ensemble designed for an optimal characterization of the externally forced response. We show that the two methods tested\nhere more efficiently reduce errors than conventional approaches such as a simple ensemble average. For instance, filtering only two realizations by\ncharacterizing their common response to external forcing reduces the random error by almost 60 %, a reduction that is only achieved by averaging\nat least 12 realizations. We further investigate the applicability of both methods to single-realization modeling experiments, including four CMIP5\nsimulations for comparison with previous regional emulation analyses. Pattern filtering leads to a varying degree of error reduction depending on\nthe model and scenario, ranging from more than 20 % to about 70 % reduction in global-mean root mean squared error compared with unfiltered\nsimulations. Our results highlight the relevance of pattern recognition methods as a tool to reduce errors in regional emulation tools of ocean\ndynamic sea-level change, especially when one or only a few realizations are available. Removing internal variability prior to tuning regional\nemulation tools can optimize the performance of the statistical model, leading to substantial differences in emulated dynamic sea level compared to\nunfiltered simulations.\n","PeriodicalId":19535,"journal":{"name":"Ocean Science","volume":null,"pages":null},"PeriodicalIF":4.1000,"publicationDate":"2023-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Improving statistical projections of ocean dynamic sea-level change using pattern recognition techniques\",\"authors\":\"Víctor Malagón-Santos, A. Slangen, T. Hermans, Sönke Dangendorf, M. Marcos, N. Maher\",\"doi\":\"10.5194/os-19-499-2023\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. Regional emulation tools based on statistical relationships, such as pattern scaling, provide a computationally inexpensive way of projecting ocean\\ndynamic sea-level change for a broad range of climate change scenarios. Such approaches usually require a careful selection of one or more predictor\\nvariables of climate change so that the statistical model is properly optimized. Even when appropriate predictors have been selected, spatiotemporal\\noscillations driven by internal climate variability can be a large source of statistical model error. Using pattern recognition techniques that\\nexploit spatial covariance information can effectively reduce internal variability in simulations of ocean dynamic sea level, significantly reducing\\nrandom errors in regional emulation tools. Here, we test two pattern recognition methods based on empirical orthogonal functions (EOFs), namely\\nsignal-to-noise maximizing EOF pattern filtering and low-frequency component analysis, for their ability to reduce errors in pattern scaling of\\nocean dynamic sea-level change. We use the Max Planck Institute Grand Ensemble (MPI-GE) as a test bed for both methods, as it is a type of\\ninitial-condition large ensemble designed for an optimal characterization of the externally forced response. We show that the two methods tested\\nhere more efficiently reduce errors than conventional approaches such as a simple ensemble average. For instance, filtering only two realizations by\\ncharacterizing their common response to external forcing reduces the random error by almost 60 %, a reduction that is only achieved by averaging\\nat least 12 realizations. We further investigate the applicability of both methods to single-realization modeling experiments, including four CMIP5\\nsimulations for comparison with previous regional emulation analyses. Pattern filtering leads to a varying degree of error reduction depending on\\nthe model and scenario, ranging from more than 20 % to about 70 % reduction in global-mean root mean squared error compared with unfiltered\\nsimulations. Our results highlight the relevance of pattern recognition methods as a tool to reduce errors in regional emulation tools of ocean\\ndynamic sea-level change, especially when one or only a few realizations are available. 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Improving statistical projections of ocean dynamic sea-level change using pattern recognition techniques
Abstract. Regional emulation tools based on statistical relationships, such as pattern scaling, provide a computationally inexpensive way of projecting ocean
dynamic sea-level change for a broad range of climate change scenarios. Such approaches usually require a careful selection of one or more predictor
variables of climate change so that the statistical model is properly optimized. Even when appropriate predictors have been selected, spatiotemporal
oscillations driven by internal climate variability can be a large source of statistical model error. Using pattern recognition techniques that
exploit spatial covariance information can effectively reduce internal variability in simulations of ocean dynamic sea level, significantly reducing
random errors in regional emulation tools. Here, we test two pattern recognition methods based on empirical orthogonal functions (EOFs), namely
signal-to-noise maximizing EOF pattern filtering and low-frequency component analysis, for their ability to reduce errors in pattern scaling of
ocean dynamic sea-level change. We use the Max Planck Institute Grand Ensemble (MPI-GE) as a test bed for both methods, as it is a type of
initial-condition large ensemble designed for an optimal characterization of the externally forced response. We show that the two methods tested
here more efficiently reduce errors than conventional approaches such as a simple ensemble average. For instance, filtering only two realizations by
characterizing their common response to external forcing reduces the random error by almost 60 %, a reduction that is only achieved by averaging
at least 12 realizations. We further investigate the applicability of both methods to single-realization modeling experiments, including four CMIP5
simulations for comparison with previous regional emulation analyses. Pattern filtering leads to a varying degree of error reduction depending on
the model and scenario, ranging from more than 20 % to about 70 % reduction in global-mean root mean squared error compared with unfiltered
simulations. Our results highlight the relevance of pattern recognition methods as a tool to reduce errors in regional emulation tools of ocean
dynamic sea-level change, especially when one or only a few realizations are available. Removing internal variability prior to tuning regional
emulation tools can optimize the performance of the statistical model, leading to substantial differences in emulated dynamic sea level compared to
unfiltered simulations.
期刊介绍:
Ocean Science (OS) is a not-for-profit international open-access scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on all aspects of ocean science: experimental, theoretical, and laboratory. The primary objective is to publish a very high-quality scientific journal with free Internet-based access for researchers and other interested people throughout the world.
Electronic submission of articles is used to keep publication costs to a minimum. The costs will be covered by a moderate per-page charge paid by the authors. The peer-review process also makes use of the Internet. It includes an 8-week online discussion period with the original submitted manuscript and all comments. If accepted, the final revised paper will be published online.
Ocean Science covers the following fields: ocean physics (i.e. ocean structure, circulation, tides, and internal waves); ocean chemistry; biological oceanography; air–sea interactions; ocean models – physical, chemical, biological, and biochemical; coastal and shelf edge processes; paleooceanography.