{"id":3183,"date":"2014-07-18T23:06:25","date_gmt":"2014-07-19T03:06:25","guid":{"rendered":"http:\/\/mseas.mit.edu\/?p=3183"},"modified":"2021-07-06T13:13:37","modified_gmt":"2021-07-06T17:13:37","slug":"issues-and-progress-in-the-prediction-of-ocean-submesoscale-features-and-internal-waves","status":"publish","type":"post","link":"https:\/\/mseas.mit.edu\/?p=3183","title":{"rendered":"Issues and Progress in the Prediction of Ocean Submesoscale Features and Internal Waves"},"content":{"rendered":"<p>Data-constrained dynamical ocean modeling for\r\nthe purpose of detailed forecasting and prediction continues to\r\nevolve and improve in quality. Modeling methods and\r\ncomputational capabilities have each improved. The result is that\r\nmesoscale phenomena can be modeled with skill, given sufficient\r\ndata. However, many submesoscale features are less well\r\nmodeled and remain largely unpredicted from a deterministic\r\nevent standpoint, and possibly also from a statistical property\r\nstandpoint. A multi-institution project is underway with goals of\r\nuncovering more of the details of a few submesoscale processes,\r\nworking toward better predictions of their occurrence and their\r\nvariability. A further component of our project is application of\r\nthe new ocean models to ocean acoustic modeling and prediction.\r\nThis paper focuses on one portion of the ongoing work: Efforts to\r\nlink nonhydrostatic-physics models of continental-shelf nonlinear\r\ninternal wave evolution to data-driven regional models. Ocean\r\nfront-related effects are also touched on.<\/p>","protected":false},"excerpt":{"rendered":"<p>Data-constrained dynamical ocean modeling for the purpose of detailed forecasting and prediction continues to evolve and improve in quality. Modeling methods and computational capabilities have each improved. The result is that mesoscale phenomena can be modeled with skill, given sufficient data. However, many submesoscale features are less well modeled and remain largely unpredicted from a [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[32,37,28,38,5,72,67],"tags":[102,104,133,134,99,103,132],"class_list":["post-3183","post","type-post","status-publish","format-standard","hentry","category-numerical-ocean-modeling","category-applications-to-ocean-dynamics","category-multiscale-ocean-modeling","category-physical-oceanography","category-publications","category-proceedings-of-refereed-conferences-multiscale-ocean-modeling","category-proceedings-of-refereed-conferences-physical-oceanography","tag-acoustic-modeling","tag-internal-waves","tag-middle-atlantic-bight","tag-mseas","tag-multiscale","tag-ocean-modeling","tag-sw06"],"_links":{"self":[{"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/posts\/3183","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=3183"}],"version-history":[{"count":8,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/posts\/3183\/revisions"}],"predecessor-version":[{"id":3538,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=\/wp\/v2\/posts\/3183\/revisions\/3538"}],"wp:attachment":[{"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=3183"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=3183"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/mseas.mit.edu\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=3183"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}