{"id":384,"date":"2017-05-30T16:42:05","date_gmt":"2017-05-30T06:42:05","guid":{"rendered":"http:\/\/cosima.org.au\/?page_id=384"},"modified":"2020-05-25T14:18:31","modified_gmt":"2020-05-25T04:18:31","slug":"mom-sis-01","status":"publish","type":"page","link":"https:\/\/cosima.org.au\/index.php\/models\/mom-sis-01\/","title":{"rendered":"MOM-SIS-01"},"content":{"rendered":"<p>MOM-SIS-01 is our\u00a0previous 1\/10\u00b0 ocean-sea ice model (now deprecated and replaced by ACCESS-OM2-01). It uses MOM5.1 with 0.1\u00b0 lateral resolution at the Equator, tripolar in the north and Mercator projection down to 65\u00b0S and 75 vertical levels. The sea ice is SIS, coupled with the FMS coupler. The model can be forced using either CORE or JRA forcing sets. The model has been used in a range perturbation experiments and publications.<\/p>\n<h3>Recent publications using this model configuration:<\/h3>\n<p>Stewart, K. D., A. M. Hogg, S. M. Griffies, A. P. Heerdegen, M. L. Ward, P. Spence, and M. H. England, 2017: <a href=\"http:\/\/dx.doi.org\/10.1016\/j.ocemod.2017.03.012\">Vertical resolution of baroclinic modes in global ocean models.<\/a> Ocean Modell, 113, 50\u201365, doi:10.1016\/j.ocemod.2017.03.012.<\/p>\n<p>&nbsp;<\/p>\n<figure id=\"attachment_387\" aria-describedby=\"caption-attachment-387\" style=\"width: 770px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-387 size-full\" src=\"https:\/\/cosima.org.au\/wp-content\/uploads\/2017\/05\/kds75_eke.png\" width=\"770\" height=\"417\" srcset=\"https:\/\/cosima.org.au\/wp-content\/uploads\/2017\/05\/kds75_eke.png 770w, https:\/\/cosima.org.au\/wp-content\/uploads\/2017\/05\/kds75_eke-300x162.png 300w, https:\/\/cosima.org.au\/wp-content\/uploads\/2017\/05\/kds75_eke-768x416.png 768w\" sizes=\"(max-width: 770px) 100vw, 770px\" \/><figcaption id=\"caption-attachment-387\" class=\"wp-caption-text\">The normalized difference in EKE (m2\/s2) between 5 years of daily (u; v)<br \/> \ffields of the 75 and 50 vertical level simulations at 1000m and 3000m depth.<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>MOM-SIS-01 is our\u00a0previous 1\/10\u00b0 ocean-sea ice model (now deprecated and replaced by ACCESS-OM2-01). It uses MOM5.1 with 0.1\u00b0 lateral resolution at the Equator, tripolar in the north and Mercator projection down to 65\u00b0S and 75 vertical levels. The sea ice is SIS, coupled with the FMS coupler. The model can be forced using either CORE&hellip;<\/p>\n","protected":false},"author":20,"featured_media":0,"parent":12,"menu_order":5,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/384"}],"collection":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/users\/20"}],"replies":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/comments?post=384"}],"version-history":[{"count":7,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/384\/revisions"}],"predecessor-version":[{"id":1021,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/384\/revisions\/1021"}],"up":[{"embeddable":true,"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/pages\/12"}],"wp:attachment":[{"href":"https:\/\/cosima.org.au\/index.php\/wp-json\/wp\/v2\/media?parent=384"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}