{"id":914,"date":"2020-02-11T17:14:32","date_gmt":"2020-02-11T21:14:32","guid":{"rendered":"https:\/\/www2.whoi.edu\/site\/aomip\/?page_id=914"},"modified":"2021-06-18T09:35:57","modified_gmt":"2021-06-18T13:35:57","slug":"surface-restoring-forcing-data","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/site\/aomip\/data\/surface-restoring-forcing-data\/","title":{"rendered":"Surface-Restoring Forcing Data"},"content":{"rendered":"\n\n\t<h1>Surface-Restoring Forcing Data<\/h1>\n<p>Restoring of surface salinity is carried out during the coordinated-spinup (Expt. #2) and coordinated-analysis experiments (Expt. #3); there is no restoring of surface temperature. The following strategy has been adopted in an effort to minimize the impact of surface-salinity restoring on the experiments.<\/p>\n<p>During the first eleven years of the integration (i.e., Jan 1948 &#8211; Dec 1958) surface restoring is applied everywhere on the ocean surface using a restoring time-scale of 180 days. During the remaining years (i.e., 1959 &#8211; forward) there is no restoring of surface salinity. The restoring is performed using an annually averaged climatology of surface salinity from the Polar Science Center Hydrographic Climatology (<a href=\"http:\/\/psc.apl.washington.edu\/Climatology.html\">PHC<\/a>) atlas.<\/p>\n<p>As an exception to this rule, global-domain models may continue to perform surface restoring of salinity after January 1959, but only in that part of their domains south of 60\u00baN.<\/p>\n<p>Restoring is also applied along the lateral boundaries of the regional AOMIP domains. The detailed specification on that restoring is the free-choice of the individual AOMIP modeling groups.<\/p>\n\t<h2>Related Files<\/h2>\n<ul>\n<li><a href=\"https:\/\/www2.whoi.edu\/site\/aomip\/wp-content\/uploads\/sites\/100\/2020\/03\/Annual_phc2.1_beta.dat_46468.zip\">Surface Temperature and Salinity (Annual Climatology)<\/a><br \/>\nThe restoring is performed using an annually averaged climatology of surface salinity from the Polar Science Center Hydrographic Climatology (PHC) atlas.<\/li>\n<\/ul>\n\n","protected":false},"excerpt":{"rendered":"<p>Surface-Restoring Forcing Data Restoring of surface salinity is carried out during the coordinated-spinup (Expt. #2) and coordinated-analysis experiments (Expt. #3); there is no restoring of surface temperature. The following strategy has been adopted in an effort to minimize the impact of surface-salinity restoring on the experiments. During the first eleven years of the integration (i.e.,&hellip;<\/p>\n","protected":false},"author":83,"featured_media":0,"parent":307,"menu_order":4,"comment_status":"closed","ping_status":"closed","template":"tpl-sidebar.php","meta":{"advanced-sidebar-menu\/link-title":"","advanced-sidebar-menu\/exclude-page":false},"_links":{"self":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/914"}],"collection":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/users\/83"}],"replies":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/comments?post=914"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/914\/revisions"}],"predecessor-version":[{"id":1703,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/914\/revisions\/1703"}],"up":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/307"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/media?parent=914"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}