{"id":749,"date":"2019-12-13T18:03:23","date_gmt":"2019-12-13T22:03:23","guid":{"rendered":"https:\/\/www2.whoi.edu\/site\/aomip\/?page_id=749"},"modified":"2021-06-18T09:24:52","modified_gmt":"2021-06-18T13:24:52","slug":"ocean-ice-exchange","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/site\/aomip\/models\/details\/ocean-ice-exchange\/","title":{"rendered":"Ocean-ice exchange"},"content":{"rendered":"\n\n\t

Ocean-ice exchange<\/h1>\n\n\n\n\n\t\n\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t\n\t

code<\/p><\/th>

ocean-ice heat exchg<\/p><\/th>

ocean-ice FW exchg<\/p><\/th>

ocean-ice momentum exchg<\/p><\/th>\n<\/tr>\n<\/thead>\n

AWI<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

\u00a0DRAKKAR<\/p><\/td>

\u00a0linear in ocean T - freezing T<\/p><\/td>

\u00a0salt rejection, freshwater flux, ice at 6 ppt<\/p><\/td>

\u00a0quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

GSFC<\/p><\/td>

\u00a0Boundary layer model (Mellor and Kantha, JGR 1989)<\/p><\/td>

\u00a0Same<\/p><\/td>

\u00a0same<\/p><\/td>\n<\/tr>\n

ICMMG<\/p><\/td>

same as LANL<\/p><\/td>

same as LANL<\/p><\/td>

same as LANL<\/p><\/td>\n<\/tr>\n

LANL<\/p><\/td>

*<\/p><\/td>

virtual salt flux, ice at 4 ppt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

LU<\/p><\/td>

linear in ocean T - freezing T<\/p><\/td>

virtual salt flux, ice at 4 ppt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

NERSC<\/p><\/td>

linear in To and Tf (Maykut and McPhee, 1995)<\/p><\/td>

virtual salt flux, ice at 6ppt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

NPS<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

NYU<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

POL<\/p><\/td>

linear in To and Tf (McPhee, 1992)<\/p><\/td>

explicit freshwater and salt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

FEMAO<\/p><\/td>

\u00a0linear in To and Tf (McPhee, 1992)<\/p><\/td>

\u00a0explicit freshwater and salt, ice at 4 ppt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p>
\n

+ Gravity wave drag<\/p><\/td>\n<\/tr>\n

INMOM<\/p><\/td>

\u00a0Ebert & Curry, 1993<\/p><\/td>

\u00a0<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

RCO<\/p><\/td>

bulk (Omstedt & Wettlaufer, 1992)<\/p><\/td>

salt rejection, freshwater flux, ice at 4 ppt<\/p><\/td>

quadratic, Cd=3.5e-3<\/p><\/td>\n<\/tr>\n

UCL<\/p><\/td>

linear in ocean T - freezing T<\/p><\/td>

salt rejection, freshwater flux<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n

UW<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

DAL<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

FSU<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

GFDL<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

IARC-A<\/p><\/td>

reset SST to freezing T<\/p><\/td>

salt rejection, freshwater flux<\/p><\/td>

quadratic, Cd=5.e-3<\/p><\/td>\n<\/tr>\n

IARC-B<\/p><\/td>

reset SST to freezing T<\/p><\/td>

salt rejection, freshwater flux<\/p><\/td>

quadratic, Cd=5.e-3<\/p><\/td>\n<\/tr>\n

ECCO2<\/p><\/td>

relax SST to freezing T<\/p><\/td>

explicit salt exchange (Nguyen et al, 2009)<\/p><\/td>

quadratic, Cd=5.56e-3<\/p><\/td>\n<\/tr>\n

MIT<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

NCAR<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

NPI<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

UMASD<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

NOCS\/ORCA25<\/p><\/td>

Turbulent mixing (McPhee, 1992)+lead model<\/p><\/td>

freshwater and salt<\/p><\/td>

quadratic, Cd=5.0e-3<\/p><\/td>\n<\/tr>\n

MCGU<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>

\u00a0<\/p><\/td>\n<\/tr>\n

LOCEAN<\/p><\/td>

linear in ocean T - freezing T<\/p><\/td>

salt rejection<\/p><\/td>

Hibler and Bryan, 1987<\/p><\/td>\n<\/tr>\n

IOS<\/p><\/td>

linear in ocean T - freezing T<\/p><\/td>

virtual salt flux, ice at 4 ppt<\/p><\/td>

quadratic, Cd=5.5e-3<\/p><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n\n

* LANL: heat, salt: ice formation in ocean (frazil) maintains temperature at or above salinity-dependent freezing temperature, up to maximum = linear in ocean T – freezing T, coef 0.575<\/p>\n\n","protected":false},"excerpt":{"rendered":"

Ocean-ice exchange * LANL: heat, salt: ice formation in ocean (frazil) maintains temperature at or above salinity-dependent freezing temperature, up to maximum = linear in ocean T – freezing T, coef 0.575<\/p>\n","protected":false},"author":83,"featured_media":0,"parent":639,"menu_order":17,"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\/749"}],"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=749"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/749\/revisions"}],"predecessor-version":[{"id":1685,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/749\/revisions\/1685"}],"up":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/pages\/639"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/site\/aomip\/wp-json\/wp\/v2\/media?parent=749"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}