{"id":161,"date":"2017-07-05T12:15:31","date_gmt":"2017-07-05T16:15:31","guid":{"rendered":"https:\/\/www2.whoi.edu\/staff\/ykwon\/?page_id=161"},"modified":"2023-02-27T16:13:29","modified_gmt":"2023-02-27T20:13:29","slug":"data","status":"publish","type":"page","link":"https:\/\/www2.whoi.edu\/staff\/ykwon\/data\/","title":{"rendered":"Data"},"content":{"rendered":"\n<h1>\n\t\tData\n\t<\/h1>\n<h2>Surface and bottom T\/S along the continental shelf off the Canadian and U.S. East Coasts<\/h2>\n<p>Please refer to the following paper for the description of the data:<\/p>\n<p>Richaud, B.*, Y.-O. Kwon, T.M. Joyce, P.S. Fratantoni, and S.J. Lentz, 2016: Surface and bottom temperature and salinity climatology along the continental shelf off the Canadian and U.S. East Coasts. <i>Cont. Shelf Res.<\/i>, <strong>124<\/strong>, 165-181, doi:10.1016\/j.csr.2016.06.005. [<a href=\"http:\/\/www.whoi.edu\/fileserver.do?id=235864&amp;pt=2&amp;p=202390\" target=\"_blank\" rel=\"noopener\">pdf<\/a>]\n<ul>\n<li>\u00a0Gridded Seasonal Climatology [<a href=\"http:\/\/www.whoi.edu\/fileserver.do?id=243384&amp;pt=2&amp;p=248769\" target=\"_blank\" rel=\"noopener\">matlab-format<\/a>] [<a href=\"http:\/\/www.whoi.edu\/fileserver.do?id=243424&amp;pt=2&amp;p=248769\" target=\"_blank\" rel=\"noopener\">netcdf-format<\/a>]\n<\/li>\n<li>\u00a0Gridded Monthly Climatology [<a href=\"http:\/\/www.whoi.edu\/fileserver.do?id=243404&amp;pt=2&amp;p=248769\" target=\"_blank\" rel=\"noopener\">matlab-format<\/a>] [<a href=\"http:\/\/www.whoi.edu\/fileserver.do?id=243444&amp;pt=2&amp;p=248769\" target=\"_blank\" rel=\"noopener\">netcdf-format<\/a>]<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h2>Hindcast 1979-2014 historical simulation using Whole Atmosphere Community Climate Model version 6 (WACCM6)<\/h2>\n<p>Please refer to the following paper for the description of the data:<\/p>\n<p>Liang, Y.-C.*, Y.-O. Kwon, C. Frankignoul, G. Danabasoglu, S. Yeager, A. Cherchi, Y. Gao, G. Gastineau, R. Ghosh, D. Matei, J.V. Mecking, D. Peano, L. Suo, and T. Tian, 2020: Quantification of the Arctic Sea Ice-Driven Atmospheric Circulation Variability in Coordinated Large Ensemble Simulations. <em>Geophys. Res. Lett.<\/em>, <strong>47<\/strong>, doi:1029\/2019GL085397. [<a href=\"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-content\/uploads\/sites\/27\/2020\/01\/Liang_et_al_2020_GRL_reduced.pdf\" target=\"_blank\" rel=\"noopener\">pdf<\/a>]\n<ul>\n<li>Selected monthly and daily variables are available from <a href=\"https:\/\/dashrepo.ucar.edu\/dataset\/189_islas.html\" target=\"_blank\" rel=\"noopener\">UCAR\/NCAR DASH repository<\/a>.<\/li>\n<li>For other variables, please email <a href=\"https:\/\/www2.whoi.edu\/staff\/ykwon\/\" target=\"_blank\" rel=\"noopener\">me<\/a>.<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h2>Mixed layer properties on the Northeast U.S. continental shelf (1993-2018)<\/h2>\n<p>Please refer to the following paper for the description of the data:<\/p>\n<p>Cai, C.*, Y.-O. Kwon, Z. Chen*, and P. Fratantoni, 2021: Mixed layer depth climatology over the Northeast U.S. continental shelf (1993-2018). <em>Cont. Shelf Res<\/em>., <strong>231<\/strong>, 104611. https:\/\/doi.org\/10.1016\/j.csr.2021.104611. [<a href=\"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-content\/uploads\/sites\/27\/2021\/11\/Cai_et_al_2021_CSR.pdf\" target=\"_blank\" rel=\"noopener\">pdf<\/a>]\n<ul>\n<li>MLD climatology: <a href=\"https:\/\/www.dropbox.com\/s\/r29pbm7f0nza1d9\/winter_mld_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">winter<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/np7d0agpqpf9dop\/spring_mld_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">spring<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/kajq9555upotur2\/summer_mld_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">summer<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/61lbodrevd8vb6b\/fall_mld_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">fall<\/a><\/li>\n<li>MLT climatology: <a href=\"https:\/\/www.dropbox.com\/s\/uo3dv51i6h30cjy\/winter_mlt_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">winter<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/yeshfgzx7z3pm4r\/spring_mlt_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">spring<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/3aitbffnxfelixw\/summer_mlt_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">summer<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/9jfuzq88178nes8\/fall_mlt_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">fall<\/a><\/li>\n<li>MLS climatology: <a href=\"https:\/\/www.dropbox.com\/s\/oda3obytt7raq2d\/winter_mls_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">winter<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/t0k3of2vrd3xje8\/spring_mls_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">spring<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/0jhm3t3ywy72fo9\/summer_mls_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">summer<\/a>, <a href=\"https:\/\/www.dropbox.com\/s\/5qdb5h2ennqq7ft\/fall_mls_climatology_renamed.nc?dl=0\" target=\"_blank\" rel=\"noopener\">fall<\/a><\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h2>Code to compare various statistical methods for estimating asymmetric relationships<\/h2>\n<p>Please find the details from the following paper:<\/p>\n<p>Frankignoul, C., and Y.-O. Kwon, 2022: On the statistical estimation of asymmetrical relationship between two climate variables. <em>Geophys. Res. Lett<\/em>., <strong>49<\/strong><em>, <\/em>e2022GL100777. https:\/\/doi.org\/10.1029\/2022GL100777.<\/p>\n<ul>\n<li>Matlab code for Figure 1: <a href=\"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-content\/uploads\/sites\/27\/2022\/09\/Figure1_matlab_m-file.pdf\" target=\"_blank\" rel=\"noopener\">Figure1.m<\/a><\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h2>Gulf Stream SST gradient index<\/h2>\n<p>Please find the details from the following paper:<\/p>\n<p>Parfitt, R., Y.-O. Kwon, and M. Andres, 2022: A monthly index for the large-scale sea surface temperature gradient across the separated Gulf Stream. <em>Geophys. Res. Lett<\/em>., <strong>49<\/strong>, e2022GL100914. https:\/\/doi.org\/10.1029\/2022GL100914.<\/p>\n<ul>\n<li>Gulf Stream SST gradient index [<a href=\"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-content\/uploads\/sites\/27\/2023\/02\/NOAA_OISST_GS_dSST_index_monthly_1993_2019_release.mat.zip\" target=\"_blank\" rel=\"noopener\">matlab-format<\/a>]<\/li>\n<\/ul>\n\n","protected":false},"excerpt":{"rendered":"<p>Data Surface and bottom T\/S along the continental shelf off the Canadian and U.S. East Coasts Please refer to the following paper for the description of the data: Richaud, B.*, Y.-O. Kwon, T.M. Joyce, P.S. Fratantoni, and S.J. Lentz, 2016: Surface and bottom temperature and salinity climatology along the continental shelf off the Canadian and&hellip;<\/p>\n","protected":false},"author":25,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/pages\/161"}],"collection":[{"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/users\/25"}],"replies":[{"embeddable":true,"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/comments?post=161"}],"version-history":[{"count":3,"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/pages\/161\/revisions"}],"predecessor-version":[{"id":480,"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/pages\/161\/revisions\/480"}],"wp:attachment":[{"href":"https:\/\/www2.whoi.edu\/staff\/ykwon\/wp-json\/wp\/v2\/media?parent=161"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}