https://submesoscale.org/publications/2020-07-29T20:43:39+00:00weekly0.6https://submesoscale.org/inthenews/2020-07-29T17:04:09+00:00weekly0.6https://submesoscale.org/a-short-history-of-the-study-of-mesoscale-ocean-eddies/https://submesoscale.org/wp-content/uploads/2014/02/spin_globe1.gifEddieshttps://submesoscale.org/wp-content/uploads/2014/01/czcs_gs.pngCZCS_GSNear-surface CHL image estimated from measurements of ocean color made by the Costal Zone Color Scanner (CZCS). Image courtesy of NASA.https://submesoscale.org/wp-content/uploads/2014/01/franklin_gs_overlay2.pngfranklin_GS_overlay2Benjimin Franklin's chart of the Gulf Stream overlaid with an image of sea surface temperature (SST) from AVHRR, showing the undulations of the Gulf Stream along with eddies shed from this boundary current.2020-04-10T04:11:10+00:00weekly0.6https://submesoscale.org/2018cosvw/https://submesoscale.org/wp-content/uploads/2018/03/nasa-cosv-workshop-2018-photo-med.jpgNASA COSV Workshop 2018 photo med2018-07-24T15:44:51+00:00weekly0.6https://submesoscale.org/naames-eddies-2/https://submesoscale.org/wp-content/uploads/2018/06/naames_eddies_cover-e1528906037429.pngnaames_eddies_cover2018-06-13T18:15:55+00:00weekly0.6https://submesoscale.org/employment-opportunities/2018-02-25T17:14:21+00:00weekly0.6https://submesoscale.org/2017/09/23/tumbling-along-like-a-tumbling-tumbleweed/https://submesoscale.org/wp-content/uploads/2017/09/drifter_rose.pngdrifter_rosehttps://submesoscale.org/wp-content/uploads/2017/09/drifter_deploy_pg_ad.jpgdrifter_deploy_PG_ADhttps://submesoscale.org/wp-content/uploads/2017/09/drifter_pete.jpgdrifter_pete2017-09-23T13:03:38+00:00monthlyhttps://submesoscale.org/2017/09/20/besties-in-the-dark/https://submesoscale.org/wp-content/uploads/2017/09/picture1.pngPicture1https://submesoscale.org/wp-content/uploads/2017/09/picture2.pngPicture2https://submesoscale.org/wp-content/uploads/2017/09/picture3.pngPicture32017-09-20T10:03:34+00:00monthlyhttps://submesoscale.org/2017/08/22/when-things-sink/2017-08-24T21:52:11+00:00monthlyhttps://submesoscale.org/2017/08/22/they-said-come-to-baja-they-said-it-would-be-warm/https://submesoscale.org/wp-content/uploads/2017/08/camrinbraun_baja_00958.jpgCamrinBraun_Baja_00958https://submesoscale.org/wp-content/uploads/2017/08/2017-05-26-18-01-35.jpg2017-05-26 18.01.35https://submesoscale.org/wp-content/uploads/2017/08/camrinbraun_baja_00822.jpgCamrinBraun_Baja_008222017-08-24T21:50:37+00:00monthlyhttps://submesoscale.org/2017/08/22/holy-mola/https://submesoscale.org/wp-content/uploads/2017/08/2016-09-19-15-07-45.jpg2016-09-19 15.07.45https://submesoscale.org/wp-content/uploads/2017/08/2016-09-19-15-07-43.jpg2016-09-19 15.07.43https://submesoscale.org/wp-content/uploads/2017/08/2016-09-15-16-58-43.jpg2016-09-15 16.58.43https://submesoscale.org/wp-content/uploads/2017/08/2016-09-15-17-11-00.jpg2016-09-15 17.11.002017-08-24T21:48:02+00:00monthlyhttps://submesoscale.org/2017/08/22/chumping-oregon/https://submesoscale.org/wp-content/uploads/2017/08/2017-07-21-09-32-06.jpg2017-07-21 09.32.06https://submesoscale.org/wp-content/uploads/2017/08/2017-07-22-08-31-14.jpg2017-07-22 08.31.14https://submesoscale.org/wp-content/uploads/2017/08/2017-07-22-08-31-22.jpg2017-07-22 08.31.222017-08-24T21:44:27+00:00monthlyhttps://submesoscale.org/projects/warm-core-rings-in-the-gulf-stream/2017-08-19T15:32:51+00:00weekly0.6https://submesoscale.org/projects/https://submesoscale.org/wp-content/uploads/2014/01/vertical_struct_with_nwra_figure.pngvertical_Struct_with_NWRA_figurehttps://submesoscale.org/wp-content/uploads/2015/08/001-2015-04slide450x240.jpg001-2015-04SLIDE450x240https://submesoscale.org/wp-content/uploads/2015/08/naames_banner_16.jpgnaames_banner_162017-08-19T00:10:17+00:00weekly0.6https://submesoscale.org/projects/influence-of-surface-mixing-layer-on-phytoplankton/2017-08-18T23:50:29+00:00weekly0.6https://submesoscale.org/projects/vertical-eddy-structure/2017-08-18T22:17:40+00:00weekly0.6https://submesoscale.org/projects/submesoscale-salinity-variability-at-fronts/2017-08-18T21:38:17+00:00weekly0.6https://submesoscale.org/projects/variability-in-phytoplankton-community-structure-and-diversity-from-underway-optics/2017-08-18T21:07:17+00:00weekly0.6https://submesoscale.org/captains-log/2017-08-17T00:28:12+00:00weekly0.6https://submesoscale.org/inthenews/emotion/https://submesoscale.org/wp-content/uploads/2015/12/primary_production.pngGulf Stream Eddies2017-07-01T17:25:47+00:00weekly0.6https://submesoscale.org/2015/10/29/preparations/https://submesoscale.org/wp-content/uploads/2015/10/atlantisbeautiful.jpgatlantisbeautifulhttps://submesoscale.org/wp-content/uploads/2015/10/naames_cruise1.pngNAAMES_cruiseThe planned expedition path overlaid on satellite estimate of the April mean climatological chlorophyll-a concentration. The NAAMES program time line is shown along the bottom of the gure with blue triangle indicating planned cruise dates.https://submesoscale.org/wp-content/uploads/2015/10/dsl_schematic.pngDSL_schematichttps://submesoscale.org/wp-content/uploads/2015/10/atlantis_main_en1_36169.jpgatlantis_main_en1_36169https://submesoscale.org/wp-content/uploads/2015/10/naames_cruise-e1446148958265.pngNAAMES_cruise2017-06-28T23:42:28+00:00monthlyhttps://submesoscale.org/2015/11/07/on-the-shelf/https://submesoscale.org/wp-content/uploads/2015/11/ifcb.pngifcbhttps://submesoscale.org/wp-content/uploads/2015/11/chogram.pngchogramhttps://submesoscale.org/wp-content/uploads/2015/11/eddy_map.pngeddy_mapMap of our cruise and track and eddies.2017-06-28T23:32:46+00:00monthlyhttps://submesoscale.org/2016/03/31/swirling-ecosystems-in-the-north-atlantic/https://submesoscale.org/wp-content/uploads/2016/03/v2016069-westernnorthatlantic-half_with_sla.pngV2016069.WesternNorthAtlantic.half_with_sla2017-06-28T23:07:47+00:00monthlyhttps://submesoscale.org/2015/11/17/our-bread-and-butter-measurement-the-ctd/2017-06-28T23:04:56+00:00monthlyhttps://submesoscale.org/2015/11/08/the-science-and-the-weather-ramp-up/2017-06-28T23:00:51+00:00monthlyhttps://submesoscale.org/2014/11/26/lydia-swims-100-miles-in-less-than-2-days-into-the-core-of-a-large-anticyclone/https://submesoscale.org/wp-content/uploads/2014/11/lydia_over_sla_11_261.pngLydia_over_SLA_11_26Lydia's track overlaid on a map of sea level anomaly. Anticyclonic eddies and meanders are shown as orange and red features, cyclonic eddies and meanders and blue and purple features.https://submesoscale.org/wp-content/uploads/2014/11/lydia_over_sla_11_26.pngLydia and SLA Nov 25-26, 2014Lydia's track overlaid on a map of sea level anomaly. Anticyclonic eddies and meanders are shown as orange and red features, cyclonic eddies and meanders and blue and purple features.2017-06-28T22:58:35+00:00monthlyhttps://submesoscale.org/2014/11/24/has-lydia-found-a-new-eddy/https://submesoscale.org/wp-content/uploads/2014/11/lydia_over_sla_11_24.pngLydia_over_SLA_11_24Lydia's track (starting 2017-06-28T22:55:00+00:00monthlyhttps://submesoscale.org/2016/07/13/what-did-we-learn/2016-07-14T03:13:16+00:00monthlyhttps://submesoscale.org/2016/05/04/sharks_with_sensors/2016-05-09T21:02:54+00:00monthlyhttps://submesoscale.org/projects/sharks_and_eddies/https://submesoscale.org/wp-content/uploads/2014/05/spot_tag.pngspot_tagFigure 1: Photo of a SPOT tag (upper most device) attached to the dorsal surface of white shark Mary Lee. Photo courtesy of <a href="http://ocearch.org" target="_blank">Ocearch.org</a>.https://submesoscale.org/wp-content/uploads/2014/05/03032013_ocearch_jacksonvillefl_robertsnow.jpg03032013_Ocearch_JacksonvilleFL_RobertSnowFigure 2: Photograph of white shark Lydia prior to release. Image courtesy of Ocearch.org.https://submesoscale.org/wp-content/uploads/2014/05/marylee_tags.jpgMaryLee_tagsFig 1: Photo of a SPOT tag (upper most device) attached to the dorsal surface of white shark Mary Lee. Photo courtesy of Ocearch.orghttps://submesoscale.org/wp-content/uploads/2014/05/lydia_td_and_ssh_examples.pngLydia_TD_and_SSH_examplesFigure 2: Temperature-Depth section collected by a pop-up archival tag (miniPAT) affixed to Lydia’s dorsal surface. The six panels above the section are snapshots of SSH overlaid with Lydia’s SPOT location estimates. Each of the panels is labeled as either an anticyclone, resulting in a downward displacement of isotherms in the temperature-depth section, or a cyclone, resulting in the shoaling of isotherms. The maximum depth of each dive is recorded as the transition from the pseudo-color image to white. Dives within anticyclones are always deeper than within cyclones.https://submesoscale.org/wp-content/uploads/2014/05/lydia_composites.pngLydia_compositesFigure 3: (a) The path of the ~900 kg. mature female white shark Lydia as recorded by a SPOT tag affixed to her dorsal fin, overlaid on a map of SSH for the week of 4 August, 2013. Anticyclonic eddies (positive SSH anomalies) are shown in red, cyclonic eddies (negative SSH anomalies) in blue to purple. Daily position estimates of Lydia when she occupied anticyclonic and cyclonic eddies are shown in panels (b) and (c), respectively. The histograms along the x and y axes display the distribution of observations and are not scaled relative to each other. The x and y axes in each panel have been scaled by the eddy radius scale L_s defined in the text. (d) Histograms of the number of daily SPOT locations per unit area of each radial annulus, as a function of radial distance from the closest eddy center. SPOT locations associated with anticyclones and cyclones are shown as red and blue stepped curves, respectively. The x axes has been scaled by the horizontal eddy radius scale L_s. The 95% confidence interval of each radial bin is shown by grey shading. Confidence intervals for the binomially distributed location counts were computed following Clopper and Pearson (1934). 2014-12-04T21:41:01+00:00weekly0.6https://submesoscale.orgdaily1.02020-07-29T20:43:39+00:00