{"id":3053,"date":"2024-06-27T21:44:59","date_gmt":"2024-06-27T21:44:59","guid":{"rendered":"https:\/\/www.marine.usf.edu\/comit\/?page_id=3053"},"modified":"2024-10-22T17:30:45","modified_gmt":"2024-10-22T17:30:45","slug":"forecasting-remote-sensing","status":"publish","type":"page","link":"https:\/\/www.marine.usf.edu\/comit\/forecasting-remote-sensing\/","title":{"rendered":"Forecasting &amp; Remote Sensing"},"content":{"rendered":"<p><div class=\"et_d4_element et_pb_section et_pb_section_0 et_animated et_pb_with_background  et_pb_css_mix_blend_mode et_section_regular et_block_section\" >\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_d4_element et_pb_row et_pb_row_0  et_pb_css_mix_blend_mode et_block_row\">\n\t\t\t\t<div class=\"et_d4_element et_pb_column_4_4 et_pb_column et_pb_column_0  et_pb_css_mix_blend_mode et-last-child et_block_column\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_module et_d4_element et_pb_text et_pb_text_0  et_pb_text_align_left et_pb_bg_layout_light\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_text_inner\"><h1>Themes and Activities<\/h1><\/div>\n\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div><div class=\"et_d4_element et_pb_section et_pb_section_1  et_pb_css_mix_blend_mode et_section_regular et_block_section\" >\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_d4_element et_pb_row et_pb_row_1  et_pb_css_mix_blend_mode et_block_row\">\n\t\t\t\t<div class=\"et_d4_element et_pb_column_4_4 et_pb_column et_pb_column_1  et_pb_css_mix_blend_mode et-last-child et_block_column\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_module et_d4_element et_pb_blurb et_pb_blurb_0  et_pb_text_align_center  et_pb_blurb_position_top et_block_module et_pb_bg_layout_light\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_blurb_content\">\n\t\t\t\t\t<div class=\"et_pb_main_blurb_image et_pb_css_mix_blend_mode\"><span class=\"et_pb_image_wrap\"><span class=\"et-waypoint et_pb_animation_top et_pb_animation_top_tablet et_pb_animation_top_phone et-pb-icon\">\uf108<\/span><\/span><\/div>\n\t\t\t\t\t<div class=\"et_pb_blurb_container\">\n\t\t\t\t\t\t<h1 class=\"et_pb_module_header\"><span>Forecasting & Remote Sensing<\/span><\/h1>\n\t\t\t\t\t\t\n\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div><div class=\"et_d4_element et_pb_row et_pb_row_2  et_pb_css_mix_blend_mode et_block_row\">\n\t\t\t\t<div class=\"et_d4_element et_pb_column_3_5 et_pb_column et_pb_column_2  et_pb_css_mix_blend_mode et_block_column\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_module et_d4_element et_pb_text et_pb_text_1  et_pb_text_align_left et_pb_bg_layout_light\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_text_inner\"><p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\"><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\"><\/span><\/p>\n<p style=\"text-align: justify;\"><strong><span style=\"font-size: large; color: #000000; font-family: Lato;\">Ocean circulation models <\/span><\/strong><span style=\"font-size: large;\"><span style=\"color: #000000; font-family: Lato;\">continue to be <strong>incredibly important<\/strong> for a number of applications from the open ocean to populated coastal areas. <\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large;\"><span style=\"color: #000000; font-family: Lato;\">The <strong>modeling team at COMIT<\/strong> is working on a number of improvements to their <strong>Tampa Bay Coastal Ocean Model (TBCOM)<\/strong> and <strong>West Florida Coastal Ocean Model (WFCOM)<\/strong>. This work has direct, immediate impact on nowcast and forecast products that a number of agencies and organizations rely upon on a daily basis.<\/span><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">Our modeling experts have also been working closely with the mapping experts on the COMIT team to <strong>improve<\/strong> upon and <strong>assess bathymetric and topographic influence on the coastal ocean circulation<\/strong>. <\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">Some of the current projects related to this theme are summarized below:<\/span><\/p><\/div>\n\t\t\t<\/div>\n\t\t\t<\/div><div class=\"et_d4_element et_pb_column_2_5 et_pb_column et_pb_column_3  et_pb_css_mix_blend_mode et-last-child et_block_column\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_module et_d4_element et_pb_image et_pb_image_0 et_pb_image_sticky\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<span class=\"et_pb_image_wrap \"><img loading=\"lazy\" decoding=\"async\" width=\"1702\" height=\"2560\" src=\"https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/ocean-buoy-comit-scaled.jpg\" alt=\"\" title=\"ocean-buoy-comit\" srcset=\"https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/ocean-buoy-comit-scaled.jpg 1702w, https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/ocean-buoy-comit-1280x1925.jpg 1280w, https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/ocean-buoy-comit-980x1474.jpg 980w, https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/ocean-buoy-comit-480x722.jpg 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) and (max-width: 1280px) 1280px, (min-width: 1281px) 1702px, 100vw\" class=\"wp-image-3061\" \/><\/span>\n\t\t\t<\/div><div class=\"et_pb_module et_d4_element et_pb_text et_pb_text_2  et_pb_text_align_left et_pb_bg_layout_light\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_text_inner\"><p style=\"text-align: center;\"><em><span style=\"color: #000000;\">Moored buoy platforms at the USF College of Marine Science waterfront<\/span><\/em><\/p><\/div>\n\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div><div class=\"et_d4_element et_pb_row et_pb_row_3  et_pb_css_mix_blend_mode et_block_row\">\n\t\t\t\t<div class=\"et_d4_element et_pb_column_4_4 et_pb_column et_pb_column_4  et_pb_css_mix_blend_mode et-last-child et_block_column\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<div class=\"et_pb_module et_d4_element et_pb_toggle et_pb_toggle_0 et_pb_toggle_item  et_pb_toggle_close\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<h2 class=\"et_pb_toggle_title\">WFCOM (Coastal Model) Improvements<\/h2>\n\t\t\t\t<div class=\"et_pb_toggle_content clearfix\"><p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato;\">The modeling team started working on <strong>modifying<\/strong> their <strong>West Florida Coastal Ocean Model<\/strong> (WFCOM) to <strong>leverage the Global HYCOM boundary forcing<\/strong> as opposed to the Gulf of Mexico HYCOM option. Decommissioning the use of the latter model was in response to its limited availability of boundary forcing.<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato;\">However - the Global HYCOM does not include any tidal components so this modification necessitated an enormous effort to successfully complete. The modeling team used a barotropic tidal model to generate tides which were subsequently incorporated into the WFCOM. The hard work paid off and the <strong>WFCOM, as well as the Tampa Bay Coastal Ocean Model (TBCOM), both resumed normal automated nowcast\/forecast runs<\/strong> as of late last year (2023).<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato;\"><strong>Model simulation results<\/strong> (including currents, temperature, and salinity, sea level, and particle trajectories <strong>are made <span style=\"text-decoration: underline;\"><a href=\"http:\/\/ocgweb.marine.usf.edu\" target=\"_blank\" rel=\"noopener\">publicly available on the web<\/a><\/span> as maps<\/strong>. These can be used immediately for quick reference of the circulation patterns.<\/span><\/p><\/div>\n\t\t\t<\/div><div class=\"et_pb_module et_d4_element et_pb_divider et_pb_divider_0 et_pb_space\"><div class=\"et_pb_divider_internal\"><\/div><\/div><div class=\"et_pb_module et_d4_element et_pb_toggle et_pb_toggle_1 et_pb_toggle_item  et_pb_toggle_close\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<h2 class=\"et_pb_toggle_title\">Impact of Bathymetry on Coastal Circulation<\/h2>\n\t\t\t\t<div class=\"et_pb_toggle_content clearfix\"><p style=\"text-align: justify;\"><span style=\"color: #000000; font-family: Lato; font-size: large;\">Due to their shallow nature, the circulation models developed for estuaries and coastal areas tend to be sensitive to bathymetric changes. To better quantify and understand the impact of bathymetric changes on sea level and current predictions in such environments, the modeling team used their TBCOM model to investigate <strong>how forcing at the mouth of Tampa Bay using existing bathymetry and bathymetry that had been purposefully altered affected hydrodynamic response<\/strong>.<\/span><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\"><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">The simulated sea level, amplitude and phase of the semi-diurnal tides, and associated currents were compared between the two experiments. <strong>Significant changes in water level (up to +\/-10 cm) and current velocities (up to 20 cm\/s) were found in the shallow peripheral areas<\/strong>.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">The results of this sensitivity test confirm that <strong>it is imperative to use accurate bathymetric data underpinning these models<\/strong> \u2013 meaning even if bathymetric data exist in a coastal area, unless it was collected relatively recently it may be sub-optimal.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">Not only is accurate bathymetry important for water level and currents, but the <strong>reliability of scalar variable estimates is diluted when water depths are incorrect<\/strong>. Thus, it is not possible to accurately assess salinity, or other ecologically important properties, if the underlying water depth itself is not accurately known.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; color: #000000; font-family: Lato; font-weight: normal;\">This collaborative work has been published as a peer-reviewed journal paper which provides further detail and discussion: Chen, J., Liu, Y., Weisberg, R. H., Murawski, S.A., Gilbert, S., Naar, D., Zheng, L., Hommeyer, M., Dietrick, C., Luther, M., Hapke, C., Meyers, E., Moghimi, S., Allen, C., Tang, L., Khazaei, B., Pe\u2019eri, S., &amp; Wang, P. (2023) Hydrodynamic response to bathymetric changes in Tampa Bay, Florida. Deep Sea Research II: Topical Studies in Oceanography, 212, 105344. https:\/\/doi.org\/10.1016\/j.dsr2.2023.105344.<\/span>\u00a0<\/p>\n<p style=\"text-align: justify;\">\n<figure style=\"text-align: center;\"><\/figure>\n<figure style=\"text-align: center;\"><\/figure>\n<figure style=\"text-align: center;\"><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/bathymetric-changes-coastal-ocean-circulation-comit.jpg\" width=\"521\" height=\"299\" alt=\"\" class=\"wp-image-3063 alignnone size-full\" style=\"display: block; margin-left: auto; margin-right: auto;\" srcset=\"https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/bathymetric-changes-coastal-ocean-circulation-comit.jpg 521w, https:\/\/www.marine.usf.edu\/comit\/wp-content\/uploads\/2024\/06\/bathymetric-changes-coastal-ocean-circulation-comit-480x275.jpg 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) 521px, 100vw\" \/><\/p>\n<p><em style=\"font-size: 14px;\"><span style=\"color: #000000; font-size: medium;\"><\/span><\/em><\/p>\n<p><em style=\"font-size: 14px;\"><span style=\"color: #000000; font-size: medium;\">Original Bathymetry (a), Altered Bathymetry (b), and the difference between the two datasets in meters (c)<\/span><\/em><\/p>\n<\/figure><\/div>\n\t\t\t<\/div><div class=\"et_pb_module et_d4_element et_pb_divider et_pb_divider_1 et_pb_space\"><div class=\"et_pb_divider_internal\"><\/div><\/div><div class=\"et_pb_module et_d4_element et_pb_toggle et_pb_toggle_2 et_pb_toggle_item  et_pb_toggle_close\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<h2 class=\"et_pb_toggle_title\">Nowcasts and Forecasts for Navigation<\/h2>\n\t\t\t\t<div class=\"et_pb_toggle_content clearfix\"><p style=\"text-align: justify;\"><span style=\"color: #000000; font-size: large; font-family: Lato; font-weight: normal;\"><strong>Precise sea level predictions increase the likelihood of safe vessel navigation<\/strong> and operation, especially in coastal and estuarine where mariners contend with shallow bathymetries, narrow channels, and other hazards.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"color: #000000; font-size: large; font-family: Lato; font-weight: normal;\">The modeling team behind the <a href=\"http:\/\/ocgweb.marine.usf.edu\/~tbm\/index_sealevel.html\">Tampa Bay Coastal Ocean Model (TBCOM)<\/a> are <strong>working with the <a href=\"https:\/\/www.porttb.com\/\">Tampa Bay Port Authority<\/a> to discuss integrating coastal ocean models<\/strong> into their workflow. <br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"color: #000000; font-size: large; font-family: Lato; font-weight: normal;\">To better understand what\u2019s needed to achieve this goal, our modeling team <strong>used TBCOM to simulate hindcast sea levels<\/strong> at five tide gauge locations around Tampa Bay, then <strong>compared these with simulations with actual observations<\/strong>. For the <strong>1-day and 2-day forecasts, there was excellent agreement<\/strong> in both the amplitude and phase at all five stations. The offsets between the forecast and observed sea levels only began to increase at the 3-day point due to deviations in forecasted and measured winds. Despite an increase in error by the 3-day mark, general agreement remained between forecasted and measured sea levels.<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"color: #000000; font-size: large; font-family: Lato; font-weight: normal;\">A full explanation of this work and discussion of its results are documented in the following peer-reviewed journal paper: Chen, J., Weisberg, R. H., Liu, Y., &amp; Zheng, L. (2023). Hillsborough bay inflow modification study: An application of the Tampa Bay Coastal Ocean Model. Estuarine, Coastal and Shelf Science, 281-108213. <a href=\"https:\/\/doi.org\/10.1016\/j.ecss.2023.108213\">https:\/\/doi.org\/10.1016\/j.ecss.2023.108213<\/a>.<\/span><\/p>\n<p><span style=\"color: #000000; font-size: large;\"><\/span><\/p><\/div>\n\t\t\t<\/div><div class=\"et_pb_module et_d4_element et_pb_divider et_pb_divider_2 et_pb_space\"><div class=\"et_pb_divider_internal\"><\/div><\/div><div class=\"et_pb_module et_d4_element et_pb_toggle et_pb_toggle_3 et_pb_toggle_item  et_pb_toggle_close\">\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t<h2 class=\"et_pb_toggle_title\">Improved Storm Surge Simulations<\/h2>\n\t\t\t\t<div class=\"et_pb_toggle_content clearfix\"><p style=\"text-align: left;\"><strong><em><span style=\"font-size: large; font-family: Lato; color: #000000;\">Storm surge simulations based on an \u201cIan-like\u201d hurricane<\/span><\/em><\/strong><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">NOAA uses the Sea, Lake and Overland Surges from Hurricanes (SLOSH) model to provide storm surge guidance for all U.S. coastal regions. SLOSH generally performs very well but its storm surge <strong>results tend towards the \"worst-case\" scenario and typically do not provide specific information about the landfall location.<\/strong><br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">Hurricane Ian made landfall near Ft. Myers, Florida as a Category 4 storm on September 28, 2022. It was the deadliest hurricane to strike the State of Florida since the 1935 Labor Day hurricane and caused enormous economic losses. <strong>The <a href=\"http:\/\/ocgweb.marine.usf.edu\/~tbm\/index.html\">TBCOM nowcast\/forecast system<\/a> successfully predicted the sea level evolution within Tampa Bay during this period.<\/strong> Being that Ian was first expected to strike near Tampa Bay, our researchers wanted to address the question of <strong>what may have happened had Ian not altered its course.<\/strong> This question was explored using <a href=\"http:\/\/ocgweb.marine.usf.edu\/~tbm\/index_sealevel.html\">TBCOM<\/a> with Ian's path translated northwest from its actual path, forcing landfall in Tampa Bay region. <\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">Numerical experiments with a modified Ian path suggest that there would have been substantial coastal inundation over the low-lying areas of the Tampa Bay vicinity.<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">This work is ongoing and will be completed in late-2024.<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\"><\/span><\/p>\n<p style=\"text-align: left;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\"><strong><em>TBCOM-Flooding Hindcast: Hurricane Idalia Storm Surge<\/em><\/strong><br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">In the Tampa Bay area, <strong>the threat of inundation during hurricanes is a significant concern<\/strong> due to the region's low-lying topography. Though it did not make direct landfall, Hurricane Idalia recently led to the highest recorded water levels in the Tampa Bay area. This resulted in flooding in low-lying waterfront areas, primarily caused by the storm surge. <strong>The modeling team is using the data from this weather event to expand the TBCOM model grid to land area and build a new TBCOM-flooding model.<\/strong><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\">This work is ongoing and will be completed in late-2024.<br \/><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: large; font-family: Lato; font-weight: normal; color: #000000;\"><\/span><\/p><\/div>\n\t\t\t<\/div>\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div>\n\t\t\t\t\n\t\t\t\t\n\t\t\t<\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"om_disable_all_campaigns":false,"_exactmetrics_skip_tracking":false,"_monsterinsights_skip_tracking":false,"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-3053","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 5.0.2 - aioseo.com -->\n\t<meta name=\"description\" content=\"Themes and Activities \uf108 Forecasting &amp; Remote Sensing Ocean circulation models continue to be incredibly important for a number of applications from the open ocean to populated coastal areas. 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