{"id":3588,"date":"2026-08-12T19:56:09","date_gmt":"2026-08-12T19:56:09","guid":{"rendered":"https:\/\/www.marine.usf.edu\/comit\/?p=3588"},"modified":"2026-08-12T19:56:13","modified_gmt":"2026-08-12T19:56:13","slug":"offshore-sea-levels-measured-with-an-anchored-spar-buoy-system-using-gps-interferometric-reflectometry","status":"publish","type":"post","link":"https:\/\/www.marine.usf.edu\/comit\/2026\/08\/12\/offshore-sea-levels-measured-with-an-anchored-spar-buoy-system-using-gps-interferometric-reflectometry\/","title":{"rendered":"Offshore Sea Levels Measured with an Anchored Spar-Buoy System Using GPS Interferometric Reflectometry"},"content":{"rendered":"\n

Xie, S., Chen, J., Dixon, T. H., Weisberg, R. H., Zumberge, M. A. 2021. JGR Oceans<\/em>, 126, 11. https:\/\/doi.org\/10.1029\/2021JC017734<\/a><\/p>\n\n\n\n

Abstract: <\/strong>Conventional tide gauges are usually housed along the coast. Satellite altimetry works well in the open ocean but poorly near the coast due to signal contamination by land returns. These limitations lead to an observational gap in the transition zone between the coast and open ocean. Using data collected by a GPS installed on top of an anchored spar-buoy in Tampa Bay, we retrieved water levels through a combination of precise positioning and interferometric reflectometry. Individual water level retrievals agree with a nearby acoustic tide gauge (19.5 km distance) at \u223c15 cm level. Amplitude and phase of the major tidal constituents are well recovered by the GPS spar-buoy measurements. Over a 2.9-year period, agreement of de-tided daily mean sea levels measured by the GPS spar-buoy and the nearby acoustic tide gauge is 4.4 cm. When sea level data measured by the GPS spar-buoy are included in the local coastal ocean circulation model, low-frequency error propagated from the open boundary is significantly reduced.<\/p>\n\n\n\n

Download PDF<\/a><\/p>\n\n\n\n

<\/p>\n","protected":false},"excerpt":{"rendered":"

Xie, S., Chen, J., Dixon, T. H., Weisberg, R. H., Zumberge, M. A. 2021. JGR Oceans, 126, 11. https:\/\/doi.org\/10.1029\/2021JC017734 Abstract: Conventional tide gauges are usually housed along the coast. Satellite altimetry works well in the open ocean but poorly near the coast due to signal contamination by land returns. These limitations lead to an observational […]<\/p>\n","protected":false},"author":41,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_et_pb_use_builder":"off","_et_pb_old_content":"","_et_gb_content_width":"","om_disable_all_campaigns":false,"_exactmetrics_skip_tracking":false,"_monsterinsights_skip_tracking":false,"footnotes":""},"categories":[121],"tags":[135],"class_list":["post-3588","post","type-post","status-publish","format-standard","hentry","category-publications","tag-135"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t