Autonomous sampling of ocean submesoscale fronts with ocean gliders and numerical model forecasting. Flexas, M. M., Troesch, M. I., Chien, S., Thompson, A. F., Chu, S., Branch, A., Farrara, J. D., & Chao, Y. Journal of Atmospheric and Oceanic Technology, March, 2018. abstract bibtex Submesoscale fronts arising from mesoscale stirring are ubiquitous in the ocean and have a strong impact on upper-ocean dynamics. This work presents a method for optimizing the sampling of ocean fronts with autonomous vehicles at meso- and submesoscales, based on a combination of numerical forecast and autonomous planning. This method uses a 48-h forecast from a real-time high-resolution data-assimilative primitive equation ocean model, feature detection techniques, and a planner that controls the observing platform. The method is tested in Monterey Bay, off the coast of California, during a 9-day experiment focused on sampling subsurface thermohaline-compensated structures using a Seaglider as the ocean observing platform. Based on model estimations, the sampling "gain," defined as the magnitude of isopycnal tracer variability sampled, is 50 percent larger in the feature-chasing case with respect to a non-feature-tracking scenario. The ability of the model to reproduce, in space and time, thermohaline submesoscale features is evaluated by quantitatively comparing the model and glider results. The model reproduces the vertical ( 50-200 m thick) and lateral ( 5-20 km) scales of subsurface subducting fronts and near-bottom features observed in the glider data. The differences between model and glider data are, in part, attributed to the selected glider optimal interpolation parameters and to uncertainties in the forecasting of the location of the structures. This method can be exported to any place in the ocean where high-resolution data-assimilative model output is available, and it allows for the incorporation of multiple observing platforms.
@article{flexas-glider-jtech-2018,
title = {Autonomous sampling of ocean submesoscale fronts with ocean gliders and numerical model forecasting},
author = {M. M. Flexas and M. I. Troesch and S. Chien and A. F. Thompson and S. Chu and A. Branch and J. D. Farrara and Y. Chao},
year = 2018,
month = {March},
journal = {Journal of Atmospheric and Oceanic Technology},
volume = {35 (3)},
abstract = {Submesoscale fronts arising from mesoscale stirring are ubiquitous in the ocean and have a strong impact on upper-ocean dynamics. This work presents a method for optimizing the sampling of ocean fronts with autonomous vehicles at meso- and submesoscales, based on a combination of numerical forecast and autonomous planning. This method uses a 48-h forecast from a real-time high-resolution data-assimilative primitive equation ocean model, feature detection techniques, and a planner that controls the observing platform. The method is tested in Monterey Bay, off the coast of California, during a 9-day experiment focused on sampling subsurface thermohaline-compensated structures using a Seaglider as the ocean observing platform. Based on model estimations, the sampling "gain," defined as the magnitude of isopycnal tracer variability sampled, is 50 percent larger in the feature-chasing case with respect to a non-feature-tracking scenario. The ability of the model to reproduce, in space and time, thermohaline submesoscale features is evaluated by quantitatively comparing the model and glider results. The model reproduces the vertical (~50-200 m thick) and lateral (~5-20 km) scales of subsurface subducting fronts and near-bottom features observed in the glider data. The differences between model and glider data are, in part, attributed to the selected glider optimal interpolation parameters and to uncertainties in the forecasting of the location of the structures. This method can be exported to any place in the ocean where high-resolution data-assimilative model output is available, and it allows for the incorporation of multiple observing platforms.},
project = {keck\_marine}
}
Downloads: 0
{"_id":"pzrsDP8wmiTx8NhNN","bibbaseid":"flexas-troesch-chien-thompson-chu-branch-farrara-chao-autonomoussamplingofoceansubmesoscalefrontswithoceanglidersandnumericalmodelforecasting-2018","author_short":["Flexas, M. M.","Troesch, M. I.","Chien, S.","Thompson, A. F.","Chu, S.","Branch, A.","Farrara, J. D.","Chao, Y."],"bibdata":{"bibtype":"article","type":"article","title":"Autonomous sampling of ocean submesoscale fronts with ocean gliders and numerical model forecasting","author":[{"firstnames":["M.","M."],"propositions":[],"lastnames":["Flexas"],"suffixes":[]},{"firstnames":["M.","I."],"propositions":[],"lastnames":["Troesch"],"suffixes":[]},{"firstnames":["S."],"propositions":[],"lastnames":["Chien"],"suffixes":[]},{"firstnames":["A.","F."],"propositions":[],"lastnames":["Thompson"],"suffixes":[]},{"firstnames":["S."],"propositions":[],"lastnames":["Chu"],"suffixes":[]},{"firstnames":["A."],"propositions":[],"lastnames":["Branch"],"suffixes":[]},{"firstnames":["J.","D."],"propositions":[],"lastnames":["Farrara"],"suffixes":[]},{"firstnames":["Y."],"propositions":[],"lastnames":["Chao"],"suffixes":[]}],"year":"2018","month":"March","journal":"Journal of Atmospheric and Oceanic Technology","volume":"35 (3)","abstract":"Submesoscale fronts arising from mesoscale stirring are ubiquitous in the ocean and have a strong impact on upper-ocean dynamics. This work presents a method for optimizing the sampling of ocean fronts with autonomous vehicles at meso- and submesoscales, based on a combination of numerical forecast and autonomous planning. This method uses a 48-h forecast from a real-time high-resolution data-assimilative primitive equation ocean model, feature detection techniques, and a planner that controls the observing platform. The method is tested in Monterey Bay, off the coast of California, during a 9-day experiment focused on sampling subsurface thermohaline-compensated structures using a Seaglider as the ocean observing platform. Based on model estimations, the sampling \"gain,\" defined as the magnitude of isopycnal tracer variability sampled, is 50 percent larger in the feature-chasing case with respect to a non-feature-tracking scenario. The ability of the model to reproduce, in space and time, thermohaline submesoscale features is evaluated by quantitatively comparing the model and glider results. The model reproduces the vertical ( 50-200 m thick) and lateral ( 5-20 km) scales of subsurface subducting fronts and near-bottom features observed in the glider data. The differences between model and glider data are, in part, attributed to the selected glider optimal interpolation parameters and to uncertainties in the forecasting of the location of the structures. This method can be exported to any place in the ocean where high-resolution data-assimilative model output is available, and it allows for the incorporation of multiple observing platforms.","project":"keck_marine","bibtex":"@article{flexas-glider-jtech-2018,\n\ttitle = {Autonomous sampling of ocean submesoscale fronts with ocean gliders and numerical model forecasting},\n\tauthor = {M. M. Flexas and M. I. Troesch and S. Chien and A. F. Thompson and S. Chu and A. Branch and J. D. Farrara and Y. Chao},\n\tyear = 2018,\n\tmonth = {March},\n\tjournal = {Journal of Atmospheric and Oceanic Technology},\n\tvolume = {35 (3)},\n\tabstract = {Submesoscale fronts arising from mesoscale stirring are ubiquitous in the ocean and have a strong impact on upper-ocean dynamics. This work presents a method for optimizing the sampling of ocean fronts with autonomous vehicles at meso- and submesoscales, based on a combination of numerical forecast and autonomous planning. This method uses a 48-h forecast from a real-time high-resolution data-assimilative primitive equation ocean model, feature detection techniques, and a planner that controls the observing platform. The method is tested in Monterey Bay, off the coast of California, during a 9-day experiment focused on sampling subsurface thermohaline-compensated structures using a Seaglider as the ocean observing platform. Based on model estimations, the sampling \"gain,\" defined as the magnitude of isopycnal tracer variability sampled, is 50 percent larger in the feature-chasing case with respect to a non-feature-tracking scenario. The ability of the model to reproduce, in space and time, thermohaline submesoscale features is evaluated by quantitatively comparing the model and glider results. The model reproduces the vertical (~50-200 m thick) and lateral (~5-20 km) scales of subsurface subducting fronts and near-bottom features observed in the glider data. The differences between model and glider data are, in part, attributed to the selected glider optimal interpolation parameters and to uncertainties in the forecasting of the location of the structures. This method can be exported to any place in the ocean where high-resolution data-assimilative model output is available, and it allows for the incorporation of multiple observing platforms.},\n\tproject = {keck\\_marine}\n}\n","author_short":["Flexas, M. M.","Troesch, M. I.","Chien, S.","Thompson, A. F.","Chu, S.","Branch, A.","Farrara, J. D.","Chao, Y."],"key":"flexas-glider-jtech-2018","id":"flexas-glider-jtech-2018","bibbaseid":"flexas-troesch-chien-thompson-chu-branch-farrara-chao-autonomoussamplingofoceansubmesoscalefrontswithoceanglidersandnumericalmodelforecasting-2018","role":"author","urls":{},"metadata":{"authorlinks":{}}},"bibtype":"article","biburl":"http://ai.jpl.nasa.gov/public/publications/jpl_aig.bib","dataSources":["fFKv7kkLuCZPtfsiH","QvdbtaigAhR3B2gH3","gKzW9rEearQxTm7ht"],"keywords":[],"search_terms":["autonomous","sampling","ocean","submesoscale","fronts","ocean","gliders","numerical","model","forecasting","flexas","troesch","chien","thompson","chu","branch","farrara","chao"],"title":"Autonomous sampling of ocean submesoscale fronts with ocean gliders and numerical model forecasting","year":2018}