9129767 RPFKFUG7 1 apa 50 date desc year Vazquez, H. J. 18 https://hvazquezperalta.scrippsprofiles.ucsd.edu/wp-content/plugins/zotpress/
%7B%22status%22%3A%22success%22%2C%22updateneeded%22%3Afalse%2C%22instance%22%3Afalse%2C%22meta%22%3A%7B%22request_last%22%3A0%2C%22request_next%22%3A0%2C%22used_cache%22%3Atrue%7D%2C%22data%22%3A%5B%7B%22key%22%3A%22NMC63K6G%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Vazquez%20et%20al.%22%2C%22parsedDate%22%3A%222023-10-01%22%2C%22numChildren%22%3A0%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Cornuelle%2C%20B.%20D.%2C%20Worcester%2C%20P.%20F.%2C%20Dzieciuch%2C%20M.%20A.%2C%20Colosi%2C%20J.%20A.%2C%20%26amp%3B%20Nash%2C%20J.%20D.%20%282023%29.%20Using%20long-range%20transmissions%20in%20the%20Beaufort%20Gyre%20to%20test%20the%20sound-speed%20equation%20at%20high%20pressure%20and%20low%20temperature.%20%3Ci%3EThe%20Journal%20of%20the%20Acoustical%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E154%3C%5C%2Fi%3E%284%29%2C%202676%26%23x2013%3B2688.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0021973%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0021973%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Using%20long-range%20transmissions%20in%20the%20Beaufort%20Gyre%20to%20test%20the%20sound-speed%20equation%20at%20high%20pressure%20and%20low%20temperature%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Heriberto%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Bruce%20D.%22%2C%22lastName%22%3A%22Cornuelle%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Peter%20F.%22%2C%22lastName%22%3A%22Worcester%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Matthew%20A.%22%2C%22lastName%22%3A%22Dzieciuch%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22John%20A.%22%2C%22lastName%22%3A%22Colosi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Jonathan%20D.%22%2C%22lastName%22%3A%22Nash%22%7D%5D%2C%22abstractNote%22%3A%22An%20ocean%20acoustic%20tomography%20array%20with%20a%20radius%20of%20150%5Cu2009km%20was%20deployed%20in%20the%20central%20Beaufort%20Gyre%20during%202016%5Cu20132017%20for%20the%20Canada%20Basin%20Acoustic%20Propagation%20Experiment.%20Five%20250-Hz%20transceivers%20were%20deployed%20in%20a%20pentagon%2C%20with%20a%20sixth%20transceiver%20at%20the%20center.%20A%20long%20vertical%20receiving%20array%20was%20located%20northwest%20of%20the%20central%20mooring.%20Travel-time%20anomalies%20for%20refracted-surface-reflected%20acoustic%20ray%20paths%20were%20calculated%20relative%20to%20travel%20times%20computed%20for%20a%20range-dependent%20sound-speed%20field%20from%20in%20situ%20temperature%20and%20salinity%20observations.%20Travel-time%20inversions%20for%20the%20three-dimensional%20sound-speed%20field%20consistent%20with%20the%20uncertainties%20in%20travel%20time%20%5B%5Cu223c2%5Cu2009ms%20root%20mean%20square%20%28rms%29%5D%2C%20receiver%20and%20source%20positions%20%28%5Cu223c%203%5Cu2009m%20rms%29%2C%20and%20sound%20speed%20calculated%20from%20conductivity-temperature-depth%20casts%20could%20not%20be%20obtained%20without%20introducing%20a%20deep%20sound-speed%20bias%20%28below%201000%5Cu2009m%29.%20Because%20of%20the%20precise%20nature%20of%20the%20travel-time%20observations%20with%20low%20mesoscale%20and%20internal%20wave%20variability%2C%20the%20conclusion%20is%20that%20the%20internationally%20accepted%20sound-speed%20equation%20%28TEOS-10%29%20gives%20values%20at%20high%20pressure%20%28greater%20than%201000%5Cu2009m%29%20and%20low%20temperature%20%28less%20than%200%5Cu2009%5Cu00b0C%29%20that%20are%20too%20high%20by%200.14%5Cu20130.16%20m%20s%5Cu22121.%22%2C%22date%22%3A%222023-10-01%22%2C%22language%22%3A%22en%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0021973%22%2C%22ISSN%22%3A%220001-4966%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fpubs.aip.org%5C%2Fjasa%5C%2Farticle%5C%2F154%5C%2F4%5C%2F2676%5C%2F2918391%5C%2FUsing-long-range-transmissions-in-the-Beaufort%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22TFFGCZNI%22%2C%22NBZ3B7BX%22%2C%22HI6QAUXX%22%5D%2C%22dateModified%22%3A%222023-12-01T19%3A32%3A40Z%22%7D%7D%2C%7B%22key%22%3A%22AAF6G8AV%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Worcester%20et%20al.%22%2C%22parsedDate%22%3A%222023-05-01%22%2C%22numChildren%22%3A0%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EWorcester%2C%20P.%20F.%2C%20Dzieciuch%2C%20M.%20A.%2C%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Cornuelle%2C%20B.%20D.%2C%20Colosi%2C%20J.%20A.%2C%20Krishfield%2C%20R.%20A.%2C%20%26amp%3B%20Kemp%2C%20J.%20N.%20%282023%29.%20Acoustic%20travel-time%20variability%20observed%20on%20a%20150-km%20radius%20tomographic%20array%20in%20the%20Canada%20Basin%20during%202016%26%23x2013%3B2017.%20%3Ci%3EThe%20Journal%20of%20the%20Acoustical%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E153%3C%5C%2Fi%3E%285%29%2C%202621.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0019304%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0019304%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Acoustic%20travel-time%20variability%20observed%20on%20a%20150-km%20radius%20tomographic%20array%20in%20the%20Canada%20Basin%20during%202016%5Cu20132017%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Peter%20F.%22%2C%22lastName%22%3A%22Worcester%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Matthew%20A.%22%2C%22lastName%22%3A%22Dzieciuch%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Heriberto%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Bruce%20D.%22%2C%22lastName%22%3A%22Cornuelle%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22John%20A.%22%2C%22lastName%22%3A%22Colosi%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Richard%20A.%22%2C%22lastName%22%3A%22Krishfield%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22John%20N.%22%2C%22lastName%22%3A%22Kemp%22%7D%5D%2C%22abstractNote%22%3A%22The%20Arctic%20Ocean%20is%20undergoing%20dramatic%20changes%20in%20response%20to%20increasing%20atmospheric%20concentrations%20of%20greenhouse%20gases.%20The%202016%5Cu20132017%20Canada%20Basin%20Acoustic%20Propagation%20Experiment%20was%20conducted%20to%20assess%20the%20effects%20of%20the%20changes%20in%20the%20sea%20ice%20and%20ocean%20structure%20in%20the%20Beaufort%20Gyre%20on%20low-frequency%20underwater%20acoustic%20propagation%20and%20ambient%20sound.%20An%20ocean%20acoustic%20tomography%20array%20with%20a%20radius%20of%20150%5Cu2009km%20that%20consisted%20of%20six%20acoustic%20transceivers%20and%20a%20long%20vertical%20receiving%20array%20measured%20the%20impulse%20responses%20of%20the%20ocean%20at%20a%20variety%20of%20ranges%20every%20four%20hours%20using%20broadband%20signals%20centered%20at%20about%20250%5Cu2009Hz.%20The%20peak-to-peak%20low-frequency%20travel-time%20variability%20of%20the%20early%2C%20resolved%20ray%20arrivals%20that%20turn%20deep%20in%20the%20ocean%20was%20only%20a%20few%20tens%20of%20milliseconds%2C%20roughly%20an%20order%20of%20magnitude%20smaller%20than%20observed%20in%20previous%20tomographic%20experiments%20at%20similar%20ranges%2C%20reflecting%20the%20small%20spatial%20scale%20and%20relative%20sparseness%20of%20mesoscale%20eddies%20in%20the%20Canada%20Basin.%20The%20high-frequency%20travel-time%20fluctuations%20were%20approximately%202%5Cu2009ms%20root-mean-square%2C%20roughly%20comparable%20to%20the%20expected%20measurement%20uncertainty%2C%20reflecting%20the%20low%20internal-wave%20energy%20level.%20The%20travel-time%20spectra%20show%20increasing%20energy%20at%20lower%20frequencies%20and%20enhanced%20semidiurnal%20variability%2C%20presumably%20due%20to%20some%20combination%20of%20the%20semidiurnal%20tides%20and%20inertial%20variability.%22%2C%22date%22%3A%222023-05-01%22%2C%22language%22%3A%22en%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0019304%22%2C%22ISSN%22%3A%220001-4966%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fpubs.aip.org%5C%2Fjasa%5C%2Farticle%5C%2F153%5C%2F5%5C%2F2621%5C%2F2887952%5C%2FAcoustic-travel-time-variability-observed-on-a-150%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22TFFGCZNI%22%2C%22NBZ3B7BX%22%2C%22HI6QAUXX%22%5D%2C%22dateModified%22%3A%222023-06-16T22%3A04%3A35Z%22%7D%7D%2C%7B%22key%22%3A%22QYE3GRSX%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Vazquez%20et%20al.%22%2C%22parsedDate%22%3A%222023%22%2C%22numChildren%22%3A0%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Gopalakrishnan%2C%20G.%2C%20%26amp%3B%20Sheinbaum%2C%20J.%20%282023%29.%20Impact%20of%20Yucatan%20Channel%20Subsurface%20Velocity%20Observations%20on%20the%20Gulf%20of%20Mexico%20State%20Estimates.%20%3Ci%3EJournal%20of%20Physical%20Oceanography%3C%5C%2Fi%3E%2C%20%3Ci%3E53%3C%5C%2Fi%3E%281%29%2C%20361%26%23x2013%3B385.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1175%5C%2FJPO-D-21-0213.1%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1175%5C%2FJPO-D-21-0213.1%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Impact%20of%20Yucatan%20Channel%20Subsurface%20Velocity%20Observations%20on%20the%20Gulf%20of%20Mexico%20State%20Estimates%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Heriberto%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Ganesh%22%2C%22lastName%22%3A%22Gopalakrishnan%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Julio%22%2C%22lastName%22%3A%22Sheinbaum%22%7D%5D%2C%22abstractNote%22%3A%22Abstract%5Cn%20%20%20%20%20%20%20%20%20%20%20%20The%20Gulf%20of%20Mexico%20%28GoM%29%20surface%20circulation%20variability%20is%20dominated%20by%20the%20Loop%20Current%20%28LC%29%20and%20the%20episodically%20released%20anticyclonic%20Loop%20Current%20eddies%20%28LCEs%29.%20The%20Yucatan%20Current%20feeds%20the%20LC%20through%20the%20Yucatan%20Channel%20%28YC%29%2C%20and%20its%20flow%20structure%20at%20the%20YC%20is%20hypothesized%20to%20affect%20the%20LC%20evolution%20critically.%20This%20study%20examines%20the%20impact%20of%20assimilating%20YC%20subsurface%20velocity%20observations%20from%20a%20tall%20mooring%20array%20across%20the%20YC%20on%20the%20GoM%20circulation.%20State%20estimates%20and%20forecasts%20of%20the%20LC%20circulation%20were%20produced%20using%20a%20regional%20implementation%20of%20the%20Massachusetts%20Institute%20of%20Technology%20general%20circulation%20model%20%28MITgcm%29%20and%20its%20adjoint-based%20four-dimensional%20variational%20%284DVAR%29%20assimilation%20system.%20The%20estimates%20were%20constrained%20by%20combinations%20of%20the%20YC%20observations%20and%20satellite-derived%20sea%20surface%20height%20%28SSH%29%20and%20sea%20surface%20temperature%20%28SST%29.%20The%20results%20show%20that%20assimilation%20of%20both%20moored%20and%20satellite%20data%20improves%20the%20model%20hindcasts%20and%20forecasts%20for%20all%20LC%20phases.%20Additionally%2C%20one%20realization%20of%20the%20state%20estimate%20that%20assimilates%20only%20moored%20data%20matches%20the%20LCE%20detachment%20timing%20with%20that%20of%20AVISO%20SSH.%20Observations%20from%20the%20moorings%20close%20to%20the%20Yucatan%20Peninsula%20significantly%20impact%20the%20LCE%20detachment.%20A%20finite-time%20Lyapunov%20exponent%20analysis%20reveals%20the%20differences%20among%20the%20assimilation%20experiments%2C%20such%20as%20eddylike%20structures%20intruding%20into%20the%20GoM%20through%20the%20YC%2C%20and%20its%20relation%20to%20the%20typical%20LC%20sudden%20growth.%20Finally%2C%20an%20adjoint%20sensitivity%20analysis%20is%20used%20to%20verify%20the%20dynamic%20link%20between%20the%20LC%20extension%20and%20the%20intrusion%20of%20eddylike%20structures%20into%20the%20GoM.%22%2C%22date%22%3A%2201%5C%2F2023%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.1175%5C%2FJPO-D-21-0213.1%22%2C%22ISSN%22%3A%220022-3670%2C%201520-0485%22%2C%22url%22%3A%22https%3A%5C%2F%5C%2Fjournals.ametsoc.org%5C%2Fview%5C%2Fjournals%5C%2Fphoc%5C%2F53%5C%2F1%5C%2FJPO-D-21-0213.1.xml%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22784978NX%22%5D%2C%22dateModified%22%3A%222023-03-20T15%3A33%3A22Z%22%7D%7D%2C%7B%22key%22%3A%22XVATGSEU%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Gemba%20et%20al.%22%2C%22parsedDate%22%3A%222022-02-01%22%2C%22numChildren%22%3A5%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EGemba%2C%20K.%20L.%2C%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Sarkar%2C%20J.%2C%20Tippman%2C%20J.%20D.%2C%20Cornuelle%2C%20B.%2C%20Hodgkiss%2C%20W.%20S.%2C%20%26amp%3B%20Kuperman%2C%20W.%20A.%20%282022%29.%20Moving%20source%20ocean%20acoustic%20tomography%20with%20uncertainty%20quantification%20using%20controlled%20source-tow%20observations.%20%3Ci%3EThe%20Journal%20of%20the%20Acoustical%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E151%3C%5C%2Fi%3E%282%29%2C%20861%26%23x2013%3B880.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0009268%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0009268%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Moving%20source%20ocean%20acoustic%20tomography%20with%20uncertainty%20quantification%20using%20controlled%20source-tow%20observations%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Kay%20L.%22%2C%22lastName%22%3A%22Gemba%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Heriberto%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Jit%22%2C%22lastName%22%3A%22Sarkar%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Jeffrey%20D.%22%2C%22lastName%22%3A%22Tippman%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Bruce%22%2C%22lastName%22%3A%22Cornuelle%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22William%20S.%22%2C%22lastName%22%3A%22Hodgkiss%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22W.%20A.%22%2C%22lastName%22%3A%22Kuperman%22%7D%5D%2C%22abstractNote%22%3A%22%22%2C%22date%22%3A%222022%5C%2F02%5C%2F01%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0009268%22%2C%22ISSN%22%3A%220001-4966%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22TFFGCZNI%22%2C%22H66LIWM4%22%2C%222AQ2ECNM%22%5D%2C%22dateModified%22%3A%222022-10-20T15%3A51%3A54Z%22%7D%7D%2C%7B%22key%22%3A%22HWE6JQSC%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Durofchalk%20et%20al.%22%2C%22parsedDate%22%3A%222021-12%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EDurofchalk%2C%20N.%20C.%2C%20Jin%2C%20J.%20H.%2C%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Gemba%2C%20K.%20L.%2C%20Romberg%2C%20J.%2C%20%26amp%3B%20Sabra%2C%20K.%20G.%20%282021%29.%20Data%20driven%20source%20localization%20using%20a%20library%20of%20nearby%20shipping%20sources%20of%20opportunity.%20%3Ci%3EJASA%20Express%20Letters%3C%5C%2Fi%3E%2C%20%3Ci%3E1%3C%5C%2Fi%3E%2812%29%2C%207.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0009083%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0009083%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Data%20driven%20source%20localization%20using%20a%20library%20of%20nearby%20shipping%20sources%20of%20opportunity%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22N.%20C.%22%2C%22lastName%22%3A%22Durofchalk%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%20H.%22%2C%22lastName%22%3A%22Jin%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20L.%22%2C%22lastName%22%3A%22Gemba%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%22%2C%22lastName%22%3A%22Romberg%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20G.%22%2C%22lastName%22%3A%22Sabra%22%7D%5D%2C%22abstractNote%22%3A%22A%20library%20of%20broadband%20%28100-1000%20Hz%29%20channel%20impulse%20responses%20%28CIRs%29%20estimated%20between%20a%20short%20bottom-mounted%20vertical%20line%20array%20%28VLA%29%20in%20the%20Santa%20Barbara%20channel%20and%20selected%20locations%20along%20the%20tracks%20of%2027%20isolated%20transiting%20ships%2C%20cumulated%20over%20nine%20days%2C%20is%20constructed%20using%20the%20ray-based%20blind%20deconvolution%20algorithm.%20Treating%20this%20CIR%20library%20either%20as%20data-derived%20replica%20for%20broadband%20matched-field%20processing%20%28MFP%29%20or%20training%20data%20for%20machine%20learning%20yields%20comparable%20ranging%20accuracy%20%28%26%20SIM%3B50%20m%29%20for%20nearby%20vessels%20up%20to%203.2%20km%20for%20both%20methods.%20Using%20model-based%20replica%20of%20the%20direct%20path%20only%20computed%20for%20an%20average%20sound-speed%20profile%20comparatively%20yields%20%26%20SIM%3B110%20m%20ranging%20accuracy.%22%2C%22date%22%3A%222021%5C%2F12%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0009083%22%2C%22ISSN%22%3A%22%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222022-02-28T17%3A24%3A37Z%22%7D%7D%2C%7B%22key%22%3A%22HN3QB9IH%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Gemba%20et%20al.%22%2C%22parsedDate%22%3A%222021-10%22%2C%22numChildren%22%3A6%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EGemba%2C%20K.%20L.%2C%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Fialkowski%2C%20J.%2C%20Edelmann%2C%20G.%20F.%2C%20Dzieciuch%2C%20M.%20A.%2C%20%26amp%3B%20Hodgkiss%2C%20W.%20S.%20%282021%29.%20A%20performance%20comparison%20between%20m-sequences%20and%20linear%20frequency-modulated%20sweeps%20for%20the%20estimation%20of%20travel-time%20with%20a%20moving%20source.%20%3Ci%3EJournal%20of%20the%20Acoustical%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E150%3C%5C%2Fi%3E%284%29%2C%202613%26%23x2013%3B2623.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0006656%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0006656%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22A%20performance%20comparison%20between%20m-sequences%20and%20linear%20frequency-modulated%20sweeps%20for%20the%20estimation%20of%20travel-time%20with%20a%20moving%20source%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22K.%20L.%22%2C%22lastName%22%3A%22Gemba%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%22%2C%22lastName%22%3A%22Fialkowski%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22G.%20F.%22%2C%22lastName%22%3A%22Edelmann%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20A.%22%2C%22lastName%22%3A%22Dzieciuch%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22W.%20S.%22%2C%22lastName%22%3A%22Hodgkiss%22%7D%5D%2C%22abstractNote%22%3A%22This%20manuscript%20discusses%20the%20utility%20of%20maximal%20period%20linear%20binary%20pseudorandom%20sequences%20%5Balso%20referred%20to%20as%20m-sequences%20or%20maximum%20length%20sequences%20%28MLSs%29%5D%20and%20linear%20frequency-modulated%20%28LFM%29%20sweeps%20for%20the%20purpose%20of%20measuring%20travel-time%20in%20ocean-acoustic%20experiments%20involving%20moving%20sources.%20Signal%20design%20and%20waveform%20response%20to%20unknown%20Doppler%20%28waveform%20dilation%20or%20scale%20factor%29%20are%20reviewed.%20For%20this%20two-parameter%20estimation%20problem%2C%20the%20well-known%20wide-band%20ambiguity%20function%20indicates%2C%20and%20moving-source%20observations%20corroborate%2C%20a%20significant%20performance%20benefit%20from%20using%20MLS%20over%20LFM%20waveforms%20of%20similar%20time%20duration%20and%20bandwidth.%20The%20comparison%20is%20illustrated%20with%20a%20typical%20experimental%20setup%20of%20a%20source%20suspended%20aft%20of%20the%20R%5C%2FV%20Sally%20Ride%20to%20a%20depth%20of%20similar%20to%2010m%20and%20towed%20at%20similar%20to%201m%5C%2Fs%20speed.%20Accounting%20for%20constant%20source%20motion%2C%20the%20root%20mean%20square%20travel-time%20variability%20over%20a%2030min%20observation%20interval%20is%2053%20mu%20s%20%28MLS%29%20and%20141%20mu%20s%20%28LFM%29.%20For%20these%20high%20signal-to-noise%20ratio%20channel%20impulse%20response%20data%2C%20LFM%20arrival-time%20fluctuations%20mostly%20appear%20random%20while%20MLS%20results%20exhibit%20structure%20believed%20to%20be%20consistent%20with%20source%20%28i.e.%2C%20towed%20transducer%29%20dynamics.%20We%20conclude%20with%20a%20discussion%20on%20signal%20coherence%20with%20integration%20times%20up%20to%2011%20MLS%20waveform%20periods%20corresponding%20to%20similar%20to%2027%20s.%22%2C%22date%22%3A%222021%5C%2F10%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0006656%22%2C%22ISSN%22%3A%220001-4966%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22NBZ3B7BX%22%2C%222AQ2ECNM%22%5D%2C%22dateModified%22%3A%222022-10-11T20%3A25%3A32Z%22%7D%7D%2C%7B%22key%22%3A%22H4XK95XT%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Vazquez%20and%20Gomez-Valdes%22%2C%22parsedDate%22%3A%222021-03%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20%26amp%3B%20Gomez-Valdes%2C%20J.%20%282021%29.%20Wind%20events%20in%20a%20subtropical%20coastal%20upwelling%20region%20as%20detected%20by%20admittance%20analysis.%20%3Ci%3EOcean%20Dynamics%3C%5C%2Fi%3E.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1007%5C%2Fs10236-021-01446-z%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1007%5C%2Fs10236-021-01446-z%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Wind%20events%20in%20a%20subtropical%20coastal%20upwelling%20region%20as%20detected%20by%20admittance%20analysis%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%22%2C%22lastName%22%3A%22Gomez-Valdes%22%7D%5D%2C%22abstractNote%22%3A%22Wind%20dominates%20the%20ocean%20surface%20circulation%20in%20the%20subtropical%20coastal%20upwelling%20regions.%20Although%20the%20wind%20events%20in%20these%20regions%20are%20mostly%20favorable%20for%20upwelling%2C%20other%20types%20of%20wind%20events%20are%20occasionally%20dominant.%20The%20typical%20patterns%20and%20statistics%20of%20wind%20events%20over%20the%20waters%20off%20northern%20Baja%20California%20are%20described.%20The%20identification%20of%20wind%20events%20was%20carried%20out%20using%20a%20systematic%20technique%20based%20on%20both%20the%20admittance%20magnitude%20and%20phase.%20This%20technique%20proved%20useful%20and%20has%20some%20of%20the%20crucial%20characteristics%20expected%20from%20a%20classification%20standpoint.%20This%20technique%20is%20applied%20to%2029%20years%20%281990-2018%29%20of%20cross-calibrated%20multiplatform%20%28CCMP%29%2010-m%20wind%20data.%20Equatorward%20along%20the%20coast%20%28upwelling-favorable%29%2C%20offshore%20%28Santa%20Ana%29%2C%20onshore%2C%20poleward%20along%20the%20coast%20%28downwelling-favorable%29%2C%20and%20relaxation%20events%20are%20identified.%20The%20wind%20stress%20and%20wind%20stress%20curl%20mean%20fields%20and%20the%20statistics%20of%20occurrence%20are%20described%20on%20a%20year-to-year%20and%20month-to-month%20basis%20for%20each%20wind%20type.%20The%20upwelling-favorable%20and%20relaxation%20events%20are%20the%20most%20frequent%20and%20occur%20throughout%20the%20year%3B%20the%20typical%20duration%20is%204%20and%201.5%20days%2C%20respectively.%20The%20offshore%20%28Santa%20Ana%29%2C%20onshore%2C%20and%20poleward%20wind%20events%20are%20sporadic%20and%20occur%20only%20during%20autumn-winter.%20The%20year-to-year%20variation%20of%20the%20frequency%20of%20occurrence%20of%20the%20equatorward%20wind%20events%20shows%20no%20trend%20during%20the%20study%20period.%22%2C%22date%22%3A%222021%5C%2F03%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.1007%5C%2Fs10236-021-01446-z%22%2C%22ISSN%22%3A%221616-7341%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222022-02-28T17%3A24%3A37Z%22%7D%7D%2C%7B%22key%22%3A%22YRK7TMI2%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Geyer%20et%20al.%22%2C%22parsedDate%22%3A%222020-02%22%2C%22numChildren%22%3A6%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EGeyer%2C%20F.%2C%20Sagen%2C%20H.%2C%20Cornuelle%2C%20B.%2C%20Mazloff%2C%20M.%20R.%2C%20%26amp%3B%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%20%282020%29.%20Using%20a%20regional%20ocean%20model%20to%20understand%20the%20structure%20and%20variability%20of%20acoustic%20arrivals%20in%20Fram%20Strait.%20%3Ci%3EJournal%20of%20the%20Acoustical%20Society%20of%20America%3C%5C%2Fi%3E%2C%20%3Ci%3E147%3C%5C%2Fi%3E%282%29%2C%201042%26%23x2013%3B1053.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0000513%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1121%5C%2F10.0000513%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Using%20a%20regional%20ocean%20model%20to%20understand%20the%20structure%20and%20variability%20of%20acoustic%20arrivals%20in%20Fram%20Strait%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22F.%22%2C%22lastName%22%3A%22Geyer%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%22%2C%22lastName%22%3A%22Sagen%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22B.%22%2C%22lastName%22%3A%22Cornuelle%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22M.%20R.%22%2C%22lastName%22%3A%22Mazloff%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%5D%2C%22abstractNote%22%3A%22A%20regional%20ocean%20model%20for%20Fram%20Strait%20provides%20a%20framework%20for%20interpretation%20of%20the%20variability%20and%20structure%20of%20acoustic%20tomography%20arrivals.%20The%20eddy-permitting%20model%20%2852%20vertical%20levels%20and%204.5%20km%20horizontal%20resolution%29%20was%20evaluated%20using%20long-term%20moored%20hydrography%20data%20and%20time%20series%20of%20depth-range%20averaged%20temperature%20obtained%20from%20the%20inversion%20of%20acoustic%20tomography%20measurements.%20Geometric%20ray%20modeling%20using%20the%20ocean%20model%20fields%20reproduces%20the%20measured%20arrival%20structure%20of%20the%20acoustic%20tomography%20experiment.%20The%20combination%20of%20ocean%20and%20acoustic%20models%20gives%20insights%20into%20acoustic%20propagation%20during%20winter%20and%20spring.%20Moreover%2C%20overlapping%20arrivals%20coming%20from%20different%20vertical%20angles%20can%20be%20resolved%20and%20explained.%20The%20overlapping%20arrival%20of%20purely%20refracted%20rays%20and%20surface-reflected%5C%2Fbottom-reflected%20%28SRBR%29%20rays%20has%20implications%20for%20the%20inversion%20of%20tomography%20data%20in%20Fram%20Strait.%20The%20increased%20knowledge%20about%20the%20ray-length%20variations%20of%20SRBR%20rays%20is%20valuable%20for%20choosing%20appropriate%20observation%20kernels%20for%20the%20data%20assimilation%20of%20acoustic%20tomography%20data%20in%20Fram%20Strait.%22%2C%22date%22%3A%222020%5C%2F02%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.1121%5C%2F10.0000513%22%2C%22ISSN%22%3A%220001-4966%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%2C%22TFFGCZNI%22%2C%22P6BBM9XF%22%5D%2C%22dateModified%22%3A%222022-08-15T18%3A58%3A46Z%22%7D%7D%2C%7B%22key%22%3A%22BZ48H2SJ%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Cruz-Gomez%20and%20Vazquez%22%2C%22parsedDate%22%3A%222018-10%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3ECruz-Gomez%2C%20R.%20C.%2C%20%26amp%3B%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%20%282018%29.%20Interaction%20of%20North%20Brazil%20Current%20rings%20with%20the%20Lesser%20Antilles%20Arc%20and%20Barbados%20Island%3A%20laboratory%20experiments%20and%20observations.%20%3Ci%3EEnvironmental%20Fluid%20Mechanics%3C%5C%2Fi%3E%2C%20%3Ci%3E18%3C%5C%2Fi%3E%285%29%2C%201203%26%23x2013%3B1226.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1007%5C%2Fs10652-018-9592-x%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1007%5C%2Fs10652-018-9592-x%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Interaction%20of%20North%20Brazil%20Current%20rings%20with%20the%20Lesser%20Antilles%20Arc%20and%20Barbados%20Island%3A%20laboratory%20experiments%20and%20observations%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22R.%20C.%22%2C%22lastName%22%3A%22Cruz-Gomez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%5D%2C%22abstractNote%22%3A%22The%20interaction%20of%20North%20Brazil%20Current%20%28NBC%29%20rings%20with%20the%20Lesser%20Antilles%20Arc%20%28LAA%29%20and%20the%20Barbados%20Island%20%28BI%29%20is%20addressed%20by%20experimental%20modeling%20and%20observations.%20Our%20results%20compare%20well%20with%20previous%20experimental%20results%20and%20numerical%20simulations.%20Several%20sizes%2C%20intensities%20and%20two%20different%20vorticity%20profiles%20%28non-isolated%20and%20initially%20isolated%20vortices%29%20were%20tested.%20Three%20regimes%20were%20found%20namely%3A%20%281%29%20the%20vortex%20surrounds%20the%20BI%20and%20its%20translational%20motion%20%28TM%29%20stops%20North%20of%20BI%3B%20%282%29%20the%20vortex%20passes%20through%20the%20corridor%20between%20the%20LAA%20and%20the%20BI%20by%20reducing%20its%20size%3B%20and%20%283%29%20The%20vortex%20stopped%20at%20the%20entrance%20to%20the%20corridor%20South%20of%20the%20BI.%20Isolated%20vortices%20were%20prone%20to%20stopped%20North%20of%20the%20BI.%20Apparently%20the%20intensity%20in%20the%20outer%20vorticity%20ring%20has%20an%20influence%20on%20the%20fate%20of%20the%20NBC%20ring.%20Non-isolated%20vortices%20can%20also%20stop%20its%20TM%20North%20of%20the%20BI%20because%20when%20in%20beta%20plane%20they%20develop%20an%20outer%20ring%20similar%20to%20the%20isolated%20vortices.%20From%20these%20results%20we%20conclude%20that%20intense%20and%20big%20NBC%20rings%20are%20likely%20to%20stop%20its%20TM%20North%20of%20the%20BI.%20Medium%20and%20moderate%20vortices%20stops%20its%20TM%20South%20of%20the%20BI%20and%20they%20reduce%20their%20size%20until%20they%20are%20able%20to%20pass%20through%20the%20corridor%20between%20the%20LAA%20and%20the%20BI.%20Mild%20vortices%20of%20all%20sizes%20stop%20South%20of%20the%20corridor%2C%20close%20to%20the%20BI%20and%20the%20LAA.%20Drifter%20trajectories%20and%20Sea%20Surface%20Height%20altimetry%20confirm%20the%20results.%22%2C%22date%22%3A%222018%5C%2F10%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.1007%5C%2Fs10652-018-9592-x%22%2C%22ISSN%22%3A%221567-7419%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222022-02-28T17%3A24%3A37Z%22%7D%7D%2C%7B%22key%22%3A%22JSMEGAC2%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Vazquez%20and%20Gomez-Valdes%22%2C%22parsedDate%22%3A%222018-06%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20%26amp%3B%20Gomez-Valdes%2C%20J.%20%282018%29.%20Wind%20relaxation%20and%20poleward%20flow%20events%20in%20the%20upwelling%20region%20off%20Baja%20California%2C%20Mexico.%20%3Ci%3ECiencias%20Marinas%3C%5C%2Fi%3E%2C%20%3Ci%3E44%3C%5C%2Fi%3E%282%29%2C%2059%26%23x2013%3B70.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.7773%5C%2Fcm.v44i2.2745%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.7773%5C%2Fcm.v44i2.2745%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Wind%20relaxation%20and%20poleward%20flow%20events%20in%20the%20upwelling%20region%20off%20Baja%20California%2C%20Mexico%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.%20J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22J.%22%2C%22lastName%22%3A%22Gomez-Valdes%22%7D%5D%2C%22abstractNote%22%3A%22Wind%20relaxation%20events%20are%20commonly%20observed%20in%20eastern%20boundary%20upwelling%20ecosystems.%20The%20wind%20fields%20over%20the%20southern%20part%20of%20the%20California%20Current%20System%20were%20separated%20into%20upwelling-favorable%20winds%20and%20wind%20relaxations%20by%20using%20a%20technique%20based%20on%20complex%20correlation%20analysis.%20Using%20vessel-mounted%20Acoustic%20Doppler%20Current%20Profiler%20and%20conductivity-temperature-depth%20observations%20from%204%20consecutive%20Mexican%20Investigations%20of%20the%20California%20Current%20%28IMECOCAL%29%20cruises%20carried%20out%20during%202001-2002%2C%20a%20description%20of%20the%20ocean%20state%20associated%20with%20these%20stages%20of%20the%20wind%20field%20was%20elaborated%20for%20the%20northern%20Baja%20California%20%28Mexico%29%20upwelling%20region.%20Relaxation%20events%20occurred%20during%20each%20cruise.%20A%20coastal%20poleward%20flow%20event%20was%20conspicuous%20when%20a%20relaxation%20event%20followed%20a%20long%20upwelling%20favorable%20wind%20event.%20This%20pattern%20was%20also%20correlated%20with%20a%20negative%20or%20close%20to%20zero%20wind%20curl%20at%20the%20coast.%20A%20coastal%20equatorial%20jet%20and%20an%20upper-ocean%20offshore%20poleward%20flow%20were%20observed%20during%20spring%2C%20representing%20a%20typical%20upwelling%20pattern%20that%20is%20correlated%20with%20a%20large%20positive%20wind%20stress%20curl%20near%20the%20coast.%20In%20winter%2C%20a%20surface%20poleward%20flow%20was%20inhibited%20by%20a%20strong%20northwest%20wind%20event%2C%20which%20generated%20a%20shallow%20equatorward%20flow.%20The%20circulation%20patterns%20described%20here%20are%20consistent%20with%20theories%20that%20explain%20surface%20poleward%20flows%20through%20wind%20relaxation%20and%20negative%20wind%20curl.%22%2C%22date%22%3A%222018%5C%2F06%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%2210.7773%5C%2Fcm.v44i2.2745%22%2C%22ISSN%22%3A%220185-3880%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222022-02-28T17%3A24%3A36Z%22%7D%7D%2C%7B%22key%22%3A%22XEKRG25U%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22G%5Cu00f3mez-Vald%5Cu00e9s%20et%20al.%22%2C%22parsedDate%22%3A%222012-06%22%2C%22numChildren%22%3A1%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3EG%26%23xF3%3Bmez-Vald%26%23xE9%3Bs%2C%20J.%2C%20Dworak%2C%20J.%20A.%2C%20%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20%26amp%3B%20Paz%2C%20M.%20%282012%29.%20Vertical%20structure%20of%20tidal%20flows%20at%20the%20entrance%20to%20Guaymas%20Bay%2C%20Mexico.%20%3Ci%3EGeof%26%23xED%3Bsica%20Internacional%3C%5C%2Fi%3E%2C%20%3Ci%3E51%3C%5C%2Fi%3E%2C%20271%26%23x2013%3B279.%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Vertical%20structure%20of%20tidal%20flows%20at%20the%20entrance%20to%20Guaymas%20Bay%2C%20Mexico%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Jos%5Cu00e9%22%2C%22lastName%22%3A%22G%5Cu00f3mez-Vald%5Cu00e9s%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Juan%20A.%22%2C%22lastName%22%3A%22Dworak%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22H.J.%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Manuel%22%2C%22lastName%22%3A%22Paz%22%7D%5D%2C%22abstractNote%22%3A%22%22%2C%22date%22%3A%222012%5C%2F06%22%2C%22language%22%3A%22%22%2C%22DOI%22%3A%22%22%2C%22ISSN%22%3A%220016-7169%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222023-08-17T16%3A34%3A36Z%22%7D%7D%2C%7B%22key%22%3A%22BSPE65IN%22%2C%22library%22%3A%7B%22id%22%3A9129767%7D%2C%22meta%22%3A%7B%22creatorSummary%22%3A%22Vazquez%20et%20al.%22%2C%22parsedDate%22%3A%222011-01%22%2C%22numChildren%22%3A2%7D%2C%22bib%22%3A%22%3Cdiv%20class%3D%5C%22csl-bib-body%5C%22%20style%3D%5C%22line-height%3A%202%3B%20padding-left%3A%201em%3B%20text-indent%3A-1em%3B%5C%22%3E%5Cn%20%20%3Cdiv%20class%3D%5C%22csl-entry%5C%22%3E%3Cstrong%3EVazquez%2C%20H.%20J.%3C%5C%2Fstrong%3E%2C%20Gomez-Valdes%2C%20J.%2C%20Ortiz%2C%20M.%2C%20%26amp%3B%20Dworak%2C%20J.%20A.%20%282011%29.%20Detiding%20shipboard%20ADCP%20data%20in%20eastern%20boundary%20current.%20%3Ci%3EJournal%20of%20Atmospheric%20and%20Oceanic%20Technology%3C%5C%2Fi%3E%2C%20%3Ci%3E28%3C%5C%2Fi%3E%281%29%2C%2094%26%23x2013%3B103.%20%3Ca%20class%3D%27zp-DOIURL%27%20href%3D%27https%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1175%5C%2F2010JTECHO697.1%27%3Ehttps%3A%5C%2F%5C%2Fdoi.org%5C%2F10.1175%5C%2F2010JTECHO697.1%3C%5C%2Fa%3E%3C%5C%2Fdiv%3E%5Cn%3C%5C%2Fdiv%3E%22%2C%22data%22%3A%7B%22itemType%22%3A%22journalArticle%22%2C%22title%22%3A%22Detiding%20shipboard%20ADCP%20data%20in%20eastern%20boundary%20current%22%2C%22creators%22%3A%5B%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Heriberto%20Jesus%22%2C%22lastName%22%3A%22Vazquez%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Jose%22%2C%22lastName%22%3A%22Gomez-Valdes%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Modesto%22%2C%22lastName%22%3A%22Ortiz%22%7D%2C%7B%22creatorType%22%3A%22author%22%2C%22firstName%22%3A%22Juan%20Adolfo%22%2C%22lastName%22%3A%22Dworak%22%7D%5D%2C%22abstractNote%22%3A%22Spatiotemporal%20fitting%20by%20the%20least%20squares%20method%20is%20commonly%20applied%20to%20distinguish%20the%20mean%20flow%20from%20the%20tidal%20current%20from%20shipboard%20ADCP%20data%20in%20coastal%20ocean.%20To%20analyze%20this%20technique%20in%20a%20pelagic%20region%20of%20an%20eastern%20boundary%20current%20system%2C%20a%206-yr%20period%20of%20shipboard%20ADCP%20data%20off%20Baja%20California%20is%20examined.%20A%20diverse%20set%20of%20basis%20functions%20is%20studied%20and%20a%20global%20tidal%20model%20is%20used%20for%20comparison%20purposes.%20The%20Gaussian%20function%20together%20with%20a%20nodal%20configuration%20of%20one%20node%20in%20the%20middle%20and%20close%20to%20the%20coast%20of%20the%20region%20is%20the%20best%20option.%20However%2C%20to%20obtain%20the%20optimal%20solution%2C%20the%20geostrophic%20flow%2C%20which%20is%20stronger%20than%20the%20tidal%20flow%20and%20highly%20variable%20off%20Baja%20California%2C%20might%20be%20removed%20prior%20to%20fitting%20the%20data.%20In%20general%2C%20the%20semimajor%20axis%20of%20the%20tidal%20ellipse%20%28M2%29%20is%20parallel%20to%20the%20coast%20and%20the%20phase%20speed%20is%20poleward%20and%20parallel%20to%20the%20coast%2C%20in%20agreement%20with%20Kelvin%20wave%20dynamics.%20Because%20the%20tides%20in%20eastern%20boundary%20currents%20are%20explained%20by%20Kelvin%20wave%20dynamics%2C%20the%20use%20of%20both%20the%20velocity%20field%20without%20geostrophic%20variability%20and%20the%20Gaussian%20function%20in%20the%20spatiotemporal%20fitting%20by%20least%20squares%20technique%20is%20a%20promising%20tool%20for%20detiding%20shipboard%20ADCP%20data%20from%20these%20systems.%22%2C%22date%22%3A%222011%5C%2F01%22%2C%22language%22%3A%22English%22%2C%22DOI%22%3A%2210.1175%5C%2F2010JTECHO697.1%22%2C%22ISSN%22%3A%22%22%2C%22url%22%3A%22%22%2C%22collections%22%3A%5B%22RPFKFUG7%22%5D%2C%22dateModified%22%3A%222022-02-28T17%3A24%3A37Z%22%7D%7D%5D%7D
Vazquez, H. J., Cornuelle, B. D., Worcester, P. F., Dzieciuch, M. A., Colosi, J. A., & Nash, J. D. (2023). Using long-range transmissions in the Beaufort Gyre to test the sound-speed equation at high pressure and low temperature. The Journal of the Acoustical Society of America, 154(4), 2676–2688. https://doi.org/10.1121/10.0021973
Worcester, P. F., Dzieciuch, M. A., Vazquez, H. J., Cornuelle, B. D., Colosi, J. A., Krishfield, R. A., & Kemp, J. N. (2023). Acoustic travel-time variability observed on a 150-km radius tomographic array in the Canada Basin during 2016–2017. The Journal of the Acoustical Society of America, 153(5), 2621. https://doi.org/10.1121/10.0019304
Vazquez, H. J., Gopalakrishnan, G., & Sheinbaum, J. (2023). Impact of Yucatan Channel Subsurface Velocity Observations on the Gulf of Mexico State Estimates. Journal of Physical Oceanography, 53(1), 361–385. https://doi.org/10.1175/JPO-D-21-0213.1
Gemba, K. L., Vazquez, H. J., Sarkar, J., Tippman, J. D., Cornuelle, B., Hodgkiss, W. S., & Kuperman, W. A. (2022). Moving source ocean acoustic tomography with uncertainty quantification using controlled source-tow observations. The Journal of the Acoustical Society of America, 151(2), 861–880. https://doi.org/10.1121/10.0009268
Durofchalk, N. C., Jin, J. H., Vazquez, H. J., Gemba, K. L., Romberg, J., & Sabra, K. G. (2021). Data driven source localization using a library of nearby shipping sources of opportunity. JASA Express Letters, 1(12), 7. https://doi.org/10.1121/10.0009083
Gemba, K. L., Vazquez, H. J., Fialkowski, J., Edelmann, G. F., Dzieciuch, M. A., & Hodgkiss, W. S. (2021). A performance comparison between m-sequences and linear frequency-modulated sweeps for the estimation of travel-time with a moving source. Journal of the Acoustical Society of America, 150(4), 2613–2623. https://doi.org/10.1121/10.0006656
Vazquez, H. J., & Gomez-Valdes, J. (2021). Wind events in a subtropical coastal upwelling region as detected by admittance analysis. Ocean Dynamics. https://doi.org/10.1007/s10236-021-01446-z
Geyer, F., Sagen, H., Cornuelle, B., Mazloff, M. R., & Vazquez, H. J. (2020). Using a regional ocean model to understand the structure and variability of acoustic arrivals in Fram Strait. Journal of the Acoustical Society of America, 147(2), 1042–1053. https://doi.org/10.1121/10.0000513
Cruz-Gomez, R. C., & Vazquez, H. J. (2018). Interaction of North Brazil Current rings with the Lesser Antilles Arc and Barbados Island: laboratory experiments and observations. Environmental Fluid Mechanics, 18(5), 1203–1226. https://doi.org/10.1007/s10652-018-9592-x
Vazquez, H. J., & Gomez-Valdes, J. (2018). Wind relaxation and poleward flow events in the upwelling region off Baja California, Mexico. Ciencias Marinas, 44(2), 59–70. https://doi.org/10.7773/cm.v44i2.2745
Gómez-Valdés, J., Dworak, J. A., Vazquez, H. J., & Paz, M. (2012). Vertical structure of tidal flows at the entrance to Guaymas Bay, Mexico. Geofísica Internacional, 51, 271–279.
Vazquez, H. J., Gomez-Valdes, J., Ortiz, M., & Dworak, J. A. (2011). Detiding shipboard ADCP data in eastern boundary current. Journal of Atmospheric and Oceanic Technology, 28(1), 94–103. https://doi.org/10.1175/2010JTECHO697.1