Tidal dynamics of the Terminos Lagoon, Mexico: observations and 3D numerical modelling
The tidal circulation patterns in the Terminos Lagoon were studied based on the analysis of 1 year of measurements and numerical simulations using a baroclinic 3D hydrodynamic model, the MARS3D. A gauging network was installed consisting of six self-recording pressure–temperature sensors, a tide gau...
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description | The tidal circulation patterns in the Terminos Lagoon were studied based on the analysis of 1 year of measurements and numerical simulations using a baroclinic 3D hydrodynamic model, the MARS3D. A gauging network was installed consisting of six self-recording pressure–temperature sensors, a tide gauge station and two current profilers, with pressure and temperature sensors moored in the main lagoon inlets. Model simulations were validated against current and sea level observations and were used to analyse the circulation patterns caused by the tidal forcing. The numerical model was forced with eight harmonic components, four diurnal (
K
1
,
O
1
,
P
1
,
Q
1
) and four semi-diurnal (
M
2
,
S
2
,
N
2
,
K
2
), extracted from the TPX0.7 database. The tidal patterns in the study area vary from mixed, mainly diurnal in the two main inlets of the lagoon, to diurnal in its interior. The tidal residual circulation inside the lagoon is dominated by a cyclonic gyre. The results indicate a net flux from the southwest Ciudad del Carmen inlet (CdC) towards the northeast Puerto Real inlet (PtR) along the southern side of the lagoon and the opposite in the northern side. The results indicate two areas of strong currents in the vicinity of the inlets and weak currents inside the lagoon. The area of strong currents in the vicinity of the CdC inlet is larger than that observed in the PtR inlet. Nevertheless, the current analysis indicates that the highest current speeds, which can reach a magnitude of 1.9 m s
−1
, occurred in PtR. A further analysis of the tide distortion in the inlets revealed that both passages are ebb dominated. |
doi_str_mv | 10.1007/s10236-014-0752-3 |
format | Article |
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K
1
,
O
1
,
P
1
,
Q
1
) and four semi-diurnal (
M
2
,
S
2
,
N
2
,
K
2
), extracted from the TPX0.7 database. The tidal patterns in the study area vary from mixed, mainly diurnal in the two main inlets of the lagoon, to diurnal in its interior. The tidal residual circulation inside the lagoon is dominated by a cyclonic gyre. The results indicate a net flux from the southwest Ciudad del Carmen inlet (CdC) towards the northeast Puerto Real inlet (PtR) along the southern side of the lagoon and the opposite in the northern side. The results indicate two areas of strong currents in the vicinity of the inlets and weak currents inside the lagoon. The area of strong currents in the vicinity of the CdC inlet is larger than that observed in the PtR inlet. Nevertheless, the current analysis indicates that the highest current speeds, which can reach a magnitude of 1.9 m s
−1
, occurred in PtR. A further analysis of the tide distortion in the inlets revealed that both passages are ebb dominated.</description><identifier>ISSN: 1616-7341</identifier><identifier>EISSN: 1616-7228</identifier><identifier>DOI: 10.1007/s10236-014-0752-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Atmospheric Sciences ; Earth and Environmental Science ; Earth Sciences ; Fluid- and Aerodynamics ; Geophysics/Geodesy ; Inlets ; Lagoons ; Mathematical models ; Monitoring/Environmental Analysis ; Numerical analysis ; Oceanography ; Sciences of the Universe ; Sensors ; Three dimensional imaging ; Tidal waves ; Topical Collection on Physics of Estuaries and Coastal Seas 2012</subject><ispartof>Ocean dynamics, 2014-09, Vol.64 (9), p.1349-1371</ispartof><rights>The Author(s) 2014</rights><rights>Springer-Verlag Berlin Heidelberg 2014</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c426t-564b0c2a164bdcc16db1bc6c9147697bf7893ac600cd87870e7fdd576df1c6493</citedby><cites>FETCH-LOGICAL-c426t-564b0c2a164bdcc16db1bc6c9147697bf7893ac600cd87870e7fdd576df1c6493</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10236-014-0752-3$$EPDF$$P50$$Gspringer$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10236-014-0752-3$$EHTML$$P50$$Gspringer$$Hfree_for_read</linktohtml><link.rule.ids>230,314,776,780,881,27901,27902,41464,42533,51294</link.rule.ids><backlink>$$Uhttps://hal.science/hal-01058574$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Contreras Ruiz Esparza, Adolfo</creatorcontrib><creatorcontrib>Douillet, Pascal</creatorcontrib><creatorcontrib>Zavala-Hidalgo, Jorge</creatorcontrib><title>Tidal dynamics of the Terminos Lagoon, Mexico: observations and 3D numerical modelling</title><title>Ocean dynamics</title><addtitle>Ocean Dynamics</addtitle><description>The tidal circulation patterns in the Terminos Lagoon were studied based on the analysis of 1 year of measurements and numerical simulations using a baroclinic 3D hydrodynamic model, the MARS3D. A gauging network was installed consisting of six self-recording pressure–temperature sensors, a tide gauge station and two current profilers, with pressure and temperature sensors moored in the main lagoon inlets. Model simulations were validated against current and sea level observations and were used to analyse the circulation patterns caused by the tidal forcing. The numerical model was forced with eight harmonic components, four diurnal (
K
1
,
O
1
,
P
1
,
Q
1
) and four semi-diurnal (
M
2
,
S
2
,
N
2
,
K
2
), extracted from the TPX0.7 database. The tidal patterns in the study area vary from mixed, mainly diurnal in the two main inlets of the lagoon, to diurnal in its interior. The tidal residual circulation inside the lagoon is dominated by a cyclonic gyre. The results indicate a net flux from the southwest Ciudad del Carmen inlet (CdC) towards the northeast Puerto Real inlet (PtR) along the southern side of the lagoon and the opposite in the northern side. The results indicate two areas of strong currents in the vicinity of the inlets and weak currents inside the lagoon. The area of strong currents in the vicinity of the CdC inlet is larger than that observed in the PtR inlet. Nevertheless, the current analysis indicates that the highest current speeds, which can reach a magnitude of 1.9 m s
−1
, occurred in PtR. A further analysis of the tide distortion in the inlets revealed that both passages are ebb dominated.</description><subject>Atmospheric Sciences</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fluid- and Aerodynamics</subject><subject>Geophysics/Geodesy</subject><subject>Inlets</subject><subject>Lagoons</subject><subject>Mathematical models</subject><subject>Monitoring/Environmental Analysis</subject><subject>Numerical analysis</subject><subject>Oceanography</subject><subject>Sciences of the Universe</subject><subject>Sensors</subject><subject>Three dimensional imaging</subject><subject>Tidal waves</subject><subject>Topical Collection on Physics of Estuaries and Coastal Seas 2012</subject><issn>1616-7341</issn><issn>1616-7228</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>C6C</sourceid><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kUtLxDAUhYso-PwB7gJuFKzmpmnSupPxCSNuRrchTdKZSJtoMjPovzelKiK4upfLdw4nOVl2CPgMMObnETApWI6B5piXJC82sh1gwHJOSLX5vRcUtrPdGF8wBs4o2cmeZ1bLDukPJ3urIvItWi4MmpnQW-cjmsq59-4UPZh3q_wF8k00YS2X1ruIpNOouEJu1ZtgVbLpvTZdZ918P9tqZRfNwdfcy55urmeTu3z6eHs_uZzmihK2zEtGG6yIhDS1UsB0A41iqgbKWc2blld1IRXDWOmKVxwb3mpdcqZbUIzWxV52MvouZCdeg-1l-BBeWnF3ORXDDQMuq5LTNST2eGRfg39bmbgUvY0q5ZXO-FUU6YsqKBmDwfboD_riV8GllwgoSwq0JrRIFIyUCj7GYNqfBIDF0IoYW0khqBhaEYOGjJqYWDc34Zfzv6JPjoGNTw</recordid><startdate>20140901</startdate><enddate>20140901</enddate><creator>Contreras Ruiz Esparza, Adolfo</creator><creator>Douillet, Pascal</creator><creator>Zavala-Hidalgo, Jorge</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><general>Springer Verlag</general><general>Springer Verlag (Germany)</general><scope>C6C</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>1XC</scope></search><sort><creationdate>20140901</creationdate><title>Tidal dynamics of the Terminos Lagoon, Mexico: observations and 3D numerical modelling</title><author>Contreras Ruiz Esparza, Adolfo ; Douillet, Pascal ; Zavala-Hidalgo, Jorge</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c426t-564b0c2a164bdcc16db1bc6c9147697bf7893ac600cd87870e7fdd576df1c6493</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Atmospheric Sciences</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fluid- and Aerodynamics</topic><topic>Geophysics/Geodesy</topic><topic>Inlets</topic><topic>Lagoons</topic><topic>Mathematical models</topic><topic>Monitoring/Environmental Analysis</topic><topic>Numerical analysis</topic><topic>Oceanography</topic><topic>Sciences of the Universe</topic><topic>Sensors</topic><topic>Three dimensional imaging</topic><topic>Tidal waves</topic><topic>Topical Collection on Physics of Estuaries and Coastal Seas 2012</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Contreras Ruiz Esparza, Adolfo</creatorcontrib><creatorcontrib>Douillet, Pascal</creatorcontrib><creatorcontrib>Zavala-Hidalgo, Jorge</creatorcontrib><collection>Springer Nature OA Free Journals</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Ocean dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Contreras Ruiz Esparza, Adolfo</au><au>Douillet, Pascal</au><au>Zavala-Hidalgo, Jorge</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tidal dynamics of the Terminos Lagoon, Mexico: observations and 3D numerical modelling</atitle><jtitle>Ocean dynamics</jtitle><stitle>Ocean Dynamics</stitle><date>2014-09-01</date><risdate>2014</risdate><volume>64</volume><issue>9</issue><spage>1349</spage><epage>1371</epage><pages>1349-1371</pages><issn>1616-7341</issn><eissn>1616-7228</eissn><abstract>The tidal circulation patterns in the Terminos Lagoon were studied based on the analysis of 1 year of measurements and numerical simulations using a baroclinic 3D hydrodynamic model, the MARS3D. A gauging network was installed consisting of six self-recording pressure–temperature sensors, a tide gauge station and two current profilers, with pressure and temperature sensors moored in the main lagoon inlets. Model simulations were validated against current and sea level observations and were used to analyse the circulation patterns caused by the tidal forcing. The numerical model was forced with eight harmonic components, four diurnal (
K
1
,
O
1
,
P
1
,
Q
1
) and four semi-diurnal (
M
2
,
S
2
,
N
2
,
K
2
), extracted from the TPX0.7 database. The tidal patterns in the study area vary from mixed, mainly diurnal in the two main inlets of the lagoon, to diurnal in its interior. The tidal residual circulation inside the lagoon is dominated by a cyclonic gyre. The results indicate a net flux from the southwest Ciudad del Carmen inlet (CdC) towards the northeast Puerto Real inlet (PtR) along the southern side of the lagoon and the opposite in the northern side. The results indicate two areas of strong currents in the vicinity of the inlets and weak currents inside the lagoon. The area of strong currents in the vicinity of the CdC inlet is larger than that observed in the PtR inlet. Nevertheless, the current analysis indicates that the highest current speeds, which can reach a magnitude of 1.9 m s
−1
, occurred in PtR. A further analysis of the tide distortion in the inlets revealed that both passages are ebb dominated.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10236-014-0752-3</doi><tpages>23</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Atmospheric Sciences Earth and Environmental Science Earth Sciences Fluid- and Aerodynamics Geophysics/Geodesy Inlets Lagoons Mathematical models Monitoring/Environmental Analysis Numerical analysis Oceanography Sciences of the Universe Sensors Three dimensional imaging Tidal waves Topical Collection on Physics of Estuaries and Coastal Seas 2012 |
title | Tidal dynamics of the Terminos Lagoon, Mexico: observations and 3D numerical modelling |
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