Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]

This study focuses on the relative importance of the forcing agents of Atrato River plume as it propagates in a tropical estuary located in the Gulf of Uraba in the Colombian Caribbean Sea. Six campaigns of intensive field data collection were carried out from 2004 to 2007 to identify the main featu...

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Fecha de publicación:: 2017

Institución:: Universidad de Medellín

Repositorio:: Repositorio UDEM

Idioma:: eng

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repository_id_str
dc.title.spa.fl_str_mv	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
title	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
spellingShingle	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia] ELCOM model Freshwater river plume Gulf of Uraba Hydrodynamics Tropical estuaries
title_short	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
title_full	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
title_fullStr	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
title_full_unstemmed	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
title_sort	Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]
dc.contributor.affiliation.spa.fl_str_mv	Montoya, L.J., School of Engineering, Universidad de Medellin, Medellin, Colombia Toro-Botero, F.M., Geosciences and Environmental Department, Facultad de Minas, Universidad Nacional de Colombia, Medellin, Colombia Gomez-Giraldo, A., Geosciences and Environmental Department, School of Mines, Universidad Nacional de Colombia, Medellin, Colombia
dc.subject.keyword.eng.fl_str_mv	ELCOM model Freshwater river plume Gulf of Uraba Hydrodynamics Tropical estuaries
topic	ELCOM model Freshwater river plume Gulf of Uraba Hydrodynamics Tropical estuaries
description	This study focuses on the relative importance of the forcing agents of Atrato River plume as it propagates in a tropical estuary located in the Gulf of Uraba in the Colombian Caribbean Sea. Six campaigns of intensive field data collection were carried out from 2004 to 2007 to identify the main features of the plume and to calibrate and validate a numerical model. Field data and numerical models revealed high spatial and temporal plume variability according to the magnitudes of river discharges, tidal cycles, and wind stress. Atrato River discharge spreads over a considerable portion of the gulf, but only occupies the top 2 m of the surface layer. The tide modifies the position of the plume by inducing a horizontal migration of the salinity front during the day. Two principal modes of circulation in the gulf were identified under different wind conditions. © The author; licensee Universidad Nacional de Colombia.
publishDate	2017
dc.date.accessioned.none.fl_str_mv	2017-12-19T19:36:48Z
dc.date.available.none.fl_str_mv	2017-12-19T19:36:48Z
dc.date.created.none.fl_str_mv	2017
dc.type.eng.fl_str_mv	Article
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dc.identifier.issn.none.fl_str_mv	127353
dc.identifier.uri.none.fl_str_mv	http://hdl.handle.net/11407/4324
dc.identifier.doi.none.fl_str_mv	10.15446/dyna.v84n200.55040
dc.identifier.reponame.spa.fl_str_mv	reponame:Repositorio Institucional Universidad de Medellín
dc.identifier.instname.spa.fl_str_mv	instname:Universidad de Medellín
identifier_str_mv	127353 10.15446/dyna.v84n200.55040 reponame:Repositorio Institucional Universidad de Medellín instname:Universidad de Medellín
url	http://hdl.handle.net/11407/4324
dc.language.iso.none.fl_str_mv	eng
language	eng
dc.relation.isversionof.spa.fl_str_mv	https://www.scopus.com/inward/record.uri?eid=2-s2.0-85021800652&doi=10.15446%2fdyna.v84n200.55040&partnerID=40&md5=24ab53e225ad729ebeda7df10748e0c4
dc.relation.ispartofes.spa.fl_str_mv	DYNA (Colombia)
dc.relation.references.spa.fl_str_mv	Bowman, M.J., Estuarine fronts, in hydrodynamics of estuaries (1988) Volume I: Estuarine Physics, pp. 86-131. , Boca Raton, FLA: CRC press Simionato, C.G., Dragani, W., Meccia, V., Nuñez, M., A numerical study of the barotropic circulation of the Río de la Plata estuary: Sensitivity to bathymetry, the Earth’s rotation and low frequency wind variability. Estuarine (2004) Coastal and Shelf Science, 61, pp. 261-273 Chao, S.Y., Wind-driven motion of estuarine plumes (1988) Journal of Physical Oceanography, 18, pp. 1144-1166 Fong, D.A., Geyer, W.R., Response of a river plume during a upwelling favourable wind event (2001) Journal of Geophysical Research, 106, pp. 1067-1084 Garcia-Berdeal, I., Hickey, B., Kawase, M., Influence of wind stress and ambient flow on a high discharge River Plume (2002) Journal of Geophysical Research – Oceans, 107 (C9), pp. 1-13 Spillman, C.M., Imberger, J., Hamilton, D.P., Hipsey, M.R., Romero, J.R., Modelling the effects of Po River discharge, internal nutrient cycling and hydrodynamics on biogeochemistry of the Northern Adriatic Sea (2007) Journal of Marine Systems, 68, pp. 167-200 Simpson, J.H., Physical processes in the ROFI regime (1997) Journal of Marine Systems, 12, pp. 3-15 Fujiwara, T., Sanford, L.P., Nakatsuji, K., Sugiyama, Y., Anti-cyclonic circulation driven by the estuarine circulation in a gulf type ROFI (1997) Journal of Marine System, 12, pp. 83-99 James, I.D., A numerical model of the development of anticyclonic circulation in a gulf-type region of freshwater influence (1997) Continental Shelf Research, 17 (14), pp. 1803-1816 Hetland, R.D., Relating river plume structure to vertical mixing (2005) Journal of Physical Oceanography, 35 (9), pp. 1667-1688 Rong, Z., Hetland, R.D., Zhang, W., Zhang, X., Current-wave interaction in the Mississippi-Atchafalaya river plume on the Texas-Louisiana shelf (2014) Ocean Modelling, 84, pp. 67-83 Wiseman, W., Garvine, R., Plumes and coastal currents near large river mouths (1995) Estuaries, 16 (3), pp. 509-517 Garvine, R., A dynamical system for classifying buoyant coastal discharges (1995) Continental Shelf Research, 15, pp. 1585-1596 Estournel, C., Broche, P., Marsaleix, P., Devenon, J.L., Auclair, F., Vehil, R., The Rhone River plume in unsteady conditions: Numerical and experimental results. Estuarine (2001) Coastal and Shelf Science, 53, pp. 25-38 Tilburg, C.E., Garvine, R.W., Three-dimensional flow in a Shallow Coastal upwelling zone: Alongshore convergence and divergence on the New Jersey shelf (2003) Journal of Physical Oceanography, 33, pp. 2113-2125 Whitney, M., Garvine, R., Simulationg the Delaware Bay Bouyant outflow: Comparison with observations (2006) Journal of Physical Oceanography, 36, pp. 3-21 Baptista, A., Zhang, Y., Chawla, A., Zulauf, M., Seaton, C., Edward, P., Myers, E.P., Turner, P., A cross-scale model for 3D baroclinic circulation in estuary–plume–shelf systems: II. Application to the Columbia River (2005) Continental Shelf Research, 25, pp. 935-972 Farcieri, F.M., Benetazzo, A., Sclavo, M., Russo, A., Carniel, S., Po River plume pattern variability investigated from model data (2014) Continental Shelf Research, 87, pp. 84-95 Nikiema, O., Devenon, J.-L., Baklouti, M., Numerical modeling of the Amazon River plume (2007) Continental Shelf Research, 27, pp. 873-899 Chevillot, P., Molina, A., Giraldo, L., Molina, C., Estudio geológico e hidrológico del golfo de Urabá (1993) Boletín Científico CIOH, 14, pp. 79-89 Bernal, G., Montoya, L.J., Garizabal, C., Toro, M., La complejidad de la dimensión física en la problemática costera del Golfo de Urabá, Colombia (2005) Gestión Y Ambiente, 8, pp. 123-135 Lonin, S., Vásquez, J., Hidrodinámica y distribución de coliformes en el Golfo de Urabá (2005) Boletín Científico CIOH, 23, pp. 76-89 Montoya, L.J., Toro, M., Calibración de un modelo hidrodinámico para el estudio de los patrones de circulación en el Golfo de Urabá, Colombia (2006) Avances En Recursos Hidráulicos, 13, pp. 37-54 Escobar, C.A., Velásquez, L., Posada, F., Marine currents in the Gulf of Urabá. Colombian Caribbean sea (2015) Journal of Coastal Research, 6, pp. 1363-1374 Correa, I.D., Vernette, G., Introducción al problema de la erosión litoral en Urabá (Sector Arboletes-Turbo) Costa Caribe Colombiana (2004) Boletín Investigaciones Marinas Y Costeras, 33, pp. 7-28 Hodges, B., Imberger, J., Saggio, A., Winters, K.B., Modeling basin-scale internal waves in strafied lake (2000) Limnology and Oceangraphy, 45 (7), pp. 1603-1620 Casulli, V., Cheng, R.T., Semi-implicit finite difference methods for three-dimensional shallow water flow (1992) International Journal for Numerical Methods in Fluids, 15, pp. 629-648 Leonard, B.P., The ULTIMATE conservative difference scheme applied to unsteady one-dimensional advection (1991) Computer Methods in Applied Mechanics and Engineering, 88, pp. 17-74 Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Dennis, J.R.J., The NCEP/NCAR 40-Year Reanalysis Project (1996) Ulletin of the American Meteorological Society, 77 (3), pp. 437-471 Poveda, G., Mesa, O.J., Velez, J.I., Mantilla, R., Ramirez, J.M., Hernández, O.O., Borja, A.F., Urzola, J.A., HidroSIG: An interactive digital atlas of Colombia’s hydro-climatology (2007) Journal of Hydroinformatics, 9, pp. 145-156 Ulses, C., Grenz, C., Marsaleix, P., Schaaff, E., Estournel, C., Meule, S., Pinazo, C., Circulation in a semi-enclosed bay under influence of strong freshwater input (2005) Journal of Marine Systems, 56, pp. 113-132 Sierra, J.P., Sanchez-Arcilla, A., Del Rio, J.G., Flos, J., Movellan, E., Mosso, C., Martinez, R., Romero, I., Spatial distribution of nutrients in the Ebro estuary and plume (2002) Continental Shelf Research, 22, pp. 361-378 Yankovsky, A.E., Chapman, D.C., A simple theory for the fate of bouyant coastal discharge (1997) Journal of Physical Oceanography, 27, pp. 1386-1401 Lentz, S.J., Largier, J., The influence of wind forcing on the Chesapeake Bay buoyant Coastal Current (2006) Journal of Physical Oceanography, 36, pp. 1305-1316
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dc.publisher.spa.fl_str_mv	Universidad Nacional de Colombia
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spelling	2017-12-19T19:36:48Z2017-12-19T19:36:48Z2017127353http://hdl.handle.net/11407/432410.15446/dyna.v84n200.55040reponame:Repositorio Institucional Universidad de Medellíninstname:Universidad de MedellínThis study focuses on the relative importance of the forcing agents of Atrato River plume as it propagates in a tropical estuary located in the Gulf of Uraba in the Colombian Caribbean Sea. Six campaigns of intensive field data collection were carried out from 2004 to 2007 to identify the main features of the plume and to calibrate and validate a numerical model. Field data and numerical models revealed high spatial and temporal plume variability according to the magnitudes of river discharges, tidal cycles, and wind stress. Atrato River discharge spreads over a considerable portion of the gulf, but only occupies the top 2 m of the surface layer. The tide modifies the position of the plume by inducing a horizontal migration of the salinity front during the day. Two principal modes of circulation in the gulf were identified under different wind conditions. © The author; licensee Universidad Nacional de Colombia.engUniversidad Nacional de ColombiaFacultad de Ingenieríashttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85021800652&doi=10.15446%2fdyna.v84n200.55040&partnerID=40&md5=24ab53e225ad729ebeda7df10748e0c4DYNA (Colombia)Bowman, M.J., Estuarine fronts, in hydrodynamics of estuaries (1988) Volume I: Estuarine Physics, pp. 86-131. , Boca Raton, FLA: CRC pressSimionato, C.G., Dragani, W., Meccia, V., Nuñez, M., A numerical study of the barotropic circulation of the Río de la Plata estuary: Sensitivity to bathymetry, the Earth’s rotation and low frequency wind variability. Estuarine (2004) Coastal and Shelf Science, 61, pp. 261-273Chao, S.Y., Wind-driven motion of estuarine plumes (1988) Journal of Physical Oceanography, 18, pp. 1144-1166Fong, D.A., Geyer, W.R., Response of a river plume during a upwelling favourable wind event (2001) Journal of Geophysical Research, 106, pp. 1067-1084Garcia-Berdeal, I., Hickey, B., Kawase, M., Influence of wind stress and ambient flow on a high discharge River Plume (2002) Journal of Geophysical Research – Oceans, 107 (C9), pp. 1-13Spillman, C.M., Imberger, J., Hamilton, D.P., Hipsey, M.R., Romero, J.R., Modelling the effects of Po River discharge, internal nutrient cycling and hydrodynamics on biogeochemistry of the Northern Adriatic Sea (2007) Journal of Marine Systems, 68, pp. 167-200Simpson, J.H., Physical processes in the ROFI regime (1997) Journal of Marine Systems, 12, pp. 3-15Fujiwara, T., Sanford, L.P., Nakatsuji, K., Sugiyama, Y., Anti-cyclonic circulation driven by the estuarine circulation in a gulf type ROFI (1997) Journal of Marine System, 12, pp. 83-99James, I.D., A numerical model of the development of anticyclonic circulation in a gulf-type region of freshwater influence (1997) Continental Shelf Research, 17 (14), pp. 1803-1816Hetland, R.D., Relating river plume structure to vertical mixing (2005) Journal of Physical Oceanography, 35 (9), pp. 1667-1688Rong, Z., Hetland, R.D., Zhang, W., Zhang, X., Current-wave interaction in the Mississippi-Atchafalaya river plume on the Texas-Louisiana shelf (2014) Ocean Modelling, 84, pp. 67-83Wiseman, W., Garvine, R., Plumes and coastal currents near large river mouths (1995) Estuaries, 16 (3), pp. 509-517Garvine, R., A dynamical system for classifying buoyant coastal discharges (1995) Continental Shelf Research, 15, pp. 1585-1596Estournel, C., Broche, P., Marsaleix, P., Devenon, J.L., Auclair, F., Vehil, R., The Rhone River plume in unsteady conditions: Numerical and experimental results. Estuarine (2001) Coastal and Shelf Science, 53, pp. 25-38Tilburg, C.E., Garvine, R.W., Three-dimensional flow in a Shallow Coastal upwelling zone: Alongshore convergence and divergence on the New Jersey shelf (2003) Journal of Physical Oceanography, 33, pp. 2113-2125Whitney, M., Garvine, R., Simulationg the Delaware Bay Bouyant outflow: Comparison with observations (2006) Journal of Physical Oceanography, 36, pp. 3-21Baptista, A., Zhang, Y., Chawla, A., Zulauf, M., Seaton, C., Edward, P., Myers, E.P., Turner, P., A cross-scale model for 3D baroclinic circulation in estuary–plume–shelf systems: II. Application to the Columbia River (2005) Continental Shelf Research, 25, pp. 935-972Farcieri, F.M., Benetazzo, A., Sclavo, M., Russo, A., Carniel, S., Po River plume pattern variability investigated from model data (2014) Continental Shelf Research, 87, pp. 84-95Nikiema, O., Devenon, J.-L., Baklouti, M., Numerical modeling of the Amazon River plume (2007) Continental Shelf Research, 27, pp. 873-899Chevillot, P., Molina, A., Giraldo, L., Molina, C., Estudio geológico e hidrológico del golfo de Urabá (1993) Boletín Científico CIOH, 14, pp. 79-89Bernal, G., Montoya, L.J., Garizabal, C., Toro, M., La complejidad de la dimensión física en la problemática costera del Golfo de Urabá, Colombia (2005) Gestión Y Ambiente, 8, pp. 123-135Lonin, S., Vásquez, J., Hidrodinámica y distribución de coliformes en el Golfo de Urabá (2005) Boletín Científico CIOH, 23, pp. 76-89Montoya, L.J., Toro, M., Calibración de un modelo hidrodinámico para el estudio de los patrones de circulación en el Golfo de Urabá, Colombia (2006) Avances En Recursos Hidráulicos, 13, pp. 37-54Escobar, C.A., Velásquez, L., Posada, F., Marine currents in the Gulf of Urabá. Colombian Caribbean sea (2015) Journal of Coastal Research, 6, pp. 1363-1374Correa, I.D., Vernette, G., Introducción al problema de la erosión litoral en Urabá (Sector Arboletes-Turbo) Costa Caribe Colombiana (2004) Boletín Investigaciones Marinas Y Costeras, 33, pp. 7-28Hodges, B., Imberger, J., Saggio, A., Winters, K.B., Modeling basin-scale internal waves in strafied lake (2000) Limnology and Oceangraphy, 45 (7), pp. 1603-1620Casulli, V., Cheng, R.T., Semi-implicit finite difference methods for three-dimensional shallow water flow (1992) International Journal for Numerical Methods in Fluids, 15, pp. 629-648Leonard, B.P., The ULTIMATE conservative difference scheme applied to unsteady one-dimensional advection (1991) Computer Methods in Applied Mechanics and Engineering, 88, pp. 17-74Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Dennis, J.R.J., The NCEP/NCAR 40-Year Reanalysis Project (1996) Ulletin of the American Meteorological Society, 77 (3), pp. 437-471Poveda, G., Mesa, O.J., Velez, J.I., Mantilla, R., Ramirez, J.M., Hernández, O.O., Borja, A.F., Urzola, J.A., HidroSIG: An interactive digital atlas of Colombia’s hydro-climatology (2007) Journal of Hydroinformatics, 9, pp. 145-156Ulses, C., Grenz, C., Marsaleix, P., Schaaff, E., Estournel, C., Meule, S., Pinazo, C., Circulation in a semi-enclosed bay under influence of strong freshwater input (2005) Journal of Marine Systems, 56, pp. 113-132Sierra, J.P., Sanchez-Arcilla, A., Del Rio, J.G., Flos, J., Movellan, E., Mosso, C., Martinez, R., Romero, I., Spatial distribution of nutrients in the Ebro estuary and plume (2002) Continental Shelf Research, 22, pp. 361-378Yankovsky, A.E., Chapman, D.C., A simple theory for the fate of bouyant coastal discharge (1997) Journal of Physical Oceanography, 27, pp. 1386-1401Lentz, S.J., Largier, J., The influence of wind forcing on the Chesapeake Bay buoyant Coastal Current (2006) Journal of Physical Oceanography, 36, pp. 1305-1316ScopusStudy of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]Articleinfo:eu-repo/semantics/articlehttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Montoya, L.J., School of Engineering, Universidad de Medellin, Medellin, ColombiaToro-Botero, F.M., Geosciences and Environmental Department, Facultad de Minas, Universidad Nacional de Colombia, Medellin, ColombiaGomez-Giraldo, A., Geosciences and Environmental Department, School of Mines, Universidad Nacional de Colombia, Medellin, ColombiaMontoya L.J.Toro-Botero F.M.Gomez-Giraldo A.School of Engineering, Universidad de Medellin, Medellin, ColombiaGeosciences and Environmental Department, Facultad de Minas, Universidad Nacional de Colombia, Medellin, ColombiaGeosciences and Environmental Department, School of Mines, Universidad Nacional de Colombia, Medellin, ColombiaELCOM modelFreshwater river plumeGulf of UrabaHydrodynamicsTropical estuariesThis study focuses on the relative importance of the forcing agents of Atrato River plume as it propagates in a tropical estuary located in the Gulf of Uraba in the Colombian Caribbean Sea. Six campaigns of intensive field data collection were carried out from 2004 to 2007 to identify the main features of the plume and to calibrate and validate a numerical model. Field data and numerical models revealed high spatial and temporal plume variability according to the magnitudes of river discharges, tidal cycles, and wind stress. Atrato River discharge spreads over a considerable portion of the gulf, but only occupies the top 2 m of the surface layer. The tide modifies the position of the plume by inducing a horizontal migration of the salinity front during the day. Two principal modes of circulation in the gulf were identified under different wind conditions. © The author; licensee Universidad Nacional de Colombia.http://purl.org/coar/access_right/c_16ecTHUMBNAIL4. Study of Atrato river plume in a tropical estuary.pdf.jpg4. Study of Atrato river plume in a tropical estuary.pdf.jpgIM Thumbnailimage/jpeg9770http://repository.udem.edu.co/bitstream/11407/4324/2/4.%20Study%20of%20Atrato%20river%20plume%20in%20a%20tropical%20estuary.pdf.jpg713717520d252151218ad17484a334abMD52ORIGINAL4. Study of Atrato river plume in a tropical estuary.pdf4. Study of Atrato river plume in a tropical estuary.pdfapplication/pdf1769381http://repository.udem.edu.co/bitstream/11407/4324/1/4.%20Study%20of%20Atrato%20river%20plume%20in%20a%20tropical%20estuary.pdf9b3eba038789c3ae1716a8b31b2f6974MD5111407/4324oai:repository.udem.edu.co:11407/43242020-05-27 17:52:44.463Repositorio Institucional Universidad de Medellinrepositorio@udem.edu.co

Study of Atrato river plume in a tropical estuary: Effects of the wind and tidal regime on the Gulf of Uraba, Colombia [Estudio de la pluma del río Atrato en un estuario en el trópico: Efectos del viento y del régimen de mareas en el Golfo de Urabá, Colombia]

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