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Relevant bibliographies by topics / Panama Bight

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Academic literature on the topic 'Panama Bight'

Author: Grafiati

Published: 4 June 2025

Last updated: 1 August 2025

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Journal articles on the topic "Panama Bight"

1

Torres, Rafael R., Estefanía Giraldo, Cristian Muñoz, Ana Caicedo, Ismael Hernández-Carrasco, and Alejandro Orfila. "Seasonal and El Niño–Southern Oscillation-related ocean variability in the Panama Bight." Ocean Science 19, no. 3 (2023): 685–701. http://dx.doi.org/10.5194/os-19-685-2023.

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Abstract. In the Panama Bight, two different seasonal surface circulation patterns coincide with a strong mean sea level variation, as observed from 27 years of absolute dynamic topography (ADT) and the use of self-organizing maps. From January to April, a cyclonic gyre with a strong southwestward Panama Jet Surface Current (PJSC) dominates the basin circulation, forced by the Panama surface wind jet that also produces upwelling, reducing sea surface temperature (SST), increasing sea surface salinity (SSS) and causing an ADT decrease. From June to December, the Choco surface wind jet enhances

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2

Spear, Larry B., and David G. Ainley. "Seabirds of the Panama Bight." Waterbirds: The International Journal of Waterbird Biology 22, no. 2 (1999): 175. http://dx.doi.org/10.2307/1522207.

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Whitaker, Justin W., and Eric D. Maloney. "Genesis of an East Pacific Easterly Wave from a Panama Bight MCS: A Case Study Analysis from June 2012." Journal of the Atmospheric Sciences 77, no. 10 (2020): 3567–84. http://dx.doi.org/10.1175/jas-d-20-0032.1.

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AbstractThis study investigates the transition of a Panama Bight mesoscale convective system (MCS) into the easterly wave (EW) that became Hurricane Carlotta (2012). Reanalysis, observations, and a convective-permitting Weather Research and Forecasting (WRF) Model simulation are used to analyze the processes contributing to EW genesis. A vorticity budget analysis shows that convective coupling and vortex stretching are very important to the transition in this case, while horizontal advection is mostly responsible for the propagation of the system. In the model, the disturbance is dominated by

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Corredor-Acosta, Andrea, Náyade Cortés-Chong, Alberto Acosta, et al. "Spatio-Temporal Variability of Chlorophyll-A and Environmental Variables in the Panama Bight." Remote Sensing 12, no. 13 (2020): 2150. http://dx.doi.org/10.3390/rs12132150.

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The analysis of synoptic satellite data of total chlorophyll-a (Chl-a) and the environmental drivers that influence nutrient and light availability for phytoplankton growth allows us to understand the spatio-temporal variability of phytoplankton biomass. In the Panama Bight Tropical region (PB; 1–9°N, 79–84°W), the spatial distribution of Chl-a is mostly related to the seasonal wind patterns and the intensity of localized upwelling centers. However, the association between the Chl-a and different physical variables and nutrient availability is still not fully assessed. In this study, we evalua

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Herrera Carmona, Julio César, John Josephraj Selvaraj, and Alan Giraldo. "Dynamic regionalization of the Panama Bight, Eastern Tropical Pacific, using remote sensing data." International Journal of Remote Sensing 43, no. 9 (2022): 3131–51. http://dx.doi.org/10.1080/01431161.2022.2063040.

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6

Pedraza, M. J., and J. A. Díaz Ochoa. "Sea level height, sea surface temperature, and tuna yields in the Panama bight during El Niño." Advances in Geosciences 6 (January 30, 2006): 155–59. http://dx.doi.org/10.5194/adgeo-6-155-2006.

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Abstract. Between 1988 and 1998, annual tuna landings at Buenaventura (Colombian Pacific) are correlated with the sea surface temperature in the central Equatorial Pacific (r=0.78, p<0.05) and the sea level height at Buenaventura (r=0.76, p<0.05) and Balboa (Panama) (r=0.79, p<0.05). Seasonal oceanic upwelling is forced by the Panama wind jet, which may favour oceanic fisheries such as tuna. Here we first apply a bivariate correlation method (Pyper and Peterman, 1994) and then a multivariate approach (principal components analysis or PCA) to investigate the relationships of these envi

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7

Villegas, Nancy, Igor Málikov, and Diana Díaz. "Variabilidad mensual de la velocidad de surgencia y clorofila a en la región del Panama Bight." Revista Mutis 6, no. 2 (2016): 82–94. http://dx.doi.org/10.21789/22561498.1153.

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<p align="justify">Las zonas de surgencia y la presencia de clorofila a en la región del Panamá Bight (golfo de Panamá) fueron comparadas en una escala mensual. Las variables utilizadas fueron la velocidad vertical de surgencia estimada mediante el software EVA. V.2.0 y la concentración de clorofila a obtenida de imágenes satelitales SeaWifs. El estudio fue realizado para el área costera entre 6° 30’ y 2° N y en los tres principales focos de ascenso de agua, el primero ubicado entre 83-84° W y 1° 30’-2° 30’ N, el segundo entre 81-82° W y 1° 30’-2° 30’ N, y el tercero entre 82-83º W y 2°

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Rincón-Díaz, Natalia, Brigitte Gavio, Muñoz Juliana Valentina Sánchez, and Luis Chasqui. "Crouania mageshimensis Itono, 1977 (Ceramiales, Rhodophyta) and three other species new to the Eastern Tropical Pacific." Check List 16, no. (5) (2020): 1171–80. https://doi.org/10.15560/16.5.1171.

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We report new records of four macroalgae species in the Eastern Tropical Pacific, specifically from the rocky reefs of northern Chocó, Colombian Pacific. Among them, three species of Rhodophyta are included—<em>Crouania mageshimensis </em>Itono, 1977; <em>Monosporus indicus </em>Børgesen, 1931; <em>Jania articulata </em>N’Yeurt & Payri, 2009—and one species of Chlorophyta—<em>Ulothrix subflaccida </em>Wille, 1901. The new records increase the knowledge of tropical marine algae in the Pacific, open the discussion about possible dispersal mechanisms, and

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Valencia, Bellineth, and Alan Giraldo. "Structure of hyperiid amphipod assemblages on Isla Gorgona, eastern tropical Pacific off Colombia." Journal of the Marine Biological Association of the United Kingdom 92, no. 7 (2011): 1489–99. http://dx.doi.org/10.1017/s0025315411001780.

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Temporal variation of hyperiid amphipod structure assemblages was studied on Isla Gorgona, eastern tropical Pacific (ETP) off Colombia between September 2005 and August 2006. Forty-six species were found during the entire sampling period:Hyperioides sibaginis, Lestrigonus bengalensis, Phronimopsis spinifera, Tetrathyrus forcipatusandParalycaea gracilisdominated the assemblage, representing 92%. The dendogram based on the Bray–Curtis similarity index showed that the hyperiid assemblages were separated into two groups, which did not coincide with the seasonality described for the ETP (wet versus

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Valencia, Bellineth, Bertha Lavaniegos, Alan Giraldo, and Efraín Rodríguez-Rubio. "Temporal and spatial variation of hyperiid amphipod assemblages in response to hydrographic processes in the Panama Bight, eastern tropical Pacific." Deep Sea Research Part I: Oceanographic Research Papers 73 (March 2013): 46–61. http://dx.doi.org/10.1016/j.dsr.2012.11.009.

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Book chapters on the topic "Panama Bight"

1

Prange, Matthias, Silke Steph, Huadong Liu, Lloyd D. Keigwin, and Michael Schulz. "Hydroclimatic Variability in the Panama Bight Region During Termination 1 and the Holocene." In Integrated Analysis of Interglacial Climate Dynamics (INTERDYNAMIC). Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-00693-2_11.

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Ballesteros-Prada, Angélica. "Modern Benthic Foraminifera “Phylum Foraminifera (D’Orbigny 1826)” of the Panama Bight: A Census Report Based on Thanatocoenoses from the Continental Slope." In Advances in South American Micropaleontology. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-02119-1_9.

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Southwood, T. R. E. "A Sparse Start." In The Story Of Life. Oxford University PressOxford, 2003. http://dx.doi.org/10.1093/oso/9780198525905.003.0008.

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Abstract The supercontinent Pangaea remained intact throughout this period and various small land masses that now constitute South-East Asia moved to join the eastern corner of Laurasia. Although Pangaea stretched from near one pole to near the other it seems that there was no land that was actually over a pole and there is no evidence of continental ice sheets. The ocean currents will have flowed freely, particularly in the enormous Panthalassic (Palaeopacific) Ocean, bringing warm water to colder latitudes. The Tethys Ocean existed as a deep bight, at tropical level, to the eastern side of P

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