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Journal articles on the topic 'Estuaire inverse'

Author: Grafiati

Published: 20 July 2024

Last updated: 31 July 2025

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1

Descroix, Luc, Yancouba Sané, Mamadou Thior, et al. "Inverse Estuaries in West Africa: Evidence of the Rainfall Recovery?" Water 12, no. 3 (2020): 647. http://dx.doi.org/10.3390/w12030647.

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In West Africa, as in many other estuaries, enormous volumes of marine water are entering the continent. Fresh water discharge is very low, and it is commonly strongly linked to rainfall level. Some of these estuaries are inverse estuaries. During the Great Sahelian Drought (1968–1993), their hyperhaline feature was exacerbated. This paper aims to describe the evolution of the two main West African inverse estuaries, those of the Saloum River and the Casamance River, since the end of the drought. Water salinity measurements were carried out over three to five years according to the sites in or

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2

Shaha, Dinesh Chandra, Yang-Ki Cho, Bong Guk Kim, M. Rafi Afruz Sony, Sampa Rani Kundu, and M. Faruqul Islam. "Spatiotemporal variation of Van der Burgh's coefficient in a salt plug estuary." Hydrology and Earth System Sciences 21, no. 9 (2017): 4563–72. http://dx.doi.org/10.5194/hess-21-4563-2017.

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Abstract. Salt water intrusion in estuaries is expected to become a serious global issue due to climate change. Van der Burgh's coefficient, K, is a good proxy for describing the relative contribution of tide-driven and gravitational (discharge-driven and density-driven) components of salt transport in estuaries. However, debate continues over the use of the K value for an estuary where K should be a constant, spatially varying, or time-independent factor for different river discharge conditions. In this study, we determined K during spring and neap tides in the dry (< 30 m−3 s−1) and wet (

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3

Lorenz, Marvin, Knut Klingbeil, and Hans Burchard. "Impact of Evaporation and Precipitation on Estuarine Mixing." Journal of Physical Oceanography 51, no. 4 (2021): 1319–33. http://dx.doi.org/10.1175/jpo-d-20-0158.1.

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AbstractRecent studies could link the quantities of estuarine exchange flows to the volume-integrated mixing inside an estuary, where mixing is defined as the destruction of salinity variance. The existing mixing relations quantify mixing inside an estuary by the net boundary fluxes of volume, salinity, and salinity variance, which are quantified as Knudsen or total exchange flow bulk values. So far, river runoff is the only freshwater flux included, and the freshwater exchange due to precipitation and evaporation is neglected. Yet, the latter is the driving force of inverse estuaries, which c

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4

BITTENCOURT, ABÍLIO C. S. P., GUILHERME C. LESSA, JOSÉ M. L. DOMINGUEZ, LOUIS MARTIN, GERALDO S. VILAS BÔAS, and FÉLIX F. FARIAS. "High and low frequency erosive and constructive cycles in estuarine beaches: an example from Garcez Point, Bahia/Brazil." Anais da Academia Brasileira de Ciências 73, no. 4 (2001): 599–610. http://dx.doi.org/10.1590/s0001-37652001000400013.

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Monitoring of the morphodynamic variations of the beaches associated with an estuary contiguous with Garcez Point, Bahia, Brazil, and the superposition of aerial photographs from the region, show the presence of distinctive erosive and constructive cycles of low and high frequencies. Between 1959 and 1989, one event of shoreline erosion and progradation was recognized on the oceanic beaches just outside the estuary. Inside the estuary, an erosion phase at the southern margin coincides with a constructive phase at the other side, and vice-versa. On the southern estuarine beach, low-frequency cy

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5

Miller, A. Whitman, Jim R. Muirhead, Amanda C. Reynolds, Mark S. Minton, and Karl J. Klug. "High-frequency continuous measurements reveal strong diel and seasonal cycling of pCO₂ and CO₂ flux in a mesohaline reach of the Chesapeake Bay." Biogeosciences 21, no. 16 (2024): 3717–34. http://dx.doi.org/10.5194/bg-21-3717-2024.

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Abstract. We estimated hourly air–water gas transfer velocities (k600) for carbon dioxide in the Rhode River, a mesohaline sub-estuary of the Chesapeake Bay. Gas transfer velocities were calculated from estuary-specific parameterizations developed explicitly for shallow microtidal estuaries in the mid-Atlantic region of the United States, using standardized wind speed measurements. Combining the gas transfer velocity with continuous measurements of pCO2 in the water and in the overlying atmosphere, we determined the direction and magnitude of CO2 flux at hourly intervals across a 3-year record

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6

Panfili, Jacques, Jean-Dominique Durand, Khady Diop, Béatrice Gourène, and Monique Simier. "Fluctuating asymmetry in fish otoliths and heterozygosity in stressful estuarine environments (West Africa)." Marine and Freshwater Research 56, no. 5 (2005): 505. http://dx.doi.org/10.1071/mf04138.

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Fluctuating asymmetry (FA) is assumed to reflect the developmental instability caused by environmental or genetic stress. Fish otoliths represent a very good tool for investigating the consequence of different effects on FA. Otolith FA analysis, coupled with genetic analysis, has been undertaken on two common West African estuarine species, Ethmalosa fimbriata (EFI) and Sarotherodon melanotheron (SME), in two neighbouring estuaries, in order to highlight the impact of salinity on developmental stability. The Gambia estuary has a normal functioning and the Saloum estuary is inverse (saltier wat

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7

Hofmann, A. F., F. J. R. Meysman, K. Soetaert, and J. J. Middelburg. "Factors governing the pH in a heterotrophic, turbid, tidal estuary." Biogeosciences Discussions 6, no. 1 (2009): 197–240. http://dx.doi.org/10.5194/bgd-6-197-2009.

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Abstract. A method to quantify the influence of kinetically modelled biogeochemical processes on the pH of an ecosystem with time variable acid-base dissociation constants is presented and applied to the heterotrophic, turbid Scheldt estuary (SW Netherlands, N Belgium). Nitrification is identified as the main process governing the pH profile of this estuary, while CO2 degassing and advective-dispersive transport "buffer" the effect of nitrification. CO2 degassing accounts for the largest proton turnover per year in the whole estuary. There is a clear inverse correlation between oxygen turnover

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8

Medeiros, AMA, JEL Barbosa, PR Medeiros, RM Rocha, and LF Silva. "Salinity and freshwater discharge determine rotifer distribution at the Mossoró River Estuary (Semiarid Region of Brazil)." Brazilian Journal of Biology 70, no. 3 (2010): 551–57. http://dx.doi.org/10.1590/s1519-69842010000300011.

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The present study aimed at evaluating differences in rotifer distribution in three estuarine zones in an inverse estuary located in the Semiarid Region of Brazil. Zones were chosen based on their proximity to the ocean and river border as a means of reflecting a horizontal salinity gradient. High freshwater discharge during the rainy season was the major determinant of rotifer composition. On the other hand, due to higher salinity values during the dry season, very low values of species richness and abundance were observed in all zones. Therefore, the study highlights the constraints of salini

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9

Cai, Huayang, Ping Zhang, Erwan Garel, et al. "A novel approach for the assessment of morphological evolution based on observed water levels in tide-dominated estuaries." Hydrology and Earth System Sciences 24, no. 4 (2020): 1871–89. http://dx.doi.org/10.5194/hess-24-1871-2020.

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Abstract. Assessing the impacts of both natural (e.g. tidal forcing from the ocean) and human-induced changes (e.g. dredging for navigation and land reclamation) on estuarine morphology is particularly important for the protection and management of the estuarine environment. In this study, a novel analytical approach is proposed for the assessment of estuarine morphological evolution in terms of tidally averaged depth on the basis of the observed water levels along the estuary. The key lies in deriving a relationship between wave celerity and tidal damping or amplification. For given observed

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10

Burchard, Hans. "Combined Effects of Wind, Tide, and Horizontal Density Gradients on Stratification in Estuaries and Coastal Seas." Journal of Physical Oceanography 39, no. 9 (2009): 2117–36. http://dx.doi.org/10.1175/2009jpo4142.1.

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Abstract The aim of this one-dimensional water column study is to combine modified versions of three characteristic parameters for periodic tidal flow under the influence of a longitudinal buoyancy gradient—the horizontal Richardson number, the inverse Strouhal number, and the inverse Ekman number—into a parameter space study, including constant wind forcing from various directions. It is shown how the underlying dynamical equations can be cast into nondimensional form, depending mainly on these three nondimensional parameters plus the relative wind speed and the wind direction. Idealized mode

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11

Abdul Aziz, Nandi, Yonvitner, Sigid Hariyadi, Syamsul Bahri Agus, and I. Wayan Nurjaya. "Sedimentation Profile in Coastal Water Jakarta Bay." Journal of Tropical Fisheries Management 6, no. 1 (2023): 35–44. http://dx.doi.org/10.29244/jppt.v6i1.43452.

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The waters of Jakarta Bay are one of the waters that are influenced by several fresh water flows that enter from the DKI Jakarta area and its surroundings. Sediment that enters the waters of Jakarta Bay is produced by the activities of the people who live in the Jakarta area and its surroundings. This study aims to analyze the sedimentation and distribution of suspended solids in the Jakarta Bay estuary using an observational approach and spatial analysis. This study uses the Inverse Distance Weighting (IDW) interpolation method. The dominant distribution of sediment in Jakarta Bay is sand wit

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12

Hein, Sebastian S. V., Vanessa Sohrt, Edgar Nehlsen, Thomas Strotmann, and Peter Fröhle. "Tidal Oscillation and Resonance in Semi-Closed Estuaries—Empirical Analyses from the Elbe Estuary, North Sea." Water 13, no. 6 (2021): 848. http://dx.doi.org/10.3390/w13060848.

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Many tidal influenced estuaries and coastal basins feature tidal amplification because of, e.g., convergence and reflection. Increasing amplification rates were observed in the Elbe estuary, with consequences for construction measures, nautical manoeuvring, flood protection, riverbed morphology and ecosystems. Although many studies were conducted investigating the tidal wave transformation in estuaries, studies based on spatially well-distributed empirical data covering periods over more than a year are rare. To fill this gap, a self-developed adapted harmonic analysis method of least squares

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13

Cai, H., H. H. G. Savenije, and C. Jiang. "Analytical approach for predicting fresh water discharge in an estuary based on tidal water level observations." Hydrology and Earth System Sciences 18, no. 10 (2014): 4153–68. http://dx.doi.org/10.5194/hess-18-4153-2014.

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Abstract. As the tidal wave propagates into an estuary, the tidally averaged water level tends to rise in landward direction due to the density difference between saline and fresh water and the asymmetry of the friction. The effect of friction on the residual slope is even more remarkable when accounting for fresh water discharge. In this study, we investigate the influence of river discharge on tidal wave propagation in the Yangtze estuary with specific attention to residual water level slope. This is done by using a one-dimensional analytical model for tidal hydrodynamics accounting for the

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14

Cai, H., H. H. G. Savenije, and C. Jiang. "Analytical approach for predicting fresh water discharge in an estuary based on tidal water level observations." Hydrology and Earth System Sciences Discussions 11, no. 6 (2014): 7053–87. http://dx.doi.org/10.5194/hessd-11-7053-2014.

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Abstract. As the tidal wave propagates into an estuary, the tidally averaged water level tends to rise in landward direction due to the density difference between saline and fresh water and the asymmetry of the friction. The effect of friction on the residual slope is even more remarkable when accounting for fresh water discharge. In this study, we investigate the influence of river discharge on tidal wave propagation in the Yangtze estuary with specific attention to residual water level slope. This is done by using a one-dimensional analytical model for tidal hydrodynamics accounting for the

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15

Lau, Clive L. F., and David K. Jacobs. "Introgression between ecologically distinct species following increased salinity in the Colorado Delta- Worldwide implications for impacted estuary diversity." PeerJ 5 (December 12, 2017): e4056. http://dx.doi.org/10.7717/peerj.4056.

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We investigate hybridization and introgression between ecologically distinct sister species of silverside fish in the Gulf of California through combined analysis of morphological, sequence, and genotypic data. Water diversions in the past century turned the Colorado River Delta from a normal estuary to a hypersaline inverse estuary, raising concerns for the local fauna, much of which is endangered. Salinity differences are known to generate ecological species pairs and we anticipated that loss of the fresher-water historic salinity regime could alter the adaptive factors maintaining distincti

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16

Bange, Hermann W., Chun Hock Sim, Daniel Bastian, et al. "Nitrous oxide (N<sub>2</sub>O) and methane (CH<sub>4</sub>) in rivers and estuaries of northwestern Borneo." Biogeosciences 16, no. 22 (2019): 4321–35. http://dx.doi.org/10.5194/bg-16-4321-2019.

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Abstract. Nitrous oxide (N2O) and methane (CH4) are atmospheric trace gases which play important roles in the climate and atmospheric chemistry of the Earth. However, little is known about their emissions from rivers and estuaries, which seem to contribute significantly to the atmospheric budget of both gases. To this end concentrations of N2O and CH4 were measured in the Rajang, Maludam, Sebuyau and Simunjan rivers draining peatland in northwestern (NW) Borneo during two campaigns in March and September 2017. The Rajang River was additionally sampled in August 2016 and the Samunsam and Semata

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17

Rochelle-Newall, E. J., V. T. Chu, O. Pringault, et al. "Phytoplankton diversity and productivity in a highly turbid, tropical coastal system (Bach Dang Estuary, Vietnam)." Biogeosciences Discussions 8, no. 1 (2011): 487–525. http://dx.doi.org/10.5194/bgd-8-487-2011.

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Abstract. The factors controlling estuarine phytoplankton diversity and production are relatively well known in temperate systems. Less however is known about the factors affecting phytoplankton community distribution in tropical estuaries. This is surprising given the economic and ecological importance of these large, deltaic ecosystems, such as are found in South East Asia. Here we present the results from an investigation into the factors controlling phytoplankton distribution and phytoplankton-bacterial coupling in the Bach Dang Estuary, a sub-estuary of the Red River system, in Northern V

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18

Sebastian, Syriac, Roy George, and K. T. Damodaran. "Studies on the Distribution of Organic Matter and Carbonate Content of Sediments in Mahe Estuary, Northern Kerala." Journal Geological Society of India 36, no. 6 (1990): 634–43. http://dx.doi.org/10.17491/jgsi/1990/360608.

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Abstract Sediment samples collected from selected stations in the Mahe estuary during the pre- and post-monsoon periods were analysed for their texture, organic matter and carbonate content. It is observed that finer sediments, mainly clayey silt, constitute the major part of the estuarine substratum. Organic matter in the bulk sediments generally follows the distribution pattern of the sediments, i.e., finer the texture greater the organic matter content, whereas the carbonate content shows an inverse relation with the texture. Studies on seasonal variations show that the post-monsoon sedimen

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19

R. Nagalakshmi, Aswath Balaji V., V. Saichand, and Pravakar Mishra. "WATER QUALITY INVESTIGATION USING GIS-BASED INTERPOLATION: A COMPARISON OF THE KOLLIDAM AND PALAR RIVER ESTUARIES." RASAYAN Journal of Chemistry 18, no. 01 (2025): 573–84. https://doi.org/10.31788/rjc.2025.1819083.

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Water is an indispensable renewable resource on earth and the quality of water directly forms the platform for a balanced socio-economic development and cannot be utilized until its quality is assessed. The life of the majority of aquatic plants and animals depends on pH, salinity, and temperature, making them crucial water monitoring parameters. In this current study, the pH, salinity, and water temperature for the Kollidam and Palar River estuary have been assessed using GIS. Interpolation being a vital tool in GIS was used to find the dispersion of pH, Salinity, and Water temperature throug

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20

Gning, Ndombour, François Le Loc'h, Omar T. Thiaw, Catherine Aliaume, and Guy Vidy. "Estuarine resources use by juvenile Flagfin mojarra (Eucinostomus melanopterus) in an inverse tropical estuary (Sine Saloum, Senegal)." Estuarine, Coastal and Shelf Science 86, no. 4 (2010): 683–91. http://dx.doi.org/10.1016/j.ecss.2009.11.037.

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21

Burchard, Hans, and Robert D. Hetland. "Quantifying the Contributions of Tidal Straining and Gravitational Circulation to Residual Circulation in Periodically Stratified Tidal Estuaries." Journal of Physical Oceanography 40, no. 6 (2010): 1243–62. http://dx.doi.org/10.1175/2010jpo4270.1.

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Abstract This numerical modeling study quantifies for the first time the contribution of various processes to estuarine circulation in periodically stratified tidal flow under the impact of a constant horizontal buoyancy gradient. The one-dimensional water column equations with periodic forcing are first cast into nondimensional form, resulting in a multidimensional parameter space spanned by the modified inverse Strouhal number and the modified horizontal Richardson number, as well as relative wind speed and wind direction and the residual runoff. The along-tide momentum equation is then solv

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22

Li, Mingming, and Chunyan Li. "Comparison of Flows through a Tidal Inlet in Late Spring and after the Passage of an Atmospheric Cold Front in Winter Using Acoustic Doppler Profilers and Vessel-Based Observations." Sensors 22, no. 9 (2022): 3478. http://dx.doi.org/10.3390/s22093478.

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This paper discusses the application of acoustic Doppler current profilers (ADCP) for the quantification of transport of water and the underlining physical mechanism. The transport of water through estuaries and tidal inlets is affected by tide, river flow, and wind. It is often assumed that wind effects in such systems are negligible unless under severe weather conditions. This study compares the ADCP-measured flows across a tidal inlet under weak wind conditions in late spring and those after the passage of an atmospheric cold front in winter. The Barataria Pass is a major inlet connecting B

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23

Kämpf, Jochen, Nicholas Payne, and Paul Malthouse. "Marine Connectivity in a Large Inverse Estuary." Journal of Coastal Research 26 (November 2010): 1047–56. http://dx.doi.org/10.2112/jcoastres-d-10-00043.1.

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24

Feng, Jiangang, Huangrong Chen, Hailong Zhang, et al. "Turbidity Estimation from GOCI Satellite Data in the Turbid Estuaries of China’s Coast." Remote Sensing 12, no. 22 (2020): 3770. http://dx.doi.org/10.3390/rs12223770.

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Knowledge of the distribution and variation of water turbidity directly represent important information related to the marine ecology and multiple biogeochemical processes, including sediment transport and resuspension and heat transfer in the upper water layer. In this study, a neural network (NN) approach was applied to derive the water turbidity using the geostationary ocean color imager (GOCI) data in turbid estuaries of the Yellow River and the Yangtze River. The results showed a good agreement between the GOCI-derived turbidity and in situ measured data with a determination coefficient (

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25

Mingelbier, M., F. Lecomte, and J. J. Dodson. "Climate change and abundance cycles of two sympatric populations of smelt (Osmerus mordax) in the middle estuary of the St. Lawrence River, Canada." Canadian Journal of Fisheries and Aquatic Sciences 58, no. 10 (2001): 2048–58. http://dx.doi.org/10.1139/f01-140.

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Commercial catches of two ecologically distinct sympatric smelt (Osmerus mordax) populations segregated along the two shores of the St. Lawrence middle estuary exhibited inverse patterns with periodicities on the order of 30 years. The influence of water level in the St. Lawrence River and air temperature, chosen to reflect variations in hydrology and climate, differed markedly between the two populations. Analyses revealed that both water level and temperature were generally positively related with north-shore smelt landings and negatively related with south-shore smelt landings. For both pop

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26

Karunarathna, Harshinie, Dominic Reeve, and Mark Spivack. "Long-term morphodynamic evolution of estuaries: An inverse problem." Estuarine, Coastal and Shelf Science 77, no. 3 (2008): 385–95. http://dx.doi.org/10.1016/j.ecss.2007.09.029.

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Shen, J., and A. Y. Kuo. "Inverse Estimation of Parameters for an Estuarine Eutrophication Model." Journal of Environmental Engineering 122, no. 11 (1996): 1031–40. http://dx.doi.org/10.1061/(asce)0733-9372(1996)122:11(1031).

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Shen, J., and A. Y. Kuo. "Application of Inverse Method to Calibrate Estuarine Eutrophication Model." Journal of Environmental Engineering 124, no. 5 (1998): 409–18. http://dx.doi.org/10.1061/(asce)0733-9372(1998)124:5(409).

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Lavı́n, M. F., V. M. Godı́nez, and L. G. Alvarez. "Inverse-estuarine Features of the Upper Gulf of California." Estuarine, Coastal and Shelf Science 47, no. 6 (1998): 769–95. http://dx.doi.org/10.1006/ecss.1998.0387.

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Messer, Lauren F., Mark V. Brown, Paul D. Van Ruth, Mark Doubell, and Justin R. Seymour. "Temperate southern Australian coastal waters are characterised by surprisingly high rates of nitrogen fixation and diversity of diazotrophs." PeerJ 9 (March 1, 2021): e10809. http://dx.doi.org/10.7717/peerj.10809.

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Biological dinitrogen (N2) fixation is one mechanism by which specific microorganisms (diazotrophs) can ameliorate nitrogen (N) limitation. Historically, rates of N2 fixation were believed to be limited outside of the low nutrient tropical and subtropical open ocean; however, emerging evidence suggests that N2 fixation is also a significant process within temperate coastal waters. Using a combination of amplicon sequencing, targeting the nitrogenase reductase gene (nifH), quantitative nifH PCR, and 15N2 stable isotope tracer experiments, we investigated spatial patterns of diazotroph assemblag

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31

Nunes Vaz, Richard A., Geoffrey W. Lennon, and David G. Bowers. "Physical behaviour of a large, negative or inverse estuary." Continental Shelf Research 10, no. 3 (1990): 277–304. http://dx.doi.org/10.1016/0278-4343(90)90023-f.

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Adama, Gueye, Badiane Insa, Youm Cheikh Ibrahima, Sow El Hadji, and Fofana Cheikh Abdoul Kader. "Les Diatomées Sub-fossiles de L’estuaire du Saloum, Sénégal: inventaire floristique et paléo-environnement fournis par la carotte de Ndangane Babou." European Scientific Journal, ESJ 18, no. 33 (2022): 55. http://dx.doi.org/10.19044/esj.2022.v18n33p55.

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Dans le programme de reconstitution de l’histoire des estuaires et lagunes du Sénégal et de l’inventaire de la microflore à diatomées de la Séné-Gambie, une carotte de sondage de 400 cm de long a été réalisée à Ndangane Babou sur un des bras de l’estuaire du Saloum (14°07′53.86″ N/16°17′40.08″ W) à 95 km de l’embouchure. L’analyse comparée de la lithologie et de la microflore a montré une corrélation significative entre la fraction pélitique, l’abondance absolue des diatomées et leur diversité spécifique. Le faible taux de sable, majoritairement d’origine marine tout au long de la carotte pour

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Nunes, RA, and GW Lennon. "Physical property distributions and seasonal trends in Spencer Gulf, South Australia: an inverse estuary." Marine and Freshwater Research 37, no. 1 (1986): 39. http://dx.doi.org/10.1071/mf9860039.

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Results are described from the first long-term, systematic program of oceanographic measurements in Spencer Gulf, South Australia. The gulf belongs to a subset of semi-enclosed seas that are characterized by a net fluid loss, in this case induced by excess evaporation, and a resulting circulation that is the reverse of that found in a classical estuary. In Spencer Gulf, this inverse estuary character involves the production of salinities as high as 48 at the head in late summer. The seasonal variations of temperature and salinity, from both large-scale CTD surveys and time-series observations

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Veeh, H. Herbert, Willard S. Moore, and Stephen V. Smith. "The behaviour of uranium and radium in an inverse estuary." Continental Shelf Research 15, no. 13 (1995): 1569–83. http://dx.doi.org/10.1016/0278-4343(95)00031-u.

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Suteja, Yulianto, Anna Ida Sunaryo Purwiyanto, and Fitri Agustriani. "Merkuri (Hg) di Permukaan Perairan Muara Sungai Banyuasin, Sumatera Selatan, Indonesia." Journal of Marine and Aquatic Sciences 5, no. 2 (2018): 177. http://dx.doi.org/10.24843/jmas.2019.v05.i02.p03.

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The purposes of this study were to determine the water quality, concentration and distribution of Hg in the surface water of Banyuasin river estuary. This research was conducted in June 2016 with 26 sampling stations. Measurement of in situ water quality was done using Conductivity Temperature Depth (CTD) multiparameter profiler while Hg metal was measured using Atomic Absorption Spectroscopy (AAS). The data obtained was interpolated by Inverse Distance Weighted (IDW) and then mapped spatially. The results showed that in general the water quality in Banyuasin river estuary still meets the seaw

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Diadhiou, H. D., P. Diop, I. Diedhiou, and A. B. Badji. "Variations inter annuelles de la production de la crevette géante tigrée <i>Penaeus</i> Monodon fabricius, 1798 (<i>penaeidae</i>) pêchée dans l’estuaire de Casamance, au Sénégal." Journal de la Recherche Scientifique de l’Université de Lomé 26, no. 1 (2024): 25–39. http://dx.doi.org/10.4314/jrsul.v26i1.5.

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La crevette géante tigrée, Penaeus monodon (Fabricius, 1798) est pêchée de façon régulière dans l’estuaire inversé de Casamance depuis 2012 par les pêcheurs migrants maliens. Sa présence dans cet estuaire est atypique, car ce n’est pas son habitat naturel. Les principales zones de pêche pour cette ressource sont les affluents et le cours principal de l'estuaire de Casamance, s'étendant de l'embouchure des cours d'eau à la ville de Ziguinchor. Dans cette zone, la crevette géante tigrée est capturée à l'aide d'un filet maillant dérivant de fond, qui est également utilisé pour la pêche du Drepane

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Messer, LF, M. Doubell, TC Jeffries, MV Brown, and JR Seymour. "Prokaryotic and diazotrophic population dynamics within a large oligotrophic inverse estuary." Aquatic Microbial Ecology 74, no. 1 (2015): 1–15. http://dx.doi.org/10.3354/ame01726.

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Winant, Clinton D., and Guillermo Gutiérrez de Velasco. "Tidal Dynamics and Residual Circulation in a Well-Mixed Inverse Estuary." Journal of Physical Oceanography 33, no. 7 (2003): 1365–79. http://dx.doi.org/10.1175/1520-0485(2003)033<1365:tdarci>2.0.co;2.

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Gutiérrez de Velasco, Guillermo, and Clinton D. Winant. "Wind- and Density-Driven Circulation in a Well-Mixed Inverse Estuary." Journal of Physical Oceanography 34, no. 5 (2004): 1103–16. http://dx.doi.org/10.1175/1520-0485(2004)034<1103:wadcia>2.0.co;2.

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Lennon, G. W., D. G. Bowers, R. A. Nunes, et al. "Gravity currents and the release of salt from an inverse estuary." Nature 327, no. 6124 (1987): 695–97. http://dx.doi.org/10.1038/327695a0.

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Jendyk, Jan, Deevesh A. Hemraj, Melissa H. Brown, Amanda V. Ellis, and Sophie C. Leterme. "Environmental variability and phytoplankton dynamics in a South Australian inverse estuary." Continental Shelf Research 91 (December 2014): 134–44. http://dx.doi.org/10.1016/j.csr.2014.08.009.

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Denis, Jérémy, Khalef Rabhi, François Le Loc’h, et al. "Role of estuarine habitats for the feeding ecology of the European eel (Anguilla anguilla L.)." PLOS ONE 17, no. 7 (2022): e0270348. http://dx.doi.org/10.1371/journal.pone.0270348.

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This study aims to characterize and compare the feeding ecology of the European eels (Anguilla anguilla L.) during the continental phase (i.e. yellow and silver) along a salinity gradient (i.e. lower, middle and upper) in six northern France estuaries (i.e. brackish water). The diet and stable isotopic (i.e. δ15N and δ13C values) compositions of eels collected with a fyke net in six estuaries (Slack, Wimereux, Liane, Canche, Authie and Somme estuaries) located along the French coast of the eastern English Channel per season over a year were described by combining gut content and stable isotope

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Otsuka, Amanda Yumi, Fernando Antônio do Nascimento Feitosa, Manuel de Jesus Flores Montes та Alex Costa da Silva. "Influence of fluvial discharge on the dynamics of Chlorophyll-α in the continental shelf adjacent to the Recife Port Basin (Pernambuco-Brazil)". Brazilian Journal of Oceanography 66, № 1 (2018): 91–103. http://dx.doi.org/10.1590/s1679-87592018149106601.

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Abstract This study was undertaken in the coastal zone of the state of Pernambuco adjacent to the Recife port area, which corresponds to the inner shelf. This research aimed to analyze the dynamics of chlorophyll-a and several other environmental variables. Sampling was undertaken bimonthly on the surface from September 11th to May 10th, thus including the rainy and dry periods, and during low tide in spring tide. The parameters analyzed were chlorophyll-a, salinity, temperature, transparency, dissolved oxygen, oxygen saturation rate, pH, suspended solids, dissolved inorganic nutrients. Phytop

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Nunes-Vaz, Richard A. "The salinity response of an inverse estuary to climate change & desalination." Estuarine, Coastal and Shelf Science 98 (February 2012): 49–59. http://dx.doi.org/10.1016/j.ecss.2011.11.023.

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Passadore, Cecilia, Luciana Möller, Fernando Diaz-Aguirre, and Guido J. Parra. "Demography of southern Australian bottlenose dolphins living in a protected inverse estuary." Aquatic Conservation: Marine and Freshwater Ecosystems 27, no. 6 (2017): 1186–97. http://dx.doi.org/10.1002/aqc.2772.

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Petrusevics, PM. "SST fronts in inverse estuaries, South Australia-indicators of reduced gulf-shlef exchange." Marine and Freshwater Research 44, no. 2 (1993): 305. http://dx.doi.org/10.1071/mf9930305.

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During the austral summer, the entrance to the South Australian gulfs exhibits sea surface temperature (SST) fronts of between 3 and 3.5°C that are clearly discernible on NOAA/AVHRR imagery. The surface fronts are formed by seasonal juxtaposition of relatively warm gulf and cooler bight water. Field surveys indicate that the SST fronts coexist with and overlay strong benthic temperature and salinity differentials of 74°C and 1.2-1.5, respectively. Density variation in the entrance to both gulfs exhibits a density minimum at all depths and suggests bottom convergence of density currents that ef

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Lomakin, P. D. "Investigation of the field of colored dissolved organic matter concentration and its relationship to the salinity field in Dnieper-Bug estuary." Monitoring systems of environment, no. 2 (June 24, 2021): 72–80. http://dx.doi.org/10.33075/2220-5861-2021-2-72-80.

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Based on the data of the expedition carried out in August 2012, the features of the structure of the salinity and fDOM concentration fields, as well as the correlation between these values in the Dnieper-Bug estuary, are analyzed. It is shown that the salinity field in the Dnieper-Bug estuary is characterized by all structural features typical of coastal sea areas freshened by river runoff, while the fDOM concentration field has anomalous properties due to the presence of an anthropogenic component of this value. The presence of fDOM of anthropogenic origin is most significant in the western

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Corlis, Nicholas J., H. Herbert Veeh, John C. Dighton та Andrew L. Herczeg. "Mixing and evaporation processes in an inverse estuary inferred from δ2H and δ18O". Continental Shelf Research 23, № 8 (2003): 835–46. http://dx.doi.org/10.1016/s0278-4343(03)00029-3.

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Petrusevics, P., J. A. T. Bye, V. Fahlbusch, J. Hammat, D. R. Tippins, and E. van Wijk. "High salinity winter outflow from a mega inverse-estuary—the Great Australian Bight." Continental Shelf Research 29, no. 2 (2009): 371–80. http://dx.doi.org/10.1016/j.csr.2008.10.003.

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Parolin, Radael de Souza, Antônio José da Silva Neto, Pedro Paulo Gomes Watts Rodrigues, and Orestes Llanes Santiago. "Estimation of a contaminant source in an estuary with an inverse problem approach." Applied Mathematics and Computation 260 (June 2015): 331–41. http://dx.doi.org/10.1016/j.amc.2015.03.054.

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