LeHavreV1, PascalFrancis, Corpus, bibRecord, 000024

Turbidity maxima in four macrotidal estuaries

Identifieur interne : 000024 ( PascalFrancis/Corpus ); précédent : 000023; suivant : 000025

Turbidity maxima in four macrotidal estuaries

Auteurs : S. B. Mitchell

Source :

Ocean & coastal management [ 0964-5691 ] ; 2013.

RBID : Pascal:13-0253272

Descripteurs français

Pascal (Inist)
- Turbidité, Hydrodynamique, Fraction fine, Transport sédiment, Navigation, Source, Cycle, Eau douce, Ecoulement, Variation saisonnière, Pluie, Bassin versant, Crue, Marée, Courant, Concentration, Matière en suspension, Topographie, Plomb, Estuaire Humber.

English descriptors

KwdEn :
- Humber Estuary, concentration, currents, cycles, drainage basins, fine-grained materials, floods, flow, fresh water, hydrodynamics, lead, navigation, rainfall, seasonal variations, sediment transport, springs, suspended materials, tides, topography, turbidity.

Abstract

Hydrodynamic and fine sediment transport characteristics of four major macrotidal Northern European estuaries are compared. The four estuaries (Weser, Seine, Scheldt, Humber) are amongst those key to navigation and shipping in that they are home to several major European ports (e.g. Hull, Antwerp, Le Havre). In particular, the characteristics and behaviour of the estuarine turbidity maximum are described for each system. While this is a complex topic that continues to benefit from ongoing research, some similarities exist between the estuaries in terms of the response of the turbidity maximum to changes in tidal range (during the neap-spring-neap cycle) and fresh water flow (due to seasonal variations in rainfall in the catchments). The hydrodynamics of the four estuaries are very similar, and are characterised by faster, shorter flood tide currents compared with longer, slower ebb tides. Under low fresh water flow conditions, the turbidity maximum is in each case moved upstream, while high fresh water flow conditions cause a net seaward movement of the turbidity maximum. While in general the concentrations of suspended sediment within turbidity maxima are no more than a few hundred milligrams per litre, the particular topography of the Humber estuary system leads to concentrations considerably higher than this.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A15	`01`			`@1 Scholl of Civil Engineering and Surveying, University of Portsmouth, Portland Building @2 Portsmouth PO1 3AH @3 GBR @Z 1 aut.`
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C01	`01`		`ENG`	@0 Hydrodynamic and fine sediment transport characteristics of four major macrotidal Northern European estuaries are compared. The four estuaries (Weser, Seine, Scheldt, Humber) are amongst those key to navigation and shipping in that they are home to several major European ports (e.g. Hull, Antwerp, Le Havre). In particular, the characteristics and behaviour of the estuarine turbidity maximum are described for each system. While this is a complex topic that continues to benefit from ongoing research, some similarities exist between the estuaries in terms of the response of the turbidity maximum to changes in tidal range (during the neap-spring-neap cycle) and fresh water flow (due to seasonal variations in rainfall in the catchments). The hydrodynamics of the four estuaries are very similar, and are characterised by faster, shorter flood tide currents compared with longer, slower ebb tides. Under low fresh water flow conditions, the turbidity maximum is in each case moved upstream, while high fresh water flow conditions cause a net seaward movement of the turbidity maximum. While in general the concentrations of suspended sediment within turbidity maxima are no more than a few hundred milligrams per litre, the particular topography of the Humber estuary system leads to concentrations considerably higher than this.
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C03	`02`	`2`	`FRE`	`@0 Hydrodynamique @5 02`
C03	`02`	`2`	`ENG`	`@0 hydrodynamics @5 02`
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C03	`04`	`2`	`FRE`	`@0 Transport sédiment @5 04`
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C03	`05`	`2`	`ENG`	`@0 navigation @5 05`
C03	`06`	`2`	`FRE`	`@0 Source @5 06`
C03	`06`	`2`	`ENG`	`@0 springs @5 06`
C03	`06`	`2`	`SPA`	`@0 Fuente @5 06`
C03	`07`	`2`	`FRE`	`@0 Cycle @5 07`
C03	`07`	`2`	`ENG`	`@0 cycles @5 07`
C03	`08`	`2`	`FRE`	`@0 Eau douce @5 08`
C03	`08`	`2`	`ENG`	`@0 fresh water @5 08`
C03	`08`	`2`	`SPA`	`@0 Agua dulce @5 08`
C03	`09`	`2`	`FRE`	`@0 Ecoulement @5 09`
C03	`09`	`2`	`ENG`	`@0 flow @5 09`
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C03	`10`	`2`	`ENG`	`@0 seasonal variations @5 10`
C03	`10`	`2`	`SPA`	`@0 Variación estacional @5 10`
C03	`11`	`2`	`FRE`	`@0 Pluie @5 11`
C03	`11`	`2`	`ENG`	`@0 rainfall @5 11`
C03	`11`	`2`	`SPA`	`@0 Lluvia @5 11`
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C03	`12`	`2`	`SPA`	`@0 Cuenca @5 12`
C03	`13`	`2`	`FRE`	`@0 Crue @5 13`
C03	`13`	`2`	`ENG`	`@0 floods @5 13`
C03	`13`	`2`	`SPA`	`@0 Crecida @5 13`
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C03	`14`	`2`	`ENG`	`@0 tides @5 14`
C03	`14`	`2`	`SPA`	`@0 Marea @5 14`
C03	`15`	`2`	`FRE`	`@0 Courant @5 15`
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C03	`16`	`2`	`ENG`	`@0 concentration @5 16`
C03	`16`	`2`	`SPA`	`@0 Concentración @5 16`
C03	`17`	`2`	`FRE`	`@0 Matière en suspension @5 17`
C03	`17`	`2`	`ENG`	`@0 suspended materials @5 17`
C03	`17`	`2`	`SPA`	`@0 Materia en suspensión @5 17`
C03	`18`	`2`	`FRE`	`@0 Topographie @5 18`
C03	`18`	`2`	`ENG`	`@0 topography @5 18`
C03	`18`	`2`	`SPA`	`@0 Topografía @5 18`
C03	`19`	`2`	`FRE`	`@0 Plomb @5 19`
C03	`19`	`2`	`ENG`	`@0 lead @5 19`
C03	`19`	`2`	`SPA`	`@0 Plomo @5 19`
C03	`20`	`2`	`FRE`	`@0 Estuaire Humber @2 NG @5 61`
C03	`20`	`2`	`ENG`	`@0 Humber Estuary @2 NG @5 61`
C03	`20`	`2`	`SPA`	`@0 Estuario Humber @2 NG @5 61`
C07	`01`	`2`	`FRE`	`@0 Humberside @2 NG`
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C07	`02`	`2`	`FRE`	`@0 Angleterre @2 NG`
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Format Inist (serveur)

NO :	PASCAL 13-0253272 INIST
ET :	Turbidity maxima in four macrotidal estuaries
AU :	MITCHELL (S. B.); MITCHELL (Steven B.); UNCLES (Reginald J.)
AF :	School of Civil Engineering and Surveying, University of Portsmouth, Portland Building/Portsmouth PO1 3AH/Royaume-Uni (1 aut.); Scholl of Civil Engineering and Surveying, University of Portsmouth, Portland Building/Portsmouth PO1 3AH/Royaume-Uni (1 aut.); Plymouth Marine Laboratory, Prospect Place/Plymouth PL1 3DH/Royaume-Uni (2 aut.)
DT :	Publication en série; Niveau analytique
SO :	Ocean & coastal management; ISSN 0964-5691; Royaume-Uni; Da. 2013; Vol. 79; Pp. 62-69; Bibl. 3/4 p.
LA :	Anglais
EA :	Hydrodynamic and fine sediment transport characteristics of four major macrotidal Northern European estuaries are compared. The four estuaries (Weser, Seine, Scheldt, Humber) are amongst those key to navigation and shipping in that they are home to several major European ports (e.g. Hull, Antwerp, Le Havre). In particular, the characteristics and behaviour of the estuarine turbidity maximum are described for each system. While this is a complex topic that continues to benefit from ongoing research, some similarities exist between the estuaries in terms of the response of the turbidity maximum to changes in tidal range (during the neap-spring-neap cycle) and fresh water flow (due to seasonal variations in rainfall in the catchments). The hydrodynamics of the four estuaries are very similar, and are characterised by faster, shorter flood tide currents compared with longer, slower ebb tides. Under low fresh water flow conditions, the turbidity maximum is in each case moved upstream, while high fresh water flow conditions cause a net seaward movement of the turbidity maximum. While in general the concentrations of suspended sediment within turbidity maxima are no more than a few hundred milligrams per litre, the particular topography of the Humber estuary system leads to concentrations considerably higher than this.
CC :	001E01P02; 001E01P01; 226C02; 226C01
FD :	Turbidité; Hydrodynamique; Fraction fine; Transport sédiment; Navigation; Source; Cycle; Eau douce; Ecoulement; Variation saisonnière; Pluie; Bassin versant; Crue; Marée; Courant; Concentration; Matière en suspension; Topographie; Plomb; Estuaire Humber
FG :	Humberside; Angleterre; Grande Bretagne; Royaume Uni; Europe Ouest; Europe
ED :	turbidity; hydrodynamics; fine-grained materials; sediment transport; navigation; springs; cycles; fresh water; flow; seasonal variations; rainfall; drainage basins; floods; tides; currents; concentration; suspended materials; topography; lead; Humber Estuary
EG :	Humberside England; England; Great Britain; United Kingdom; Western Europe; Europe
SD :	Turbiedad; Hidrodinámica; Fracción fina; Fuente; Agua dulce; Variación estacional; Lluvia; Cuenca; Crecida; Marea; Concentración; Materia en suspensión; Topografía; Plomo; Estuario Humber
LO :	INIST-16464.354000503053910070
ID :	13-0253272

Links to Exploration step

Pascal:13-0253272

Le document en format XML

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<front><div type="abstract" xml:lang="en">Hydrodynamic and fine sediment transport characteristics of four major macrotidal Northern European estuaries are compared. The four estuaries (Weser, Seine, Scheldt, Humber) are amongst those key to navigation and shipping in that they are home to several major European ports (e.g. Hull, Antwerp, Le Havre). In particular, the characteristics and behaviour of the estuarine turbidity maximum are described for each system. While this is a complex topic that continues to benefit from ongoing research, some similarities exist between the estuaries in terms of the response of the turbidity maximum to changes in tidal range (during the neap-spring-neap cycle) and fresh water flow (due to seasonal variations in rainfall in the catchments). The hydrodynamics of the four estuaries are very similar, and are characterised by faster, shorter flood tide currents compared with longer, slower ebb tides. Under low fresh water flow conditions, the turbidity maximum is in each case moved upstream, while high fresh water flow conditions cause a net seaward movement of the turbidity maximum. While in general the concentrations of suspended sediment within turbidity maxima are no more than a few hundred milligrams per litre, the particular topography of the Humber estuary system leads to concentrations considerably higher than this.</div>
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<s5>04</s5>
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<s5>06</s5>
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<fC03 i1="06" i2="2" l="ENG"><s0>springs</s0>
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</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>fresh water</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Agua dulce</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Ecoulement</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>flow</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Variation saisonnière</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>seasonal variations</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Variación estacional</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Pluie</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>rainfall</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Lluvia</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Bassin versant</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>drainage basins</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Cuenca</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Crue</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>floods</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Crecida</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Marée</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>tides</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Marea</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Courant</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>currents</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Concentration</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>concentration</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Concentración</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Matière en suspension</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>suspended materials</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Materia en suspensión</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Topographie</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>topography</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Topografía</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Plomb</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>lead</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Plomo</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Estuaire Humber</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>Humber Estuary</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Estuario Humber</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Humberside</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Humberside England</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Angleterre</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>England</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Inglaterra</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Grande Bretagne</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Great Britain</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Gran Bretaña</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Royaume Uni</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>United Kingdom</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Reino Unido</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Europe Ouest</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Western Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Europa del Oeste</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="06" i2="2" l="SPA"><s0>Europa</s0>
<s2>564</s2>
</fC07>
<fN21><s1>245</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 13-0253272 INIST</NO>
<ET>Turbidity maxima in four macrotidal estuaries</ET>
<AU>MITCHELL (S. B.); MITCHELL (Steven B.); UNCLES (Reginald J.)</AU>
<AF>School of Civil Engineering and Surveying, University of Portsmouth, Portland Building/Portsmouth PO1 3AH/Royaume-Uni (1 aut.); Scholl of Civil Engineering and Surveying, University of Portsmouth, Portland Building/Portsmouth PO1 3AH/Royaume-Uni (1 aut.); Plymouth Marine Laboratory, Prospect Place/Plymouth PL1 3DH/Royaume-Uni (2 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Ocean & coastal management; ISSN 0964-5691; Royaume-Uni; Da. 2013; Vol. 79; Pp. 62-69; Bibl. 3/4 p.</SO>
<LA>Anglais</LA>
<EA>Hydrodynamic and fine sediment transport characteristics of four major macrotidal Northern European estuaries are compared. The four estuaries (Weser, Seine, Scheldt, Humber) are amongst those key to navigation and shipping in that they are home to several major European ports (e.g. Hull, Antwerp, Le Havre). In particular, the characteristics and behaviour of the estuarine turbidity maximum are described for each system. While this is a complex topic that continues to benefit from ongoing research, some similarities exist between the estuaries in terms of the response of the turbidity maximum to changes in tidal range (during the neap-spring-neap cycle) and fresh water flow (due to seasonal variations in rainfall in the catchments). The hydrodynamics of the four estuaries are very similar, and are characterised by faster, shorter flood tide currents compared with longer, slower ebb tides. Under low fresh water flow conditions, the turbidity maximum is in each case moved upstream, while high fresh water flow conditions cause a net seaward movement of the turbidity maximum. While in general the concentrations of suspended sediment within turbidity maxima are no more than a few hundred milligrams per litre, the particular topography of the Humber estuary system leads to concentrations considerably higher than this.</EA>
<CC>001E01P02; 001E01P01; 226C02; 226C01</CC>
<FD>Turbidité; Hydrodynamique; Fraction fine; Transport sédiment; Navigation; Source; Cycle; Eau douce; Ecoulement; Variation saisonnière; Pluie; Bassin versant; Crue; Marée; Courant; Concentration; Matière en suspension; Topographie; Plomb; Estuaire Humber</FD>
<FG>Humberside; Angleterre; Grande Bretagne; Royaume Uni; Europe Ouest; Europe</FG>
<ED>turbidity; hydrodynamics; fine-grained materials; sediment transport; navigation; springs; cycles; fresh water; flow; seasonal variations; rainfall; drainage basins; floods; tides; currents; concentration; suspended materials; topography; lead; Humber Estuary</ED>
<EG>Humberside England; England; Great Britain; United Kingdom; Western Europe; Europe</EG>
<SD>Turbiedad; Hidrodinámica; Fracción fina; Fuente; Agua dulce; Variación estacional; Lluvia; Cuenca; Crecida; Marea; Concentración; Materia en suspensión; Topografía; Plomo; Estuario Humber</SD>
<LO>INIST-16464.354000503053910070</LO>
<ID>13-0253272</ID>
</server>
</inist>
</record>

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Turbidity maxima in four macrotidal estuaries

Turbidity maxima in four macrotidal estuaries

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