AustralieFrV1, PascalFrancis, Corpus, bibRecord, 003E43

Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia

Identifieur interne : 003E43 ( PascalFrancis/Corpus ); précédent : 003E42; suivant : 003E44

Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia

Auteurs : Bruno Castelle ; Julien Bourget ; Nathalie Molnar ; Darrell Strauss ; Sophie Deschamps ; Rodger Tomlinson

Source :

Coastal engineering [ 0378-3839 ] ; 2007.

RBID : Pascal:07-0057712

Descripteurs français

Pascal (Inist)
- Onde, Passe intertidale, Plage, Exposition, Morphologie, Croissance, Bras mer, Barre sableuse, Flèche littorale, Migration, Crue, Navigation, Dragage, Programme, Photographie aérienne, Modèle, Sable, Chenal, Circulation, Transport, Courant littoral, Energie, Erosion, Australie.

English descriptors

KwdEn :
- Australia, aerial photography, beaches, channels, circulation, dredging, energy, erosion, exhibits, floods, growth, inlets, longshore currents, migration, models, morphology, navigation, programs, sand, sand bars, spits, tidal inlets, transport, waves.

Abstract

Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A11	`02`	`1`		`@1 BOURGET (Julien)`
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C01	`01`		`ENG`	@0 Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.
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C03	`02`	`2`	`SPA`	`@0 Estrecho mareal @5 02`
C03	`03`	`2`	`FRE`	`@0 Plage @5 03`
C03	`03`	`2`	`ENG`	`@0 beaches @5 03`
C03	`03`	`2`	`SPA`	`@0 Playa @5 03`
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C03	`08`	`2`	`FRE`	`@0 Barre sableuse @5 08`
C03	`08`	`2`	`ENG`	`@0 sand bars @5 08`
C03	`09`	`2`	`FRE`	`@0 Flèche littorale @5 09`
C03	`09`	`2`	`ENG`	`@0 spits @5 09`
C03	`09`	`2`	`SPA`	`@0 Espiga litoral @5 09`
C03	`10`	`2`	`FRE`	`@0 Migration @5 10`
C03	`10`	`2`	`ENG`	`@0 migration @5 10`
C03	`10`	`2`	`SPA`	`@0 Migración @5 10`
C03	`11`	`2`	`FRE`	`@0 Crue @5 11`
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C03	`20`	`2`	`SPA`	`@0 Transporte @5 20`
C03	`21`	`2`	`FRE`	`@0 Courant littoral @5 21`
C03	`21`	`2`	`ENG`	`@0 longshore currents @5 21`
C03	`21`	`2`	`SPA`	`@0 Corriente litoral @5 21`
C03	`22`	`2`	`FRE`	`@0 Energie @5 22`
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Format Inist (serveur)

NO :	PASCAL 07-0057712 INIST
ET :	Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia
AU :	CASTELLE (Bruno); BOURGET (Julien); MOLNAR (Nathalie); STRAUSS (Darrell); DESCHAMPS (Sophie); TOMLINSON (Rodger)
AF :	Griffith Centre for Coastal Management, Gold Coast Campus. Griffith University, PMB 50 Gold Coast Mail Centre/Queensland 9726/Australie (1 aut., 3 aut., 4 aut., 5 aut., 6 aut.); UMR EPOC 4805, Avenue des Facultes/33405 Talence/France (2 aut.)
DT :	Publication en série; Niveau analytique
SO :	Coastal engineering; ISSN 0378-3839; Coden COENDE; Pays-Bas; Da. 2007; Vol. 54; No. 1; Pp. 77-90; Bibl. 49 ref.
LA :	Anglais
EA :	Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.
CC :	226C02; 226C01; 001E01P02; 001E01P01
FD :	Onde; Passe intertidale; Plage; Exposition; Morphologie; Croissance; Bras mer; Barre sableuse; Flèche littorale; Migration; Crue; Navigation; Dragage; Programme; Photographie aérienne; Modèle; Sable; Chenal; Circulation; Transport; Courant littoral; Energie; Erosion; Australie
FG :	Australasie
ED :	waves; tidal inlets; beaches; exhibits; morphology; growth; inlets; sand bars; spits; migration; floods; navigation; dredging; programs; aerial photography; models; sand; channels; circulation; transport; longshore currents; energy; erosion; Australia
EG :	Australasia
SD :	Estrecho mareal; Playa; Morfología; Brazo mar; Espiga litoral; Migración; Crecida; Dragado; Programa; Fotografía aérea; Modelo; Arena; Canal; Transporte; Corriente litoral; Energía; Erosión; Australia
LO :	INIST-17559.354000159626820060
ID :	07-0057712

Links to Exploration step

Pascal:07-0057712

Le document en format XML

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<term>dredging</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Onde</term>
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<term>Photographie aérienne</term>
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<front><div type="abstract" xml:lang="en">Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.</div>
</front>
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<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0378-3839</s0>
</fA01>
<fA02 i1="01"><s0>COENDE</s0>
</fA02>
<fA03 i2="1"><s0>Coastal eng.</s0>
</fA03>
<fA05><s2>54</s2>
</fA05>
<fA06><s2>1</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>CASTELLE (Bruno)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>BOURGET (Julien)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>MOLNAR (Nathalie)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>STRAUSS (Darrell)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>DESCHAMPS (Sophie)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>TOMLINSON (Rodger)</s1>
</fA11>
<fA14 i1="01"><s1>Griffith Centre for Coastal Management, Gold Coast Campus. Griffith University, PMB 50 Gold Coast Mail Centre</s1>
<s2>Queensland 9726</s2>
<s3>AUS</s3>
<sZ>1 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>UMR EPOC 4805, Avenue des Facultes</s1>
<s2>33405 Talence</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA20><s1>77-90</s1>
</fA20>
<fA21><s1>2007</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>17559</s2>
<s5>354000159626820060</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2007 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>49 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>07-0057712</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Coastal engineering</s0>
</fA64>
<fA66 i1="01"><s0>NLD</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>226C02</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>226C01</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>001E01P02</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>001E01P01</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Onde</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>waves</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Passe intertidale</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>tidal inlets</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Estrecho mareal</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Plage</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>beaches</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Playa</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Exposition</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>exhibits</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Morphologie</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>morphology</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Morfología</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Croissance</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>growth</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Bras mer</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>inlets</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Brazo mar</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Barre sableuse</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>sand bars</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Flèche littorale</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>spits</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Espiga litoral</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Migration</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>migration</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Migración</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Crue</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>floods</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Crecida</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Navigation</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>navigation</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Dragage</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>dredging</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Dragado</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Programme</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>programs</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Programa</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Photographie aérienne</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>aerial photography</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Fotografía aérea</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Modèle</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>models</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Modelo</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Sable</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>sand</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Arena</s0>
<s5>17</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Chenal</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>channels</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Canal</s0>
<s5>18</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Circulation</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>circulation</s0>
<s5>19</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Transport</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>transport</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Transporte</s0>
<s5>20</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Courant littoral</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>longshore currents</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Corriente litoral</s0>
<s5>21</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Energie</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>energy</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Energía</s0>
<s5>22</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Erosion</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>erosion</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Erosión</s0>
<s5>23</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="24" i2="2" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="24" i2="2" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fN21><s1>036</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
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<fN82><s1>OTO</s1>
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<server><NO>PASCAL 07-0057712 INIST</NO>
<ET>Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia</ET>
<AU>CASTELLE (Bruno); BOURGET (Julien); MOLNAR (Nathalie); STRAUSS (Darrell); DESCHAMPS (Sophie); TOMLINSON (Rodger)</AU>
<AF>Griffith Centre for Coastal Management, Gold Coast Campus. Griffith University, PMB 50 Gold Coast Mail Centre/Queensland 9726/Australie (1 aut., 3 aut., 4 aut., 5 aut., 6 aut.); UMR EPOC 4805, Avenue des Facultes/33405 Talence/France (2 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Coastal engineering; ISSN 0378-3839; Coden COENDE; Pays-Bas; Da. 2007; Vol. 54; No. 1; Pp. 77-90; Bibl. 49 ref.</SO>
<LA>Anglais</LA>
<EA>Currumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.</EA>
<CC>226C02; 226C01; 001E01P02; 001E01P01</CC>
<FD>Onde; Passe intertidale; Plage; Exposition; Morphologie; Croissance; Bras mer; Barre sableuse; Flèche littorale; Migration; Crue; Navigation; Dragage; Programme; Photographie aérienne; Modèle; Sable; Chenal; Circulation; Transport; Courant littoral; Energie; Erosion; Australie</FD>
<FG>Australasie</FG>
<ED>waves; tidal inlets; beaches; exhibits; morphology; growth; inlets; sand bars; spits; migration; floods; navigation; dredging; programs; aerial photography; models; sand; channels; circulation; transport; longshore currents; energy; erosion; Australia</ED>
<EG>Australasia</EG>
<SD>Estrecho mareal; Playa; Morfología; Brazo mar; Espiga litoral; Migración; Crecida; Dragado; Programa; Fotografía aérea; Modelo; Arena; Canal; Transporte; Corriente litoral; Energía; Erosión; Australia</SD>
<LO>INIST-17559.354000159626820060</LO>
<ID>07-0057712</ID>
</server>
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Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia

Dynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australia

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