Beach-fill equilibration and dune growth at two large-scale nourishment sites
Natural dune growth after nourishment is often observed, and such growth plays an important role in beach management for coastal communities. Nourishment sand equilibration after construction is another important topic for project planning and design. Large-scale nourishment projects at Nags Head (N...
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| Veröffentlicht in: | Ocean dynamics 2018-09, Vol.68 (9), p.1191-1206 |
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| creator | Kaczkowski, Haiqing Liu Kana, Timothy W. Traynum, Steven B. Visser, Ruben |
| description | Natural dune growth after nourishment is often observed, and such growth plays an important role in beach management for coastal communities. Nourishment sand equilibration after construction is another important topic for project planning and design. Large-scale nourishment projects at Nags Head (NC, USA) (completed in 2011) and Bridgehampton–Sagaponack (NY, USA) (completed in 2014) are under comparatively high-wave energy conditions and offer new insight regarding these topics. After nourishment, a natural beach and inshore morphology were produced with high rates of dune growth by eolian transport. At Nags Head, volumetric dune growth averaged 8 m
3
/m/yr over the first 5 years following project completion, while Bridgehampton–Sagaponack averaged 9 m
3
/m/yr over the first 3 post-project years. Results are compared with the Bagnold (
1941
) analytical model predictions of dune growth and are shown to correlate and decay closely with dry-sand beach width as the nourished profile equilibrates. The extra volume and elevation in the dunes have provided a higher level of storm protection and have helped the sites avoid any major damage to oceanfront properties during hurricanes or numerous severe winter storms. |
| doi_str_mv | 10.1007/s10236-018-1176-2 |
| format | Article |
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3
/m/yr over the first 5 years following project completion, while Bridgehampton–Sagaponack averaged 9 m
3
/m/yr over the first 3 post-project years. Results are compared with the Bagnold (
1941
) analytical model predictions of dune growth and are shown to correlate and decay closely with dry-sand beach width as the nourished profile equilibrates. The extra volume and elevation in the dunes have provided a higher level of storm protection and have helped the sites avoid any major damage to oceanfront properties during hurricanes or numerous severe winter storms.</description><identifier>ISSN: 1616-7341</identifier><identifier>EISSN: 1616-7228</identifier><identifier>DOI: 10.1007/s10236-018-1176-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>12-16 June 2017 ; Atmospheric Sciences ; Balancing ; Beach nourishment ; Beaches ; Coastal management ; Coastal zone management ; Coasts ; Construction ; Denmark ; Dunes ; Earth and Environmental Science ; Earth Sciences ; Eolian transport ; Fluid- and Aerodynamics ; Geophysics/Geodesy ; Grain size ; Growth ; Helsingør ; Hurricanes ; Mathematical models ; Monitoring/Environmental Analysis ; Morphology ; Oceanography ; Project planning ; Property damage ; Sand ; Sediments ; Shoreline protection ; Soil erosion ; Storm damage ; Storms ; Topical Collection on the 8th International conference on Coastal Dynamics ; Wave energy ; Wave power ; Winter storms</subject><ispartof>Ocean dynamics, 2018-09, Vol.68 (9), p.1191-1206</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2018</rights><rights>Ocean Dynamics is a copyright of Springer, (2018). All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c316t-7ecc11d40031891dbfd2249768bd146736400c7c0e0e3ff5a9dba824db0ae94e3</citedby><cites>FETCH-LOGICAL-c316t-7ecc11d40031891dbfd2249768bd146736400c7c0e0e3ff5a9dba824db0ae94e3</cites><orcidid>0000-0002-9106-0118</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10236-018-1176-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10236-018-1176-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Kaczkowski, Haiqing Liu</creatorcontrib><creatorcontrib>Kana, Timothy W.</creatorcontrib><creatorcontrib>Traynum, Steven B.</creatorcontrib><creatorcontrib>Visser, Ruben</creatorcontrib><title>Beach-fill equilibration and dune growth at two large-scale nourishment sites</title><title>Ocean dynamics</title><addtitle>Ocean Dynamics</addtitle><description>Natural dune growth after nourishment is often observed, and such growth plays an important role in beach management for coastal communities. Nourishment sand equilibration after construction is another important topic for project planning and design. Large-scale nourishment projects at Nags Head (NC, USA) (completed in 2011) and Bridgehampton–Sagaponack (NY, USA) (completed in 2014) are under comparatively high-wave energy conditions and offer new insight regarding these topics. After nourishment, a natural beach and inshore morphology were produced with high rates of dune growth by eolian transport. At Nags Head, volumetric dune growth averaged 8 m
3
/m/yr over the first 5 years following project completion, while Bridgehampton–Sagaponack averaged 9 m
3
/m/yr over the first 3 post-project years. Results are compared with the Bagnold (
1941
) analytical model predictions of dune growth and are shown to correlate and decay closely with dry-sand beach width as the nourished profile equilibrates. The extra volume and elevation in the dunes have provided a higher level of storm protection and have helped the sites avoid any major damage to oceanfront properties during hurricanes or numerous severe winter storms.</description><subject>12-16 June 2017</subject><subject>Atmospheric Sciences</subject><subject>Balancing</subject><subject>Beach nourishment</subject><subject>Beaches</subject><subject>Coastal management</subject><subject>Coastal zone management</subject><subject>Coasts</subject><subject>Construction</subject><subject>Denmark</subject><subject>Dunes</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Eolian transport</subject><subject>Fluid- and Aerodynamics</subject><subject>Geophysics/Geodesy</subject><subject>Grain size</subject><subject>Growth</subject><subject>Helsingør</subject><subject>Hurricanes</subject><subject>Mathematical models</subject><subject>Monitoring/Environmental Analysis</subject><subject>Morphology</subject><subject>Oceanography</subject><subject>Project planning</subject><subject>Property damage</subject><subject>Sand</subject><subject>Sediments</subject><subject>Shoreline protection</subject><subject>Soil erosion</subject><subject>Storm damage</subject><subject>Storms</subject><subject>Topical Collection on the 8th International conference on Coastal Dynamics</subject><subject>Wave energy</subject><subject>Wave power</subject><subject>Winter storms</subject><issn>1616-7341</issn><issn>1616-7228</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp1kE9LxDAQxYMouK5-AG8Bz9FMUpP2qIv_YMWLnkOaTHe7dNvdJGXx2xup4knmMAPz3pvhR8gl8GvgXN9E4EIqxqFkAFoxcURmoEAxLUR5_DvLAk7JWYwbzrOoEDPyeo_WrVnTdh3F_dh2bR1saoee2t5TP_ZIV2E4pDW1iabDQDsbVsiisx3SfhhDG9db7BONbcJ4Tk4a20W8-Olz8vH48L54Zsu3p5fF3ZI5CSoxjc4B-IJzCWUFvm68EEWlVVl7KJSWKq-cdhw5yqa5tZWvbSkKX3OLVYFyTq6m3F0Y9iPGZDb5lT6fNIIrwQupc80JTCoXhhgDNmYX2q0Nnwa4-aZmJmomUzPf1IzIHjF5Ytb2Kwx_yf-bvgBqeW9l</recordid><startdate>20180901</startdate><enddate>20180901</enddate><creator>Kaczkowski, Haiqing Liu</creator><creator>Kana, Timothy W.</creator><creator>Traynum, Steven B.</creator><creator>Visser, Ruben</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><orcidid>https://orcid.org/0000-0002-9106-0118</orcidid></search><sort><creationdate>20180901</creationdate><title>Beach-fill equilibration and dune growth at two large-scale nourishment sites</title><author>Kaczkowski, Haiqing Liu ; Kana, Timothy W. ; Traynum, Steven B. ; Visser, Ruben</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c316t-7ecc11d40031891dbfd2249768bd146736400c7c0e0e3ff5a9dba824db0ae94e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>12-16 June 2017</topic><topic>Atmospheric Sciences</topic><topic>Balancing</topic><topic>Beach nourishment</topic><topic>Beaches</topic><topic>Coastal management</topic><topic>Coastal zone management</topic><topic>Coasts</topic><topic>Construction</topic><topic>Denmark</topic><topic>Dunes</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Eolian transport</topic><topic>Fluid- and Aerodynamics</topic><topic>Geophysics/Geodesy</topic><topic>Grain size</topic><topic>Growth</topic><topic>Helsingør</topic><topic>Hurricanes</topic><topic>Mathematical models</topic><topic>Monitoring/Environmental Analysis</topic><topic>Morphology</topic><topic>Oceanography</topic><topic>Project planning</topic><topic>Property damage</topic><topic>Sand</topic><topic>Sediments</topic><topic>Shoreline protection</topic><topic>Soil erosion</topic><topic>Storm damage</topic><topic>Storms</topic><topic>Topical Collection on the 8th International conference on Coastal Dynamics</topic><topic>Wave energy</topic><topic>Wave power</topic><topic>Winter storms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kaczkowski, Haiqing Liu</creatorcontrib><creatorcontrib>Kana, Timothy W.</creatorcontrib><creatorcontrib>Traynum, Steven B.</creatorcontrib><creatorcontrib>Visser, Ruben</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Ocean dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kaczkowski, Haiqing Liu</au><au>Kana, Timothy W.</au><au>Traynum, Steven B.</au><au>Visser, Ruben</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Beach-fill equilibration and dune growth at two large-scale nourishment sites</atitle><jtitle>Ocean dynamics</jtitle><stitle>Ocean Dynamics</stitle><date>2018-09-01</date><risdate>2018</risdate><volume>68</volume><issue>9</issue><spage>1191</spage><epage>1206</epage><pages>1191-1206</pages><issn>1616-7341</issn><eissn>1616-7228</eissn><abstract>Natural dune growth after nourishment is often observed, and such growth plays an important role in beach management for coastal communities. Nourishment sand equilibration after construction is another important topic for project planning and design. Large-scale nourishment projects at Nags Head (NC, USA) (completed in 2011) and Bridgehampton–Sagaponack (NY, USA) (completed in 2014) are under comparatively high-wave energy conditions and offer new insight regarding these topics. After nourishment, a natural beach and inshore morphology were produced with high rates of dune growth by eolian transport. At Nags Head, volumetric dune growth averaged 8 m
3
/m/yr over the first 5 years following project completion, while Bridgehampton–Sagaponack averaged 9 m
3
/m/yr over the first 3 post-project years. Results are compared with the Bagnold (
1941
) analytical model predictions of dune growth and are shown to correlate and decay closely with dry-sand beach width as the nourished profile equilibrates. The extra volume and elevation in the dunes have provided a higher level of storm protection and have helped the sites avoid any major damage to oceanfront properties during hurricanes or numerous severe winter storms.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10236-018-1176-2</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-9106-0118</orcidid></addata></record> |
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| subjects | 12-16 June 2017 Atmospheric Sciences Balancing Beach nourishment Beaches Coastal management Coastal zone management Coasts Construction Denmark Dunes Earth and Environmental Science Earth Sciences Eolian transport Fluid- and Aerodynamics Geophysics/Geodesy Grain size Growth Helsingør Hurricanes Mathematical models Monitoring/Environmental Analysis Morphology Oceanography Project planning Property damage Sand Sediments Shoreline protection Soil erosion Storm damage Storms Topical Collection on the 8th International conference on Coastal Dynamics Wave energy Wave power Winter storms |
| title | Beach-fill equilibration and dune growth at two large-scale nourishment sites |
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