Recent shifts in coastline change and shoreline stabilization linked to storm climate change
Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization e...
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| Autor*in: |
Johnson, Jennifer M [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Earth surface processes and landforms - New York, NY [u.a.] : Wiley, 1981, 40(2015), 5, Seite 569-585 |
|---|---|
| Übergeordnetes Werk: |
volume:40 ; year:2015 ; number:5 ; pages:569-585 |
| Links: |
|---|
| DOI / URN: |
10.1002/esp.3650 |
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| 520 | |a Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. | ||
| 540 | |a Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. | ||
| 650 | 4 | |a shoreline change | |
| 650 | 4 | |a human impacts on coastlines | |
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| 700 | 1 | |a Moore, Laura J |4 oth | |
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| 700 | 1 | |a Jaeger, John M |4 oth | |
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10.1002/esp.3650 doi PQ20160617 (DE-627)OLC196250610X (DE-599)GBVOLC196250610X (PRQ)p2070-4cbae4f3ae87092bdd3e6bcf0c5159b53c44b191f86ab0415b5825dfd7f5f4843 (KEY)0004410520150000040000500569recentshiftsincoastlinechangeandshorelinestabiliza DE-627 ger DE-627 rakwb eng 910 DNB Johnson, Jennifer M verfasserin aut Recent shifts in coastline change and shoreline stabilization linked to storm climate change 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. shoreline change human impacts on coastlines coastline shape cuspate coastlines wave climate Moore, Laura J oth Ells, Kenneth oth Murray, A. Brad oth Adams, Peter N oth MacKenzie, Richard A oth Jaeger, John M oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 40(2015), 5, Seite 569-585 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:40 year:2015 number:5 pages:569-585 http://dx.doi.org/10.1002/esp.3650 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.3650/abstract http://search.proquest.com/docview/1672760935 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 40 2015 5 569-585 |
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10.1002/esp.3650 doi PQ20160617 (DE-627)OLC196250610X (DE-599)GBVOLC196250610X (PRQ)p2070-4cbae4f3ae87092bdd3e6bcf0c5159b53c44b191f86ab0415b5825dfd7f5f4843 (KEY)0004410520150000040000500569recentshiftsincoastlinechangeandshorelinestabiliza DE-627 ger DE-627 rakwb eng 910 DNB Johnson, Jennifer M verfasserin aut Recent shifts in coastline change and shoreline stabilization linked to storm climate change 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. shoreline change human impacts on coastlines coastline shape cuspate coastlines wave climate Moore, Laura J oth Ells, Kenneth oth Murray, A. Brad oth Adams, Peter N oth MacKenzie, Richard A oth Jaeger, John M oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 40(2015), 5, Seite 569-585 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:40 year:2015 number:5 pages:569-585 http://dx.doi.org/10.1002/esp.3650 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.3650/abstract http://search.proquest.com/docview/1672760935 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 40 2015 5 569-585 |
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10.1002/esp.3650 doi PQ20160617 (DE-627)OLC196250610X (DE-599)GBVOLC196250610X (PRQ)p2070-4cbae4f3ae87092bdd3e6bcf0c5159b53c44b191f86ab0415b5825dfd7f5f4843 (KEY)0004410520150000040000500569recentshiftsincoastlinechangeandshorelinestabiliza DE-627 ger DE-627 rakwb eng 910 DNB Johnson, Jennifer M verfasserin aut Recent shifts in coastline change and shoreline stabilization linked to storm climate change 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. shoreline change human impacts on coastlines coastline shape cuspate coastlines wave climate Moore, Laura J oth Ells, Kenneth oth Murray, A. Brad oth Adams, Peter N oth MacKenzie, Richard A oth Jaeger, John M oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 40(2015), 5, Seite 569-585 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:40 year:2015 number:5 pages:569-585 http://dx.doi.org/10.1002/esp.3650 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.3650/abstract http://search.proquest.com/docview/1672760935 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 40 2015 5 569-585 |
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10.1002/esp.3650 doi PQ20160617 (DE-627)OLC196250610X (DE-599)GBVOLC196250610X (PRQ)p2070-4cbae4f3ae87092bdd3e6bcf0c5159b53c44b191f86ab0415b5825dfd7f5f4843 (KEY)0004410520150000040000500569recentshiftsincoastlinechangeandshorelinestabiliza DE-627 ger DE-627 rakwb eng 910 DNB Johnson, Jennifer M verfasserin aut Recent shifts in coastline change and shoreline stabilization linked to storm climate change 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. shoreline change human impacts on coastlines coastline shape cuspate coastlines wave climate Moore, Laura J oth Ells, Kenneth oth Murray, A. Brad oth Adams, Peter N oth MacKenzie, Richard A oth Jaeger, John M oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 40(2015), 5, Seite 569-585 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:40 year:2015 number:5 pages:569-585 http://dx.doi.org/10.1002/esp.3650 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.3650/abstract http://search.proquest.com/docview/1672760935 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 40 2015 5 569-585 |
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recent shifts in coastline change and shoreline stabilization linked to storm climate change |
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Recent shifts in coastline change and shoreline stabilization linked to storm climate change |
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Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. |
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Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. |
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Since cuspate coastlines are especially sensitive to changes in wave climate, they serve as potential indicators of initial responses to changing wave conditions. Previous work demonstrates that Cape Hatteras and Cape Lookout, North Carolina, which are largely unaffected by shoreline stabilization efforts, have become increasingly asymmetric over the past 30 years, consistent with model predictions for coastline response to increases in Atlantic Ocean summer wave heights and resulting changes in the distribution of wave‐approach angles. Historic and recent shoreline change observations for Cape Fear, North Carolina, and model simulations of coastline response to an increasingly asymmetric wave climate in the presence of beach nourishment, produce comparable differences in shoreline change rates in response to changes in wave climate. Results suggest that the effect of beach nourishment is to compensate for – and therefore to mask – natural responses to wave climate change that might otherwise be discernible in patterns of shoreline change alone. Therefore, this case study suggests that the effects of wave climate change on human‐modified coastlines may be detectable in the spatial and temporal patterns of shoreline stabilization activities. Similar analyses of cuspate features in areas where the change in wave climate is less pronounced (i.e. Fishing Point, Maryland/Virginia) and where local geology appears to exert control on coastline shape (i.e. Cape Canaveral, Florida), suggest that changes in shoreline configuration that may be arising from shifting wave climate are currently limited to sandy wave‐dominated coastlines where the change in wave climate has been most pronounced. However, if hurricane‐generated wave heights continue to increase, large‐scale shifts in patterns of erosion and accretion will likely extend beyond sensitive cuspate features as the larger‐scale coastline shape comes into equilibrium with changing wave conditions. Copyright © 2014 John Wiley & Sons, Ltd. |
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