Impact of Sea-level Rise and Storm Surges on a Coastal Community
Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-th...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Mcinnes, K. L. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2003 |
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| Schlagwörter: |
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| Anmerkung: |
© Kluwer Academic Publishers 2003 |
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| Übergeordnetes Werk: |
Enthalten in: Natural hazards - Kluwer Academic Publishers, 1988, 30(2003), 2 vom: Okt., Seite 187-207 |
|---|---|
| Übergeordnetes Werk: |
volume:30 ; year:2003 ; number:2 ; month:10 ; pages:187-207 |
| Links: |
|---|
| DOI / URN: |
10.1023/A:1026118417752 |
|---|
| Katalog-ID: |
OLC2053640944 |
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| 520 | |a Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. | ||
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10.1023/A:1026118417752 doi (DE-627)OLC2053640944 (DE-He213)A:1026118417752-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mcinnes, K. L. verfasserin aut Impact of Sea-level Rise and Storm Surges on a Coastal Community 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2003 Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. Cyclone Return Period Storm Tide Greenhouse Climate Enhance Greenhouse Effect Walsh, K. J. E. aut Hubbert, G. D. aut Beer, T. aut Enthalten in Natural hazards Kluwer Academic Publishers, 1988 30(2003), 2 vom: Okt., Seite 187-207 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:30 year:2003 number:2 month:10 pages:187-207 https://doi.org/10.1023/A:1026118417752 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 AR 30 2003 2 10 187-207 |
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10.1023/A:1026118417752 doi (DE-627)OLC2053640944 (DE-He213)A:1026118417752-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mcinnes, K. L. verfasserin aut Impact of Sea-level Rise and Storm Surges on a Coastal Community 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2003 Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. Cyclone Return Period Storm Tide Greenhouse Climate Enhance Greenhouse Effect Walsh, K. J. E. aut Hubbert, G. D. aut Beer, T. aut Enthalten in Natural hazards Kluwer Academic Publishers, 1988 30(2003), 2 vom: Okt., Seite 187-207 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:30 year:2003 number:2 month:10 pages:187-207 https://doi.org/10.1023/A:1026118417752 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 AR 30 2003 2 10 187-207 |
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10.1023/A:1026118417752 doi (DE-627)OLC2053640944 (DE-He213)A:1026118417752-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mcinnes, K. L. verfasserin aut Impact of Sea-level Rise and Storm Surges on a Coastal Community 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2003 Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. Cyclone Return Period Storm Tide Greenhouse Climate Enhance Greenhouse Effect Walsh, K. J. E. aut Hubbert, G. D. aut Beer, T. aut Enthalten in Natural hazards Kluwer Academic Publishers, 1988 30(2003), 2 vom: Okt., Seite 187-207 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:30 year:2003 number:2 month:10 pages:187-207 https://doi.org/10.1023/A:1026118417752 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 AR 30 2003 2 10 187-207 |
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10.1023/A:1026118417752 doi (DE-627)OLC2053640944 (DE-He213)A:1026118417752-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mcinnes, K. L. verfasserin aut Impact of Sea-level Rise and Storm Surges on a Coastal Community 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2003 Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. Cyclone Return Period Storm Tide Greenhouse Climate Enhance Greenhouse Effect Walsh, K. J. E. aut Hubbert, G. D. aut Beer, T. aut Enthalten in Natural hazards Kluwer Academic Publishers, 1988 30(2003), 2 vom: Okt., Seite 187-207 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:30 year:2003 number:2 month:10 pages:187-207 https://doi.org/10.1023/A:1026118417752 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 AR 30 2003 2 10 187-207 |
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10.1023/A:1026118417752 doi (DE-627)OLC2053640944 (DE-He213)A:1026118417752-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Mcinnes, K. L. verfasserin aut Impact of Sea-level Rise and Storm Surges on a Coastal Community 2003 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 2003 Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. Cyclone Return Period Storm Tide Greenhouse Climate Enhance Greenhouse Effect Walsh, K. J. E. aut Hubbert, G. D. aut Beer, T. aut Enthalten in Natural hazards Kluwer Academic Publishers, 1988 30(2003), 2 vom: Okt., Seite 187-207 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:30 year:2003 number:2 month:10 pages:187-207 https://doi.org/10.1023/A:1026118417752 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT GBV_ILN_24 GBV_ILN_40 GBV_ILN_70 AR 30 2003 2 10 187-207 |
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10.1023/A:1026118417752 |
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550 |
| title_sort |
impact of sea-level rise and storm surges on a coastal community |
| title_auth |
Impact of Sea-level Rise and Storm Surges on a Coastal Community |
| abstract |
Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. © Kluwer Academic Publishers 2003 |
| abstractGer |
Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. © Kluwer Academic Publishers 2003 |
| abstract_unstemmed |
Abstract A technique to evaluate the risk of storm tides (the combination of a storm surge and tide) under present and enhanced greenhouse conditions has been applied to Cairns on the north-eastern Australian coast. The technique combines a statistical model for cyclone occurrence with a state-of-the-art storm surge inundation model and involves the random generation of a large number of storm tide simulations. The set of simulations constitutes a synthetic record of extreme sea-level events that can be analysed to produce storm tide return periods. The use of a dynamic storm surge model with overland flooding capability means that the spatial extent of flooding is also implicitly modelled. The technique has the advantage that it can readily be modified to include projected changes to cyclone behaviour due to the enhanced greenhouse effect. Sea-level heights in the current climate for return periods of 50, 100, 500 and 1000 years have been determined to be 2.0 m, 2.3 m, 3.0 m and 3.4 m respectively. In an enhanced greenhouse climate (around 2050), projected increases in cyclone intensity and mean sea-level see these heights increase to 2.4 m, 2.8 m, 3.8 m and 4.2 m respectively. The average area inundated by events with a return period greater than 100 years is found to more than double under enhanced greenhouse conditions. © Kluwer Academic Publishers 2003 |
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Impact of Sea-level Rise and Storm Surges on a Coastal Community |
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Walsh, K. J. E. Hubbert, G. D. Beer, T. |
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| up_date |
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