Magnitude-frequency relationship of coastal sand delivery by a southern California stream
Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Stow, Douglas W. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1987 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag New York Inc 1987 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Geo-marine letters - Springer-Verlag, 1981, 7(1987), 4 vom: Dez., Seite 217-222 |
|---|---|
| Übergeordnetes Werk: |
volume:7 ; year:1987 ; number:4 ; month:12 ; pages:217-222 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02242774 |
|---|
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OLC203616627X |
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| 520 | |a Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. | ||
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10.1007/BF02242774 doi (DE-627)OLC203616627X (DE-He213)BF02242774-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Stow, Douglas W. verfasserin aut Magnitude-frequency relationship of coastal sand delivery by a southern California stream 1987 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc 1987 Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. Numerical Model Sediment Transport Sediment Yield Unsteady Flow Annual Sediment Chang, Howard H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 7(1987), 4 vom: Dez., Seite 217-222 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:7 year:1987 number:4 month:12 pages:217-222 https://doi.org/10.1007/BF02242774 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 7 1987 4 12 217-222 |
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10.1007/BF02242774 doi (DE-627)OLC203616627X (DE-He213)BF02242774-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Stow, Douglas W. verfasserin aut Magnitude-frequency relationship of coastal sand delivery by a southern California stream 1987 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc 1987 Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. Numerical Model Sediment Transport Sediment Yield Unsteady Flow Annual Sediment Chang, Howard H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 7(1987), 4 vom: Dez., Seite 217-222 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:7 year:1987 number:4 month:12 pages:217-222 https://doi.org/10.1007/BF02242774 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 7 1987 4 12 217-222 |
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10.1007/BF02242774 doi (DE-627)OLC203616627X (DE-He213)BF02242774-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Stow, Douglas W. verfasserin aut Magnitude-frequency relationship of coastal sand delivery by a southern California stream 1987 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc 1987 Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. Numerical Model Sediment Transport Sediment Yield Unsteady Flow Annual Sediment Chang, Howard H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 7(1987), 4 vom: Dez., Seite 217-222 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:7 year:1987 number:4 month:12 pages:217-222 https://doi.org/10.1007/BF02242774 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 7 1987 4 12 217-222 |
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10.1007/BF02242774 doi (DE-627)OLC203616627X (DE-He213)BF02242774-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Stow, Douglas W. verfasserin aut Magnitude-frequency relationship of coastal sand delivery by a southern California stream 1987 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc 1987 Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. Numerical Model Sediment Transport Sediment Yield Unsteady Flow Annual Sediment Chang, Howard H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 7(1987), 4 vom: Dez., Seite 217-222 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:7 year:1987 number:4 month:12 pages:217-222 https://doi.org/10.1007/BF02242774 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 7 1987 4 12 217-222 |
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10.1007/BF02242774 doi (DE-627)OLC203616627X (DE-He213)BF02242774-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Stow, Douglas W. verfasserin aut Magnitude-frequency relationship of coastal sand delivery by a southern California stream 1987 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag New York Inc 1987 Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. Numerical Model Sediment Transport Sediment Yield Unsteady Flow Annual Sediment Chang, Howard H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 7(1987), 4 vom: Dez., Seite 217-222 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:7 year:1987 number:4 month:12 pages:217-222 https://doi.org/10.1007/BF02242774 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_70 GBV_ILN_267 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4082 AR 7 1987 4 12 217-222 |
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Magnitude-frequency relationship of coastal sand delivery by a southern California stream |
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Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. © Springer-Verlag New York Inc 1987 |
| abstractGer |
Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. © Springer-Verlag New York Inc 1987 |
| abstract_unstemmed |
Abstract Coastal sand delivery by a stream in southern California is estimated based on a numerical model which stimulates unsteady flow, sediment transport, and the associated channel adjustments for a stream-delta system. An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. Of the total sand delivery by the stream, 20.5 percent is contributed from floods greater than the 100-year flood; 17.6 percent from those between the 50- and 100-year events; 28.4 percent from those between the 25- and 50 year floods; and 33.5 percent from those smaller than the 25-year flood. © Springer-Verlag New York Inc 1987 |
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Magnitude-frequency relationship of coastal sand delivery by a southern California stream |
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https://doi.org/10.1007/BF02242774 |
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false |
| author2 |
Chang, Howard H. |
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Chang, Howard H. |
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129932140 |
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| doi_str |
10.1007/BF02242774 |
| up_date |
2024-07-04T02:49:13.663Z |
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1803615053987971072 |
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An average annual sediment yield of 51,400 $ m^{3} $/yr is estimated for the San Dieguito River, which drains a semiarid watershed controlled by dams. 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