The temporal and spatial scales of rocky coast geomorphology: a commentary
Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kennedy, David M [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: Copyright © 2017 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, 42(2017), 10, Seite 1597-1600 |
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| Übergeordnetes Werk: |
volume:42 ; year:2017 ; number:10 ; pages:1597-1600 |
| Links: |
|---|
| DOI / URN: |
10.1002/esp.4150 |
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OLC1995744816 |
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| 520 | |a Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. | ||
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| 650 | 4 | |a Erosion mechanisms | |
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| 650 | 4 | |a Landforms | |
| 650 | 4 | |a Rocky shores | |
| 650 | 4 | |a Climate change | |
| 650 | 4 | |a Climate | |
| 650 | 4 | |a Climatic changes | |
| 650 | 4 | |a Work platforms | |
| 650 | 4 | |a Shores | |
| 650 | 4 | |a Cliffs | |
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| 650 | 4 | |a Geomorphology | |
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| 650 | 4 | |a Rocky environments | |
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10.1002/esp.4150 doi PQ20170901 (DE-627)OLC1995744816 (DE-599)GBVOLC1995744816 (PRQ)p950-2516258af643dd312b81f1271c6791a08cc7cbefa7deb52681d6705aad3bd2c13 (KEY)0004410520170000042001001597temporalandspatialscalesofrockycoastgeomorphologya DE-627 ger DE-627 rakwb eng 910 DNB Kennedy, David M verfasserin aut The temporal and spatial scales of rocky coast geomorphology: a commentary 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. Coastlines Sea level Earth Erosion mechanisms Coastal environments Landforms Rocky shores Climate change Climate Climatic changes Work platforms Shores Cliffs Erosion Geomorphology Earth surface Rocky environments Weathering Research Spatial discrimination Coasts Modelling Coombes, Martin A oth Mottershead, Derek N oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 42(2017), 10, Seite 1597-1600 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:42 year:2017 number:10 pages:1597-1600 http://dx.doi.org/10.1002/esp.4150 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.4150/abstract https://search.proquest.com/docview/1925515281 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 42 2017 10 1597-1600 |
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10.1002/esp.4150 doi PQ20170901 (DE-627)OLC1995744816 (DE-599)GBVOLC1995744816 (PRQ)p950-2516258af643dd312b81f1271c6791a08cc7cbefa7deb52681d6705aad3bd2c13 (KEY)0004410520170000042001001597temporalandspatialscalesofrockycoastgeomorphologya DE-627 ger DE-627 rakwb eng 910 DNB Kennedy, David M verfasserin aut The temporal and spatial scales of rocky coast geomorphology: a commentary 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2017 John Wiley & Sons, Ltd. Coastlines Sea level Earth Erosion mechanisms Coastal environments Landforms Rocky shores Climate change Climate Climatic changes Work platforms Shores Cliffs Erosion Geomorphology Earth surface Rocky environments Weathering Research Spatial discrimination Coasts Modelling Coombes, Martin A oth Mottershead, Derek N oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 42(2017), 10, Seite 1597-1600 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:42 year:2017 number:10 pages:1597-1600 http://dx.doi.org/10.1002/esp.4150 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.4150/abstract https://search.proquest.com/docview/1925515281 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 42 2017 10 1597-1600 |
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Kennedy, David M |
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910 DNB The temporal and spatial scales of rocky coast geomorphology: a commentary Coastlines Sea level Earth Erosion mechanisms Coastal environments Landforms Rocky shores Climate change Climate Climatic changes Work platforms Shores Cliffs Erosion Geomorphology Earth surface Rocky environments Weathering Research Spatial discrimination Coasts Modelling |
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The temporal and spatial scales of rocky coast geomorphology: a commentary |
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temporal and spatial scales of rocky coast geomorphology: a commentary |
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The temporal and spatial scales of rocky coast geomorphology: a commentary |
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Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. |
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Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. |
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Rocky shores are complex landforms that result from marine erosion and subaerial weathering. They are time‐integrated features where their present day form is the result of instantaneous erosion, often on the millimetre to sub‐metre scale, occurring for centuries to millennia. As a result, research on rocky coasts focuses on a range of temporal and spatial scales from granular‐scale swelling of a rock surface and instantaneous wave impact to modelling millennial‐scale sea level drivers. The challenge for rocky coast researchers is either to upscale or to downscale their results to the human‐timescales of greatest interest to managers. The research presented in Earth Surface Processes and Landforms over the past 3 years highlights the range of spatial and temporal approaches to the study of coastal cliffs and shore platforms. We identify a key temporal and spatial gap in current research. Seasonal–annual timeframes over hundreds of metres to kilometre scale studies appear to be lacking and are likely critical in understanding the future evolution of rocky coasts, especially their response to climate change. Copyright © 2017 John Wiley & Sons, Ltd. |
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The temporal and spatial scales of rocky coast geomorphology: a commentary |
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