A new constraint on the size of Heinrich Events from an iceberg/sediment model
Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Roberts, William H.G. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Schlagwörter: |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption - Kılıç Depren, Serpil ELSEVIER, 2022, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:386 ; year:2014 ; day:15 ; month:01 ; pages:1-9 ; extent:9 |
| Links: |
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| DOI / URN: |
10.1016/j.epsl.2013.10.020 |
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| 520 | |a Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. | ||
| 520 | |a Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. | ||
| 650 | 7 | |a Heinrich layers |2 Elsevier | |
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10.1016/j.epsl.2013.10.020 doi GBVA2014020000021.pica (DE-627)ELV023049138 (ELSEVIER)S0012-821X(13)00583-9 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 333.7 VZ BIODIV DE-30 fid 42.90 bkl 42.11 bkl Roberts, William H.G. verfasserin aut A new constraint on the size of Heinrich Events from an iceberg/sediment model 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich layers Elsevier Heinrich events Elsevier iceberg modelling Elsevier Valdes, Paul J. oth Payne, Antony J. oth Enthalten in Elsevier Kılıç Depren, Serpil ELSEVIER Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption 2022 Amsterdam [u.a.] (DE-627)ELV008390509 volume:386 year:2014 day:15 month:01 pages:1-9 extent:9 https://doi.org/10.1016/j.epsl.2013.10.020 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 42.90 Ökologie: Allgemeines VZ 42.11 Biomathematik Biokybernetik VZ AR 386 2014 15 0115 1-9 9 045F 550 |
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10.1016/j.epsl.2013.10.020 doi GBVA2014020000021.pica (DE-627)ELV023049138 (ELSEVIER)S0012-821X(13)00583-9 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 333.7 VZ BIODIV DE-30 fid 42.90 bkl 42.11 bkl Roberts, William H.G. verfasserin aut A new constraint on the size of Heinrich Events from an iceberg/sediment model 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich layers Elsevier Heinrich events Elsevier iceberg modelling Elsevier Valdes, Paul J. oth Payne, Antony J. oth Enthalten in Elsevier Kılıç Depren, Serpil ELSEVIER Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption 2022 Amsterdam [u.a.] (DE-627)ELV008390509 volume:386 year:2014 day:15 month:01 pages:1-9 extent:9 https://doi.org/10.1016/j.epsl.2013.10.020 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 42.90 Ökologie: Allgemeines VZ 42.11 Biomathematik Biokybernetik VZ AR 386 2014 15 0115 1-9 9 045F 550 |
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10.1016/j.epsl.2013.10.020 doi GBVA2014020000021.pica (DE-627)ELV023049138 (ELSEVIER)S0012-821X(13)00583-9 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 333.7 VZ BIODIV DE-30 fid 42.90 bkl 42.11 bkl Roberts, William H.G. verfasserin aut A new constraint on the size of Heinrich Events from an iceberg/sediment model 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich layers Elsevier Heinrich events Elsevier iceberg modelling Elsevier Valdes, Paul J. oth Payne, Antony J. oth Enthalten in Elsevier Kılıç Depren, Serpil ELSEVIER Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption 2022 Amsterdam [u.a.] (DE-627)ELV008390509 volume:386 year:2014 day:15 month:01 pages:1-9 extent:9 https://doi.org/10.1016/j.epsl.2013.10.020 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 42.90 Ökologie: Allgemeines VZ 42.11 Biomathematik Biokybernetik VZ AR 386 2014 15 0115 1-9 9 045F 550 |
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10.1016/j.epsl.2013.10.020 doi GBVA2014020000021.pica (DE-627)ELV023049138 (ELSEVIER)S0012-821X(13)00583-9 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 333.7 VZ BIODIV DE-30 fid 42.90 bkl 42.11 bkl Roberts, William H.G. verfasserin aut A new constraint on the size of Heinrich Events from an iceberg/sediment model 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich layers Elsevier Heinrich events Elsevier iceberg modelling Elsevier Valdes, Paul J. oth Payne, Antony J. oth Enthalten in Elsevier Kılıç Depren, Serpil ELSEVIER Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption 2022 Amsterdam [u.a.] (DE-627)ELV008390509 volume:386 year:2014 day:15 month:01 pages:1-9 extent:9 https://doi.org/10.1016/j.epsl.2013.10.020 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 42.90 Ökologie: Allgemeines VZ 42.11 Biomathematik Biokybernetik VZ AR 386 2014 15 0115 1-9 9 045F 550 |
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10.1016/j.epsl.2013.10.020 doi GBVA2014020000021.pica (DE-627)ELV023049138 (ELSEVIER)S0012-821X(13)00583-9 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 333.7 VZ BIODIV DE-30 fid 42.90 bkl 42.11 bkl Roberts, William H.G. verfasserin aut A new constraint on the size of Heinrich Events from an iceberg/sediment model 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. Heinrich layers Elsevier Heinrich events Elsevier iceberg modelling Elsevier Valdes, Paul J. oth Payne, Antony J. oth Enthalten in Elsevier Kılıç Depren, Serpil ELSEVIER Energy consumption and environmental degradation nexus: A systematic review and meta-analysis of fossil fuel and renewable energy consumption 2022 Amsterdam [u.a.] (DE-627)ELV008390509 volume:386 year:2014 day:15 month:01 pages:1-9 extent:9 https://doi.org/10.1016/j.epsl.2013.10.020 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA 42.90 Ökologie: Allgemeines VZ 42.11 Biomathematik Biokybernetik VZ AR 386 2014 15 0115 1-9 9 045F 550 |
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a new constraint on the size of heinrich events from an iceberg/sediment model |
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A new constraint on the size of Heinrich Events from an iceberg/sediment model |
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Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. |
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Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. |
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Heinrich Layers, anomalously thick layers of ice-borne sediment in the North Atlantic ocean, have long been associated with abrupt climate changes in glacial times. However, there is still no consensus on either the exact amount of ice needed to transport this sediment or how such a large volume of ice could be produced. Using an iceberg model that includes sediment, we simulate the delivery of sediment to the North Atlantic during such an event. Our model assumes that sediment is uniformly distributed within the ice with a concentration of 4%. Unlike sediment models which assume that the sediment lies in a single layer, this model can carry sediment all the way from the western to the eastern North Atlantic. We use a variety of different estimates for the total volume of ice released to model the sediment layer thickness and we show that to best fit the observations 60 × 10 4 km 3 (with a plausible range of 30 – 120 × 10 4 km 3 ) of ice needs to be released. This is equivalent to a 0.04 Sv ( 10 6 m 3 s − 1 , with a plausible range of 0.02–0.08 Sv) release of freshwater over the 500 yr of a typical Heinrich Event. This is a smaller flux of water than is required to show a significant impact on the global climate in most current “state of the art” GCMs. |
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