On predicting the response of forests in eastern North America to future climatic change
Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed clim...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cook, Edward R. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1991 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Kluwer Academic Publishers 1991 |
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| Übergeordnetes Werk: |
Enthalten in: Climatic change - Kluwer Academic Publishers, 1977, 19(1991), 3 vom: Okt., Seite 271-282 |
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| Übergeordnetes Werk: |
volume:19 ; year:1991 ; number:3 ; month:10 ; pages:271-282 |
| Links: |
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| DOI / URN: |
10.1007/BF00140166 |
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| Katalog-ID: |
OLC2062581106 |
|---|
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| 520 | |a Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. | ||
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10.1007/BF00140166 doi (DE-627)OLC2062581106 (DE-He213)BF00140166-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Cook, Edward R. verfasserin aut On predicting the response of forests in eastern North America to future climatic change 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1991 Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. Climatic Change Tree Species Simulation Model North America Individual Tree Cole, Julie aut Enthalten in Climatic change Kluwer Academic Publishers, 1977 19(1991), 3 vom: Okt., Seite 271-282 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:19 year:1991 number:3 month:10 pages:271-282 https://doi.org/10.1007/BF00140166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 19 1991 3 10 271-282 |
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10.1007/BF00140166 doi (DE-627)OLC2062581106 (DE-He213)BF00140166-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Cook, Edward R. verfasserin aut On predicting the response of forests in eastern North America to future climatic change 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1991 Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. Climatic Change Tree Species Simulation Model North America Individual Tree Cole, Julie aut Enthalten in Climatic change Kluwer Academic Publishers, 1977 19(1991), 3 vom: Okt., Seite 271-282 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:19 year:1991 number:3 month:10 pages:271-282 https://doi.org/10.1007/BF00140166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 19 1991 3 10 271-282 |
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10.1007/BF00140166 doi (DE-627)OLC2062581106 (DE-He213)BF00140166-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Cook, Edward R. verfasserin aut On predicting the response of forests in eastern North America to future climatic change 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1991 Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. Climatic Change Tree Species Simulation Model North America Individual Tree Cole, Julie aut Enthalten in Climatic change Kluwer Academic Publishers, 1977 19(1991), 3 vom: Okt., Seite 271-282 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:19 year:1991 number:3 month:10 pages:271-282 https://doi.org/10.1007/BF00140166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 19 1991 3 10 271-282 |
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10.1007/BF00140166 doi (DE-627)OLC2062581106 (DE-He213)BF00140166-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Cook, Edward R. verfasserin aut On predicting the response of forests in eastern North America to future climatic change 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1991 Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. Climatic Change Tree Species Simulation Model North America Individual Tree Cole, Julie aut Enthalten in Climatic change Kluwer Academic Publishers, 1977 19(1991), 3 vom: Okt., Seite 271-282 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:19 year:1991 number:3 month:10 pages:271-282 https://doi.org/10.1007/BF00140166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 19 1991 3 10 271-282 |
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10.1007/BF00140166 doi (DE-627)OLC2062581106 (DE-He213)BF00140166-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Cook, Edward R. verfasserin aut On predicting the response of forests in eastern North America to future climatic change 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1991 Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. Climatic Change Tree Species Simulation Model North America Individual Tree Cole, Julie aut Enthalten in Climatic change Kluwer Academic Publishers, 1977 19(1991), 3 vom: Okt., Seite 271-282 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:19 year:1991 number:3 month:10 pages:271-282 https://doi.org/10.1007/BF00140166 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_40 GBV_ILN_47 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 19 1991 3 10 271-282 |
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Cook, Edward R. |
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Cook, Edward R. ddc 550 ssgn 14 rvk RA 1000 misc Climatic Change misc Tree Species misc Simulation Model misc North America misc Individual Tree On predicting the response of forests in eastern North America to future climatic change |
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On predicting the response of forests in eastern North America to future climatic change |
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On predicting the response of forests in eastern North America to future climatic change |
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on predicting the response of forests in eastern north america to future climatic change |
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On predicting the response of forests in eastern North America to future climatic change |
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Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. © Kluwer Academic Publishers 1991 |
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Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. © Kluwer Academic Publishers 1991 |
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Abstract Our ability to accurately predict the response of forests in eastern North America to future climatic change is limited by our knowledge of how different tree species respond to climate. When the climatic response of eastern hemlock is modeled across its range, we find that the assumed climatic response used in simulation models is not sufficient to explain how this species is presently responding to climate. This is also the case for red spruce growing in the northern Appalachian Mountains. Consequently, simulations of future change to forests that include eastern hemlock and red spruce may need to be improved. We suspect that similar findings will be made when other tree species are studied in detail using tree-ring analysis. If so, our present understanding of how individual tree species respond to climate may not be adequate for accurately predicting future changes to these forests. Tree-ring analysis can increase our understanding of how climate affects tree growth in eastern North America and, hence, provide the knowledge necessary to produce more accurate predictions. © Kluwer Academic Publishers 1991 |
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