DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES

Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few av...
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Autor*in:	LUCKMAN, BRIAN H. [verfasserIn]

Format:	Artikel
Sprache:	Englisch

Erschienen:	1997

Schlagwörter:	Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record

Systematik:	RA 1000

Anmerkung:	© Kluwer Academic Publishers 1997

Übergeordnetes Werk:	Enthalten in: Climatic change - Kluwer Academic Publishers, 1977, 36(1997), 3-4 vom: Juli, Seite 455-476
Übergeordnetes Werk:	volume:36 ; year:1997 ; number:3-4 ; month:07 ; pages:455-476

Links:	Volltext

DOI / URN:	10.1023/A:1005376713554

Katalog-ID:	OLC2062585691

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520			\|a Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale.
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allfields	10.1023/A:1005376713554 doi (DE-627)OLC2062585691 (DE-He213)A:1005376713554-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk LUCKMAN, BRIAN H. verfasserin aut DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record Enthalten in Climatic change Kluwer Academic Publishers, 1977 36(1997), 3-4 vom: Juli, Seite 455-476 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:36 year:1997 number:3-4 month:07 pages:455-476 https://doi.org/10.1023/A:1005376713554 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_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 36 1997 3-4 07 455-476
spelling	10.1023/A:1005376713554 doi (DE-627)OLC2062585691 (DE-He213)A:1005376713554-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk LUCKMAN, BRIAN H. verfasserin aut DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record Enthalten in Climatic change Kluwer Academic Publishers, 1977 36(1997), 3-4 vom: Juli, Seite 455-476 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:36 year:1997 number:3-4 month:07 pages:455-476 https://doi.org/10.1023/A:1005376713554 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_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 36 1997 3-4 07 455-476
allfields_unstemmed	10.1023/A:1005376713554 doi (DE-627)OLC2062585691 (DE-He213)A:1005376713554-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk LUCKMAN, BRIAN H. verfasserin aut DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record Enthalten in Climatic change Kluwer Academic Publishers, 1977 36(1997), 3-4 vom: Juli, Seite 455-476 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:36 year:1997 number:3-4 month:07 pages:455-476 https://doi.org/10.1023/A:1005376713554 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_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 36 1997 3-4 07 455-476
allfieldsGer	10.1023/A:1005376713554 doi (DE-627)OLC2062585691 (DE-He213)A:1005376713554-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk LUCKMAN, BRIAN H. verfasserin aut DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record Enthalten in Climatic change Kluwer Academic Publishers, 1977 36(1997), 3-4 vom: Juli, Seite 455-476 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:36 year:1997 number:3-4 month:07 pages:455-476 https://doi.org/10.1023/A:1005376713554 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_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 36 1997 3-4 07 455-476
allfieldsSound	10.1023/A:1005376713554 doi (DE-627)OLC2062585691 (DE-He213)A:1005376713554-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk LUCKMAN, BRIAN H. verfasserin aut DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1997 Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record Enthalten in Climatic change Kluwer Academic Publishers, 1977 36(1997), 3-4 vom: Juli, Seite 455-476 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:36 year:1997 number:3-4 month:07 pages:455-476 https://doi.org/10.1023/A:1005376713554 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_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_130 GBV_ILN_154 GBV_ILN_381 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4325 RA 1000 AR 36 1997 3-4 07 455-476
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author	LUCKMAN, BRIAN H.
spellingShingle	LUCKMAN, BRIAN H. ddc 550 ssgn 14 rvk RA 1000 misc Glacier Area misc Glacier Inventory misc Residual Chronology misc Standard Chronology misc Proxy Climate Record DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES
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topic_title	550 VZ 14 ssgn RA 1000 VZ rvk DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES Glacier Area Glacier Inventory Residual Chronology Standard Chronology Proxy Climate Record
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title	DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES
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title_full	DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES
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title_sort	developing a proxy climate record for the last 300 years in the canadian rockies – some problems and opportunities
title_auth	DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES
abstract	Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. © Kluwer Academic Publishers 1997
abstractGer	Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. © Kluwer Academic Publishers 1997
abstract_unstemmed	Abstract Available meteorological, dendrochronological and glacier area change data are reviewed for the central Canadian Rockies. Limited glacier inventory studies indicate a loss of ca 25% of glacier area (greater for smaller glaciers) since the Little Ice Age maximum 130–150 years ago. The few available long climacte records are from widely spaced, valley floor sites, well below treeline. Available gridded or regional climate data sets similarly contain no high elevation sites. The five long (75 yr) station records contain a strong common signal but show differences in the relative amplitude and timing of temperature variations indicating links to either prairie or pacific stations. However the station network is too sparse to define the spatial extent of these patterns. Tree-ring chronologies from a network of Picea engelmannii (21), Larix lyallii (17) and Pinus albicaulis (2) treeline sites are presented and reviewed. Residual chronologies show stronger intercorrelation than standard chronologies and the larix chronologies are more highly correlated than picea, probably because of the narrower range of sites sampled. Many standard chronologies show a strong common regional signal of above average growth in the late 17th, late 18th and mid-20th centuries and reduced growth in the early 17th, early 18th and for most of the 19th centuries. However, examination of individual chronologies shows strong local or sub-regional divergence from this pattern that reflects smaller scale climate or non-climatic influences. Differences in the density and location of sites between the climate and tree-ring networks will create problems in resolving climate variation at the sub-regional scale. © Kluwer Academic Publishers 1997
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title_short	DEVELOPING A PROXY CLIMATE RECORD FOR THE LAST 300 YEARS IN THE CANADIAN ROCKIES – SOME PROBLEMS AND OPPORTUNITIES
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