Estimates of White Spruce density at two elevations from 1600-present

Paleoecological investigations of ecosystem responses to past climate change can provide insight into plausible scenarios of response to future change and can elucidate factors that may influence the overall predictability of such responses. There is particular interest in the rate at which subarcti...

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Other Authors: ChristopherFastie
Format: Dataset
Language:unknown
Published: Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 2011
Subjects:
Online Access:http://hdl.handle.net/10255/dryad.12074
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.90.8/xml
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spelling ftdryad:oai:v1.datadryad.org:10255/dryad.12074 2023-05-15T13:09:36+02:00 Estimates of White Spruce density at two elevations from 1600-present ChristopherFastie This is a treeline site in the White Mts. -147.3333333 W -144.05 E 65.5 N 63.25 S 2002-06-01 to 2002-09-28 2011-04-21T16:23:48Z http://hdl.handle.net/10255/dryad.12074 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.90.8/xml unknown Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.90.8/xml knb-lter-bnz.90.8 http://hdl.handle.net/10255/dryad.12074 Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set. paleoecological climate picea spruce tundra forests warming white mountains Alaska Range treeline tree line dataset 2011 ftdryad 2020-01-01T14:26:52Z Paleoecological investigations of ecosystem responses to past climate change can provide insight into plausible scenarios of response to future change and can elucidate factors that may influence the overall predictability of such responses. There is particular interest in the rate at which subarctic Picea populations respond to climate change, as the rate of conversion from tundra to forest may affect the rate of future climate warming. We investigated recent changes in the structure and distribution of treeline white spruce forests in the White Mountains and the Alaska Range. Treeline advance was ubiquitous, but asynchronous in time, occurring significantly earlier in the White Mountains in interior Alaska than in the Alaska Range. The mean lag between initiation of recruitment and forest development was estimated at approximately 200 years, similar to what modeling studies have found. Although continued advance of Picea is the most likely scenario of future change, the recent history of treeline advance suggests that nonlinear responses to warming may be likely due to nonlinear growth responses of individual trees to temperature, limitation of Picea establishment in highly permafrost-affected sites, and decreasing seed availability as the advancing front moves farther from dense seed sources. All of these factors may cause Picea populations to respond nonlinearly to future warming, and these potential nonlinearities caution against uncritical extrapolation from recent trends. Dataset alaska range permafrost Subarctic Tundra Alaska Dryad Digital Repository (Duke University)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic paleoecological
climate
picea
spruce
tundra
forests
warming
white mountains
Alaska Range
treeline
tree line
spellingShingle paleoecological
climate
picea
spruce
tundra
forests
warming
white mountains
Alaska Range
treeline
tree line
Estimates of White Spruce density at two elevations from 1600-present
topic_facet paleoecological
climate
picea
spruce
tundra
forests
warming
white mountains
Alaska Range
treeline
tree line
description Paleoecological investigations of ecosystem responses to past climate change can provide insight into plausible scenarios of response to future change and can elucidate factors that may influence the overall predictability of such responses. There is particular interest in the rate at which subarctic Picea populations respond to climate change, as the rate of conversion from tundra to forest may affect the rate of future climate warming. We investigated recent changes in the structure and distribution of treeline white spruce forests in the White Mountains and the Alaska Range. Treeline advance was ubiquitous, but asynchronous in time, occurring significantly earlier in the White Mountains in interior Alaska than in the Alaska Range. The mean lag between initiation of recruitment and forest development was estimated at approximately 200 years, similar to what modeling studies have found. Although continued advance of Picea is the most likely scenario of future change, the recent history of treeline advance suggests that nonlinear responses to warming may be likely due to nonlinear growth responses of individual trees to temperature, limitation of Picea establishment in highly permafrost-affected sites, and decreasing seed availability as the advancing front moves farther from dense seed sources. All of these factors may cause Picea populations to respond nonlinearly to future warming, and these potential nonlinearities caution against uncritical extrapolation from recent trends.
author2 ChristopherFastie
format Dataset
title Estimates of White Spruce density at two elevations from 1600-present
title_short Estimates of White Spruce density at two elevations from 1600-present
title_full Estimates of White Spruce density at two elevations from 1600-present
title_fullStr Estimates of White Spruce density at two elevations from 1600-present
title_full_unstemmed Estimates of White Spruce density at two elevations from 1600-present
title_sort estimates of white spruce density at two elevations from 1600-present
publisher Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251
publishDate 2011
url http://hdl.handle.net/10255/dryad.12074
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.90.8/xml
op_coverage This is a treeline site in the White Mts.
-147.3333333 W -144.05 E 65.5 N 63.25 S
2002-06-01 to 2002-09-28
genre alaska range
permafrost
Subarctic
Tundra
Alaska
genre_facet alaska range
permafrost
Subarctic
Tundra
Alaska
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.90.8/xml
knb-lter-bnz.90.8
http://hdl.handle.net/10255/dryad.12074
op_rights Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set.
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