Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds
Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wilmking, Martin [verfasserIn] Juday, Glenn P. [verfasserIn] Barber, Valerie A. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|
| Erschienen: |
Oxford, UK: Blackwell Science Ltd ; 2004 |
|---|
| Schlagwörter: |
|---|
| Umfang: |
Online-Ressource |
|---|
| Reproduktion: |
2004 ; Blackwell Publishing Journal Backfiles 1879-2005 |
|---|---|
| Übergeordnetes Werk: |
In: Global change biology - Oxford [u.a.] : Wiley-Blackwell, 1995, 10(2004), 10, Seite 0 |
| Übergeordnetes Werk: |
volume:10 ; year:2004 ; number:10 ; pages:0 |
| Links: |
|---|
| DOI / URN: |
10.1111/j.1365-2486.2004.00826.x |
|---|
| Katalog-ID: |
NLEJ242852386 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | NLEJ242852386 | ||
| 003 | DE-627 | ||
| 005 | 20210707165008.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 120427s2004 xx |||||o 00| ||und c | ||
| 024 | 7 | |a 10.1111/j.1365-2486.2004.00826.x |2 doi | |
| 035 | |a (DE-627)NLEJ242852386 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 100 | 1 | |a Wilmking, Martin |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| 264 | 1 | |a Oxford, UK |b Blackwell Science Ltd |c 2004 | |
| 300 | |a Online-Ressource | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. | ||
| 533 | |d 2004 |f Blackwell Publishing Journal Backfiles 1879-2005 |7 |2004|||||||||| | ||
| 650 | 4 | |a Alaska | |
| 700 | 1 | |a Juday, Glenn P. |e verfasserin |4 aut | |
| 700 | 1 | |a Barber, Valerie A. |e verfasserin |4 aut | |
| 700 | 1 | |a Zald, Harold S. J. |4 oth | |
| 773 | 0 | 8 | |i In |t Global change biology |d Oxford [u.a.] : Wiley-Blackwell, 1995 |g 10(2004), 10, Seite 0 |h Online-Ressource |w (DE-627)NLEJ243925816 |w (DE-600)2020313-5 |x 1365-2486 |7 nnns |
| 773 | 1 | 8 | |g volume:10 |g year:2004 |g number:10 |g pages:0 |
| 856 | 4 | 0 | |u http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x |q text/html |x Verlag |z Deutschlandweit zugänglich |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a ZDB-1-DJB | ||
| 912 | |a GBV_NL_ARTICLE | ||
| 951 | |a AR | ||
| 952 | |d 10 |j 2004 |e 10 |h 0 | ||
| author_variant |
m w mw g p j gp gpj v a b va vab |
|---|---|
| matchkey_str |
article:13652486:2004----::eetlmtwrigocsotatngotrsossfhtsrcatelniaa |
| hierarchy_sort_str |
2004 |
| publishDate |
2004 |
| allfields |
10.1111/j.1365-2486.2004.00826.x doi (DE-627)NLEJ242852386 DE-627 ger DE-627 rakwb Wilmking, Martin verfasserin aut Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Oxford, UK Blackwell Science Ltd 2004 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. 2004 Blackwell Publishing Journal Backfiles 1879-2005 |2004|||||||||| Alaska Juday, Glenn P. verfasserin aut Barber, Valerie A. verfasserin aut Zald, Harold S. J. oth In Global change biology Oxford [u.a.] : Wiley-Blackwell, 1995 10(2004), 10, Seite 0 Online-Ressource (DE-627)NLEJ243925816 (DE-600)2020313-5 1365-2486 nnns volume:10 year:2004 number:10 pages:0 http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 10 2004 10 0 |
| spelling |
10.1111/j.1365-2486.2004.00826.x doi (DE-627)NLEJ242852386 DE-627 ger DE-627 rakwb Wilmking, Martin verfasserin aut Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Oxford, UK Blackwell Science Ltd 2004 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. 2004 Blackwell Publishing Journal Backfiles 1879-2005 |2004|||||||||| Alaska Juday, Glenn P. verfasserin aut Barber, Valerie A. verfasserin aut Zald, Harold S. J. oth In Global change biology Oxford [u.a.] : Wiley-Blackwell, 1995 10(2004), 10, Seite 0 Online-Ressource (DE-627)NLEJ243925816 (DE-600)2020313-5 1365-2486 nnns volume:10 year:2004 number:10 pages:0 http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 10 2004 10 0 |
| allfields_unstemmed |
10.1111/j.1365-2486.2004.00826.x doi (DE-627)NLEJ242852386 DE-627 ger DE-627 rakwb Wilmking, Martin verfasserin aut Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Oxford, UK Blackwell Science Ltd 2004 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. 2004 Blackwell Publishing Journal Backfiles 1879-2005 |2004|||||||||| Alaska Juday, Glenn P. verfasserin aut Barber, Valerie A. verfasserin aut Zald, Harold S. J. oth In Global change biology Oxford [u.a.] : Wiley-Blackwell, 1995 10(2004), 10, Seite 0 Online-Ressource (DE-627)NLEJ243925816 (DE-600)2020313-5 1365-2486 nnns volume:10 year:2004 number:10 pages:0 http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 10 2004 10 0 |
| allfieldsGer |
10.1111/j.1365-2486.2004.00826.x doi (DE-627)NLEJ242852386 DE-627 ger DE-627 rakwb Wilmking, Martin verfasserin aut Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Oxford, UK Blackwell Science Ltd 2004 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. 2004 Blackwell Publishing Journal Backfiles 1879-2005 |2004|||||||||| Alaska Juday, Glenn P. verfasserin aut Barber, Valerie A. verfasserin aut Zald, Harold S. J. oth In Global change biology Oxford [u.a.] : Wiley-Blackwell, 1995 10(2004), 10, Seite 0 Online-Ressource (DE-627)NLEJ243925816 (DE-600)2020313-5 1365-2486 nnns volume:10 year:2004 number:10 pages:0 http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 10 2004 10 0 |
| allfieldsSound |
10.1111/j.1365-2486.2004.00826.x doi (DE-627)NLEJ242852386 DE-627 ger DE-627 rakwb Wilmking, Martin verfasserin aut Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Oxford, UK Blackwell Science Ltd 2004 Online-Ressource nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. 2004 Blackwell Publishing Journal Backfiles 1879-2005 |2004|||||||||| Alaska Juday, Glenn P. verfasserin aut Barber, Valerie A. verfasserin aut Zald, Harold S. J. oth In Global change biology Oxford [u.a.] : Wiley-Blackwell, 1995 10(2004), 10, Seite 0 Online-Ressource (DE-627)NLEJ243925816 (DE-600)2020313-5 1365-2486 nnns volume:10 year:2004 number:10 pages:0 http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x text/html Verlag Deutschlandweit zugänglich Volltext GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE AR 10 2004 10 0 |
| source |
In Global change biology 10(2004), 10, Seite 0 volume:10 year:2004 number:10 pages:0 |
| sourceStr |
In Global change biology 10(2004), 10, Seite 0 volume:10 year:2004 number:10 pages:0 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Alaska |
| isfreeaccess_bool |
false |
| container_title |
Global change biology |
| authorswithroles_txt_mv |
Wilmking, Martin @@aut@@ Juday, Glenn P. @@aut@@ Barber, Valerie A. @@aut@@ Zald, Harold S. J. @@oth@@ |
| publishDateDaySort_date |
2004-01-01T00:00:00Z |
| hierarchy_top_id |
NLEJ243925816 |
| id |
NLEJ242852386 |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ242852386</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707165008.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120427s2004 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-2486.2004.00826.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ242852386</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wilmking, Martin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Science Ltd</subfield><subfield code="c">2004</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2004</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2004||||||||||</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Alaska</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Juday, Glenn P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Barber, Valerie A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zald, Harold S. J.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Global change biology</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1995</subfield><subfield code="g">10(2004), 10, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243925816</subfield><subfield code="w">(DE-600)2020313-5</subfield><subfield code="x">1365-2486</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2004</subfield><subfield code="g">number:10</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2004</subfield><subfield code="e">10</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| series2 |
Blackwell Publishing Journal Backfiles 1879-2005 |
| author |
Wilmking, Martin |
| spellingShingle |
Wilmking, Martin misc Alaska Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| authorStr |
Wilmking, Martin |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)NLEJ243925816 |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut aut |
| collection |
NL |
| publishPlace |
Oxford, UK |
| remote_str |
true |
| illustrated |
Not Illustrated |
| issn |
1365-2486 |
| topic_title |
Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds Alaska |
| publisher |
Blackwell Science Ltd |
| publisherStr |
Blackwell Science Ltd |
| topic |
misc Alaska |
| topic_unstemmed |
misc Alaska |
| topic_browse |
misc Alaska |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
h s j z hsj hsjz |
| hierarchy_parent_title |
Global change biology |
| hierarchy_parent_id |
NLEJ243925816 |
| hierarchy_top_title |
Global change biology |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)NLEJ243925816 (DE-600)2020313-5 |
| title |
Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| ctrlnum |
(DE-627)NLEJ242852386 |
| title_full |
Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| author_sort |
Wilmking, Martin |
| journal |
Global change biology |
| journalStr |
Global change biology |
| isOA_bool |
false |
| recordtype |
marc |
| publishDateSort |
2004 |
| contenttype_str_mv |
zzz |
| container_start_page |
0 |
| author_browse |
Wilmking, Martin Juday, Glenn P. Barber, Valerie A. |
| container_volume |
10 |
| physical |
Online-Ressource |
| format_se |
Elektronische Aufsätze |
| author-letter |
Wilmking, Martin |
| doi_str_mv |
10.1111/j.1365-2486.2004.00826.x |
| author2-role |
verfasserin |
| title_sort |
recent climate warming forces contrasting growth responses of white spruce at treeline in alaska through temperature thresholds |
| title_auth |
Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| abstract |
Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. |
| abstractGer |
Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. |
| abstract_unstemmed |
Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios. |
| collection_details |
GBV_USEFLAG_U ZDB-1-DJB GBV_NL_ARTICLE |
| container_issue |
10 |
| title_short |
Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds |
| url |
http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x |
| remote_bool |
true |
| author2 |
Juday, Glenn P. Barber, Valerie A. Zald, Harold S. J. |
| author2Str |
Juday, Glenn P. Barber, Valerie A. Zald, Harold S. J. |
| ppnlink |
NLEJ243925816 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth |
| doi_str |
10.1111/j.1365-2486.2004.00826.x |
| up_date |
2024-07-06T03:24:47.502Z |
| _version_ |
1803798485404745729 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">NLEJ242852386</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20210707165008.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">120427s2004 xx |||||o 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1111/j.1365-2486.2004.00826.x</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)NLEJ242852386</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Wilmking, Martin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Recent climate warming forces contrasting growth responses of white spruce at treeline in Alaska through temperature thresholds</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Oxford, UK</subfield><subfield code="b">Blackwell Science Ltd</subfield><subfield code="c">2004</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Northern and high-latitude alpine treelines are generally thought to be limited by available warmth. Most studies of tree-growth–climate interaction at treeline as well as climate reconstructions using dendrochronology report positive growth response of treeline trees to warmer temperatures. However, population-wide responses of treeline trees to climate remain largely unexamined. We systematically sampled 1558 white spruce at 13 treeline sites in the Brooks Range and Alaska Range. Our findings of both positive and negative growth responses to climate warming at treeline challenge the widespread assumption that arctic treeline trees grow better with warming climate. High mean temperatures in July decreased the growth of 40% of white spruce at treeline areas in Alaska, whereas warm springs enhance growth of additional 36% of trees and 24% show no significant correlation with climate. Even though these opposing growth responses are present in all sampled sites, their relative proportion varies between sites and there is no overall clear relationship between growth response and landscape position within a site. Growth increases and decreases appear in our sample above specific temperature index values (temperature thresholds), which occurred more frequently in the late 20th century. Contrary to previous findings, temperature explained more variability in radial growth after 1950. Without accounting for these opposite responses and temperature thresholds, climate reconstructions based on ring width will miscalibrate past climate, and biogeochemical and dynamic vegetation models will overestimate carbon uptake and treeline advance under future warming scenarios.</subfield></datafield><datafield tag="533" ind1=" " ind2=" "><subfield code="d">2004</subfield><subfield code="f">Blackwell Publishing Journal Backfiles 1879-2005</subfield><subfield code="7">|2004||||||||||</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Alaska</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Juday, Glenn P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Barber, Valerie A.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zald, Harold S. J.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Global change biology</subfield><subfield code="d">Oxford [u.a.] : Wiley-Blackwell, 1995</subfield><subfield code="g">10(2004), 10, Seite 0</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)NLEJ243925816</subfield><subfield code="w">(DE-600)2020313-5</subfield><subfield code="x">1365-2486</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:10</subfield><subfield code="g">year:2004</subfield><subfield code="g">number:10</subfield><subfield code="g">pages:0</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.1111/j.1365-2486.2004.00826.x</subfield><subfield code="q">text/html</subfield><subfield code="x">Verlag</subfield><subfield code="z">Deutschlandweit zugänglich</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-1-DJB</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_NL_ARTICLE</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">10</subfield><subfield code="j">2004</subfield><subfield code="e">10</subfield><subfield code="h">0</subfield></datafield></record></collection>
|
| score |
7.400505 |