Abstract
We have developed a 247-year ring-width chronology of Betura ermanii Cham. growing in an open canopy forest close to the tree line at a coastal site in southern Kamchatka. Climatic response analyses revealed that the ring width was primarily controlled by July-August temperature. The regression models that we used for statistical reconstruction passed the stringent calibration-verification tests used in dendroclimatology, resulting in the first quality-controlled tree-ring reconstruction for southern Kamchatka. The reconstructed temperature shows a cool period from the 1830s to the 1880s, followed by gradual warming until ca. 1940, then a cooling trend extending to the 1970s, and finally a warming trend continuing to the present. Spatial correlation analyses with sea surface temperature in the North Pacific indicated that the seas surrounding the Kamchatka peninsula play a role in modulating temperature variations in the study area whereas the effects of the Pacific Decadal Oscillation are relatively weak.
| Original language | English |
|---|---|
| Pages (from-to) | 234-240 |
| Number of pages | 7 |
| Journal | Journal of Forest Research |
| Volume | 15 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 2010 |
| Externally published | Yes |
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Keywords
- Climate reconstruction
- Dendrochronology
- Pacific Decadal Oscillation
- Sea surface temperature
ASJC Scopus subject areas
- Forestry
Cite this
Summer temperature variations in southern Kamchatka as reconstructed from a 247-year tree-ring chronology of Betula ermanii. / Sano, Masaki; Furuta, Fumito; Sweda, Tatsuo.
In: Journal of Forest Research, Vol. 15, No. 4, 2010, p. 234-240.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Summer temperature variations in southern Kamchatka as reconstructed from a 247-year tree-ring chronology of Betula ermanii
AU - Sano, Masaki
AU - Furuta, Fumito
AU - Sweda, Tatsuo
PY - 2010
Y1 - 2010
N2 - We have developed a 247-year ring-width chronology of Betura ermanii Cham. growing in an open canopy forest close to the tree line at a coastal site in southern Kamchatka. Climatic response analyses revealed that the ring width was primarily controlled by July-August temperature. The regression models that we used for statistical reconstruction passed the stringent calibration-verification tests used in dendroclimatology, resulting in the first quality-controlled tree-ring reconstruction for southern Kamchatka. The reconstructed temperature shows a cool period from the 1830s to the 1880s, followed by gradual warming until ca. 1940, then a cooling trend extending to the 1970s, and finally a warming trend continuing to the present. Spatial correlation analyses with sea surface temperature in the North Pacific indicated that the seas surrounding the Kamchatka peninsula play a role in modulating temperature variations in the study area whereas the effects of the Pacific Decadal Oscillation are relatively weak.
AB - We have developed a 247-year ring-width chronology of Betura ermanii Cham. growing in an open canopy forest close to the tree line at a coastal site in southern Kamchatka. Climatic response analyses revealed that the ring width was primarily controlled by July-August temperature. The regression models that we used for statistical reconstruction passed the stringent calibration-verification tests used in dendroclimatology, resulting in the first quality-controlled tree-ring reconstruction for southern Kamchatka. The reconstructed temperature shows a cool period from the 1830s to the 1880s, followed by gradual warming until ca. 1940, then a cooling trend extending to the 1970s, and finally a warming trend continuing to the present. Spatial correlation analyses with sea surface temperature in the North Pacific indicated that the seas surrounding the Kamchatka peninsula play a role in modulating temperature variations in the study area whereas the effects of the Pacific Decadal Oscillation are relatively weak.
KW - Climate reconstruction
KW - Dendrochronology
KW - Pacific Decadal Oscillation
KW - Sea surface temperature
UR - http://www.scopus.com/inward/record.url?scp=77955087439&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=77955087439&partnerID=8YFLogxK
U2 - 10.1007/s10310-010-0183-z
DO - 10.1007/s10310-010-0183-z
M3 - Article
AN - SCOPUS:77955087439
VL - 15
SP - 234
EP - 240
JO - Journal of Forest Research
JF - Journal of Forest Research
SN - 1341-6979
IS - 4
ER -