Tarmo Aalto
Biographic Data
| ID | 6570676 |
|---|---|
| NAME | Tarmo Aalto |
| GIVEN NAMES | Tarmo |
| FAMILY NAME | Aalto |
| SIGNATURE | AALTO T |
| AFFILIATIONS | Metla, Rovaniemi Research Unit, PO Box 16, FI 96301 Rovaniemi, Finland |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 5 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2009 |
| LATEST PUBLICATION YEAR | 2010 |
| H-INDEX | 2 |
The height-increment record of summer temperature extended over the last millennium in Fennoscandia
New data have allowed us to extend a previous height-increment chronology of Scots pine ( Pinus sylvestris L.) at the northern Fennoscandian timberline 817 years backwards in time, from 1561 to 745. Our final transfer model accounts for 31% of the dependent instrumental (mean June—August) temperature variance between 1908 and 2007. According to the 1263 yr long summer temperature proxy, the most severe summers were experienced in 1601, 1790 and 7…
A summer temperature proxy from height increment of Scots pine since 1561 at the northern timberline in Fennoscandia
Height increments of 60 Scots pine trees were used to reconstruct mean June—August temperature variability at interannual to decadal scales from 1561 to 2004. Three standardization methods (67%, 33% flexible splines, and a fixed 22 years spline) were compared in building chronologies in order to optimize the frequency response in relation to major climatic forcing factors. The height-growth chronology built using the 33% spline standardization pr…
The height-increment record of summer temperature extended over the last millennium in Fennoscandia
New data have allowed us to extend a previous height-increment chronology of Scots pine ( Pinus sylvestris L.) at the northern Fennoscandian timberline 817 years backwards in time, from 1561 to 745. Our final transfer model accounts for 31% of the dependent instrumental (mean June—August) temperature variance between 1908 and 2007. According to the 1263 yr long summer temperature proxy, the most severe summers were experienced in 1601, 1790 and 7…
A summer temperature proxy from height increment of Scots pine since 1561 at the northern timberline in Fennoscandia
Height increments of 60 Scots pine trees were used to reconstruct mean June—August temperature variability at interannual to decadal scales from 1561 to 2004. Three standardization methods (67%, 33% flexible splines, and a fixed 22 years spline) were compared in building chronologies in order to optimize the frequency response in relation to major climatic forcing factors. The height-growth chronology built using the 33% spline standardization pr…
A summer temperature proxy from height increment of Scots pine since 1561 at the northern timberline in Fennoscandia
Height increments of 60 Scots pine trees were used to reconstruct mean June—August temperature variability at interannual to decadal scales from 1561 to 2004. Three standardization methods (67%, 33% flexible splines, and a fixed 22 years spline) were compared in building chronologies in order to optimize the frequency response in relation to major climatic forcing factors. The height-growth chronology built using the 33% spline standardization pr…
The height-increment record of summer temperature extended over the last millennium in Fennoscandia
New data have allowed us to extend a previous height-increment chronology of Scots pine ( Pinus sylvestris L.) at the northern Fennoscandian timberline 817 years backwards in time, from 1561 to 745. Our final transfer model accounts for 31% of the dependent instrumental (mean June—August) temperature variance between 1908 and 2007. According to the 1263 yr long summer temperature proxy, the most severe summers were experienced in 1601, 1790 and 7…
Archaeology (2 works) · Chronology (2 works) · Climatology (2 works) · Environmental Science (2 works) · Forcing (mathematics (2 works) · Geography (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Physical geography (2 works) · Pinus (2 works)