A matter of divergence: Tracking recent warming at hemispheric scales using tree ring data

Publication Type  Journal Article
Year of Publication  2007
Authors  Wilson, R.; D'Arrigo, R.; Buckley, B.; Buntgen, U.; Esper, J.; Frank, D.; Luckman, B.; Payette, S.; Vose, R.; Youngblut, D.
Journal Title  Journal of Geophysical Research-Atmospheres
Volume  112
Issue  D17
Pages  -
Journal Date  Sep 11
ISBN Number  0148-0227
Accession Number  ISI:000249518500005
Key Words  decadal temperature variability; maximum latewood density; summer temperatures; dendroclimatic reconstruction; growth/climate response; minimum temperature; width chronology; growth-responses; last millennium; european alps
Abstract  

No current tree ring (TR) based reconstruction of extratropical Northern Hemisphere (ENH) temperatures that extends into the 1990s captures the full range of late 20th century warming observed in the instrumental record. Over recent decades, a divergence between cooler reconstructed and warmer instrumental large-scale temperatures is observed. We hypothesize that this problem is partly related to the fact that some of the constituent chronologies used for previous reconstructions show divergence against local temperatures in the recent period. In this study, we compiled TR data and published local/regional reconstructions that show no divergence against local temperatures. These data have not been included in other large-scale temperature reconstructions. Utilizing this data set, we developed a new, completely independent reconstruction of ENH annual temperatures (1750-2000). This record is not meant to replace existing reconstructions but allows some degree of independent validation of these earlier studies as well as demonstrating that TR data can better model recent warming at large scales when careful selection of constituent chronologies is made at the local scale. Although the new series tracks the increase in ENH annual temperatures over the last few decades better than any existing reconstruction, it still slightly under predicts values in the post-1988 period. We finally discuss possible reasons why it is so difficult to model post-mid-1980s warming, provide some possible alternative approaches with regards to the instrumental target and detail several recommendations that should be followed in future large-scale reconstruction attempts that may result in more robust temperature estimates.

Notes  

211IWTimes Cited:2Cited References Count:80

URL  <Go to ISI>://000249518500005
DOI  Doi 10.1029/2006jd008318