Tree Rings and Temperatures

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Combining precipitation <strong>and</strong> temperature- sensitive tree-ring series to reconstruct glacier mass balance +70 -317 Cumulative net mass balance (blue solid line) Mean balances 1673-1883. +70 mm w.e./yr. 1883-1993 -317 mm w.e./yr. Dated moraines in Canadian Rockies (66 glaciers) (in 25 year intervals) Net Mass balance 1673-1995 Reconstructed from tree rings (Watson <strong>and</strong> Luckman 2004) Main moraine building periods follow times of strong positive mass balance
And, at a global scale High frequency precipitation variability influenced by ENSO Comparisons based on proxy climate data (Villalba et al., in press)
Page 1 and 2: Tree rings and temperatures Brian L
Page 3 and 4: Tree Rings Deliver • A precisely
Page 5 and 6: All series rigourously checked to e
Page 7 and 8: there is no change in the limiting
Page 9 and 10: Tree-ring Densitometry Precisely sa
Page 11 and 12: Negative exponential Linear negativ
Page 13 and 14: The Principle of Aggregate Tree Gro
Page 15 and 16: Long tree-ring chronologies and old
Page 17 and 18: Athabasca Glacier Maximum May-Augus
Page 19 and 20: Comparison with other Northern Hemi
Page 21 and 22: Northern Hemisphere densitometric c
Page 23 and 24: Annual maps show strong but regiona
Page 25 and 26: Interhemispheric Linkages ( tempera
Page 28 and 29: Comparison of three millennial leng
Page 30 and 31: Challenges basic assumptions of den
Page 32 and 33: 68-69°N, 18-28°E 65°N, 69°E 65
Page 34 and 35: Major droughts on the Canadian Prai
Page 38 and 39: Take home messages trees are not th

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