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Spring-Summer Temperatures Since AD 1780 Reconstructed from Stable Oxygen Isotope Ratios in White Spruce Tree-Rings from the Mackenzie Delta, Northwestern CanadaHigh-latitude delta(exp 18)O archives deriving from meteoric water (e.g., tree-rings and ice-cores) can provide valuable information on past temperature variability, but stationarity of temperature signals in these archives depends on the stability of moisture source/trajectory and precipitation seasonality, both of which can be affected by atmospheric circulation changes. A tree-ring delta(exp 18)O record (AD 1780-2003) from the Mackenzie Delta is evaluated as a temperature proxy based on linear regression diagnostics. The primary source of moisture for this region is the North Pacific and, thus, North Pacific atmospheric circulation variability could potentially affect the tree-ring delta(exp 18)O-temperature signal. Over the instrumental period (AD 1892-2003), tree-ring delta(exp 18)O explained 29% of interannual variability in April-July minimum temperatures, and the explained variability increases substantially at lower-frequencies. A split-period calibration/verification analysis found the delta(exp 18)O-temperature relation was time-stable, which supported a temperature reconstruction back to AD 1780. The stability of the delta(exp 18)O-temperature signal indirectly implies the study region is insensitive to North Pacific circulation effects, since North Pacific circulation was not constant over the calibration period. Simulations from the NASA-GISS ModelE isotope-enabled general circulation model confirm that meteoric delta(exp 18)O and precipitation seasonality in the study region are likely insensitive to North Pacific circulation effects, highlighting the paleoclimatic value of tree-ring and possibly other delta(exp 18)O records from this region. Our delta(exp 18)O-based temperature reconstruction is the first of its kind in northwestern North America, and one of few worldwide, and provides a long-term context for evaluating recent climate warming in the Mackenzie Delta region.
Document ID
20150002123
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
Authors
Porter, Trevor J.
(Alberta Univ. Edmonton, Alberta, Canada)
Pisaric, Michael F. J.
(Carleton Univ. Ottawa, Ontario, Canada)
Field, Robert D.
(Columbia Univ. New York, NY, United States)
Kokelj, Steven V.
(Aboriginal Affairs and Northern Development Canada Yellowknife, Canada)
Edwards, Thomas W. D.
(Waterloo Univ. Ontario, Canada)
deMontigny, Peter
(Carleton Univ. Ottawa, Ontario, Canada)
Healy, Richard
(Columbia Univ. New York, NY, United States)
LeGrande, Allegra N.
(NASA Goddard Inst. for Space Studies New York, NY, United States)
Date Acquired
February 25, 2015
Publication Date
January 30, 2013
Publication Information
Publication: Climate Dynamics
Publisher: Springer
Volume: 42
Issue: 4-Mar
Subject Category
Meteorology And Climatology
Report/Patent Number
GSFC-E-DAA-TN18988
Funding Number(s)
CONTRACT_GRANT: NNX14AB99A
Distribution Limits
Public
Copyright
Public Use Permitted.
Keywords
Canada
Tree rings
Temperature
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