A ring-width-based reconstruction of June–July minimum temperatures since AD 1245 from white spruce stands in the Mackenzie Delta region, northwestern Canada
Bibliographic Data
| ID | 24088809 |
|---|---|
| Authors | Trevor J Porter (0000-0002-5916-1998, University of Alberta, corresponding author), Michael Fj Pisaric (0000-0003-3806-8986, Brock University), Michael F J Pisaric, Steven V Kokelj (0000-0002-2840-2605, Aboriginal Affairs Northern Dev Canada), Peter deMontigny (Carleton University) |
| Year | 2013 |
| Volume | 80 |
| Issue | 2 |
| Pages | 167-179 |
| Publication date | 2013-09-01 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Quaternary Research (JOURNAL) |
| Journal identifiers | ISSN: 0033-5894 • E-ISSN: 1096-0287 |
| Publisher | Cambridge University Press (CUP) (PUBLISHER) |
| DOI | 10.1016/j.yqres.2013.05.004 |
| OpenAlex | W1979315892 |
| Language | EN |
| Citations received | 3 |
| References cited | 53 |
We present a reconstruction of June–July minimum temperatures since AD 1245 for the Mackenzie Delta region based on a 29-site network of white spruce ( Picea glauca ) ring-width series. Most but not all trees experienced a divergent temperature–growth response, similar to the divergence that has affected other white spruce trees across Yukon and Alaska. However, divergence in the study region began as early as AD 1900 and we have documented our methods to avoid including divergent signals in the reconstruction. Calibration/verification testing based on local temperature data, and multi-century coherence with nearby and large-scale temperature proxy records, confirm that our reconstruction is robust. The reconstruction shows cool conditions in the late 13th, early 18th and early 19th centuries, corresponding with solar minima and increased volcanism. These cool periods are interrupted by warm periods consistent with early to mid-20th century warmth. The late 20th century is the warmest interval, and the last decade is estimated to be 1.4°C warmer than any decade before the mid-20th century. The reconstructed climate history corroborates other proxy-based inferences and supports the notion that high-latitude regions such as the Mackenzie Delta have experienced rapid warming in recent decades that is exceptional in the last eight centuries.
Climate change · Climatology · Delta · Dendrochronology · Dendroclimatology · Geodesy · Geography · Latitude · Little ice age · Paleoclimatology · Physical geography · Proxy (statistics) · Geology · Geology and Paleoclimatology Research · Oceanography · Paleontology · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses
Reconstruction of past temperature and climate anomalies from tree rings of Fokienia hodginsii in South-Central Vietnam
A Direct Comparison of Sympatric High-Latitude Pinus contorta and Picea albertiana Ring-Width Chronologies
Tundra vegetation stability versus lake-basin variability on the Yukon Coastal Plain (NW Canada) during the past three centuries
Dendroclimatic Reconstruction of Summer Temperatures in Northwestern Canada since A.D. 1638 Based on Age-Dependent Modeling
Recent Warming Reverses Long-Term Arctic Cooling
The Circumpolar Arctic vegetation map
The evidence for shrub expansion in Northern Alaska and the Pan‐Arctic
Uncertainty estimates in regional and global observed temperature changes
Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability
A 1,400-year tree-ring record of summer temperatures in Fennoscandia
Varying boreal forest response to Arctic environmental change at the Firth River, Alaska
Responses of the circumpolar boreal forest to 20th century climate variability
Dendroclimatic reconstruction of maximum summer temperatures from upper treeline sites in Interior British Columbia, Canada
A 930-year ring-width chronology from moisture-sensitive white spruce (Picea glauca Moench) in northwestern Canada
The 'segment length curse' in long tree-ring chronology development for palaeoclimatic studies
Tree-ring width and density data around the Northern Hemisphere
Cross-dating methods in dendrochronology
| Unique citing works | 3 |
|---|---|
| Citations per year | 0,33 |
| Citation span | 2017 - 2026 (10) |
| Citation velocity | current |
| Highly cited | No |
| Citation types | Neutral: 1 |