Firth River Tree Ring Data [Anchukaitis, K.]
106.460
Northwestern North America has one of the highest rates of recent temperature increase in the world, but the putative "divergence problem" in dendroclimatology potentially limits the ability of tree-ring proxy data at high latitudes to provide long-term context for current anthropogenic change. Here, summer temperatures are reconstructed from a Picea glauca maximum latewood density (MXD) chronology that shows a stable relationship to regional temperatures and spans most of the last millennium at the Firth River in northeastern Alaska. The warmest epoch in the last nine centuries is estimated to have occurred during the late twentieth century, with average temperatures over the last 30 yr of the reconstruction developed for this study [1973-2002 in the Common Era (CE)] approximately 1.3° ± 0.4°C warmer than the long-term preindustrial mean (1100-1850 CE), a change associated with rapid increases in greenhouse gases. Prior to the late twentieth century, multidecadal temperature fluctuations covary broadly with changes in natural radiative forcing. The findings presented here emphasize that tree-ring proxies can provide reliable indicators of temperature variability even in a rapidly warming climate.
dataset
https://data.eol.ucar.edu//dataset/106.460
protocol: https
name: Firth River Tree Ring Data [Anchukaitis, K.] homepage
description: Dataset homepage
106.460
climatologyMeteorologyAtmosphere
dataset
revision
2014-10-16
Field Surveys
Land Based
Ecology
Paleoclimatology
Arctic
Biology
EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > TREE RINGS
EARTH SCIENCE > BIOSPHERE > VEGETATION > TREE RINGS
EARTH SCIENCE > CLIMATE INDICATORS > PALEOCLIMATE INDICATORS > BIOLOGICAL RECORDS > TREE RINGS
revision
2018-02-27
-141.63000
-141.63000
68.65000
68.65000
1073-01-01T00:00:00Z
2002-12-31T23:59:59Z
publication
2015-05-26T19:24:03Z
none
none
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pointOfContact
EOL Data Support
UCAR/NCAR - Earth Observing Laboratory
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80307-3000
name: homepage
pointOfContact
2024-02-07T22:42:23Z