Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction
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 ch...
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EOL Data Support. UCAR/NCAR - Earth Observing Laboratory
2020
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ftdatacite:10.18739/a2bc3sz08 2023-05-15T15:06:44+02:00 Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction Anchukaitis, Kevin D'Arrigo, Rosanne Hayles, Laia Frank, David Verstege, Anne Curtis, Ashley Buckley, Brendan Jacoby, Gordon Cook, Edward 2020 text/xml https://dx.doi.org/10.18739/a2bc3sz08 https://arcticdata.io/catalog/view/doi:10.18739/A2BC3SZ08 en eng EOL Data Support. UCAR/NCAR - Earth Observing Laboratory Arctic Ecology FOS Biological sciences climatologyMeteorologyAtmosphere dataset Dataset 2020 ftdatacite https://doi.org/10.18739/a2bc3sz08 2021-11-05T12:55:41Z 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*deg* *plusmn* 0.4*deg*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 Arctic Alaska DataCite Metadata Store (German National Library of Science and Technology) Arctic Firth River ENVELOPE(-139.508,-139.508,69.542,69.542) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Arctic Ecology FOS Biological sciences climatologyMeteorologyAtmosphere |
spellingShingle |
Arctic Ecology FOS Biological sciences climatologyMeteorologyAtmosphere Anchukaitis, Kevin D'Arrigo, Rosanne Hayles, Laia Frank, David Verstege, Anne Curtis, Ashley Buckley, Brendan Jacoby, Gordon Cook, Edward Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
topic_facet |
Arctic Ecology FOS Biological sciences climatologyMeteorologyAtmosphere |
description |
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*deg* *plusmn* 0.4*deg*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. |
format |
Dataset |
author |
Anchukaitis, Kevin D'Arrigo, Rosanne Hayles, Laia Frank, David Verstege, Anne Curtis, Ashley Buckley, Brendan Jacoby, Gordon Cook, Edward |
author_facet |
Anchukaitis, Kevin D'Arrigo, Rosanne Hayles, Laia Frank, David Verstege, Anne Curtis, Ashley Buckley, Brendan Jacoby, Gordon Cook, Edward |
author_sort |
Anchukaitis, Kevin |
title |
Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
title_short |
Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
title_full |
Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
title_fullStr |
Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
title_full_unstemmed |
Firth River Alaska 930 Year Maximum Latewood Density Temperature Reconstruction |
title_sort |
firth river alaska 930 year maximum latewood density temperature reconstruction |
publisher |
EOL Data Support. UCAR/NCAR - Earth Observing Laboratory |
publishDate |
2020 |
url |
https://dx.doi.org/10.18739/a2bc3sz08 https://arcticdata.io/catalog/view/doi:10.18739/A2BC3SZ08 |
long_lat |
ENVELOPE(-139.508,-139.508,69.542,69.542) |
geographic |
Arctic Firth River |
geographic_facet |
Arctic Firth River |
genre |
Arctic Alaska |
genre_facet |
Arctic Alaska |
op_doi |
https://doi.org/10.18739/a2bc3sz08 |
_version_ |
1766338295622533120 |