noaa-recon-6342
Pauling et al. 2006 European Gridded Seasonal Precipitation Reconstructions
Pauling, A.; Luterbacher, J.; Casty, C.; Wanner, H.
Pauling et al. 2006 European Gridded Seasonal Precipitation Reconstructions
2006-07-01
NCDC-Paleoclimatology
ONLINE Files
Pending
https://www.ncdc.noaa.gov/paleo/study/6342
Investigator
A.
Pauling
Investigator
J.
Luterbacher
Investigator
C.
Casty
Investigator
H.
Wanner
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Sep-Nov,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Mar-May,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Jun-Aug,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Sep-Nov,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Mar-May,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Jun-Aug,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Dec-Feb,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Sep-Nov,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Dec-Feb,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Dec-Feb,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Mar-May,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Sep-Nov,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Mar-May,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Dec-Feb,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Sep-Nov,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Jun-Aug,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Dec-Feb,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Sep-Nov,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Dec-Feb,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error upper bound,millimeter,Mar-May,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Jun-Aug,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,two standard error lower bound,millimeter,Mar-May,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Jun-Aug,climate reconstructions,null,principal component analysis|regression analysis,N,Data from 1901-2000 are observational estimates from the Mitchell and Jones (2005) dataset. Data prior to 1901 are reconstructed values; principal components regression
earth science
paleoclimate
climate reconstructions
age,null,null,year Common Era,null,climate reconstructions,null,null,N,null
earth science
paleoclimate
climate reconstructions
precipitation,multiple proxies,null,millimeter,Jun-Aug,climate reconstructions,averaged,principal component analysis|regression analysis,N,European spatial average; principal components regression
earth science
paleoclimate
reconstructions
geoscientificInformation
Precipitation Reconstruction
1500 AD
2000 AD
450 cal yr BP
-50 cal yr BP
Complete
30
71
-30
40
Continent
Europe
Europe to 30N/30W>LATITUDE >LONGITUDE
None
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English
DOC/NOAA/NESDIS/NCEI
National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce
https://www.ncdc.noaa.gov/data-access/paleoclimatology-data
DATA Center Contact
Bruce
Bauer
bruce.a.bauer@noaa.gov
paleo@noaa.gov
303-497-6280
303-497-6513
325 Broadway, E/NE31
Boulder
CO
80305-3328
USA
online
ASCII
Records of past temperature, precipitation, and other climate variables derived from paleoclimate proxies. Parameter keywords describe what was measured in this data set. Additional summary information can be found in the abstracts of papers listed in the data set citations.
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/precmean-pauling-au.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/readme-pauling2006.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/prec-pauling-sp.txt.gz
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/prec-pauling-su.txt.gz
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/precmean-pauling-wi.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/prec-pauling-au.txt.gz
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/precmean-pauling-sp.txt
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/prec-pauling-wi.txt.gz
GET DATA
https://www1.ncdc.noaa.gov/pub/data/paleo/historical/europe/pauling2006precip/precmean-pauling-su.txt
USA/NOAA
DIF
Version 9.8.4
2019-03-06
2019-03-06