NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized
R= -0.56 P auto < 0.001 RMSEP = 43.0 mm/year,mm/year,Annual,climate reconstruction,5 year filter,Statistical model,N,
"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized
Length < 4000yrs but in region of limited coverage
R= -0.56 P auto < 0.001 RMSEP = 43.0 mm/year,mm/year,Annual,climate reconstruction,51 year filter,Statistical model,N,Relationship based on correlation with Instrumental records 1911-2000
NA; paleoData_summaryStatistic has been standardized
NA; paleoData_isPrimary has been standardized
Ratio between reflectance at 660 and 670 nm wavelength - degree of diagenesis,Gretag-Spectrolino,N,Relationship based on correlation with Instrumental records 1911-2000
originalDataUrl: 'https://www.ncdc.noaa.gov/paleo/study/22416' has been replaced by 'https://doi.org/10.25921/hkmx-k527'
originalDataUrl: 'https://www.ncei.noaa.gov/access/paleo-search/study/22416' has been replaced by 'https://www.ncdc.noaa.gov/paleo/study/22416'
precipitation (WEBb3fd19e6): interpretation1_variableDetail: 'precipitation@surface' has been replaced by 'amount@surface'
precipitation (WEBb3fd19e6): paleoData_notes: '((( "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380���730 nm) and instrumental precipitation record (1912���2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100���2800 cal yr BP, wet conditions from ca. 2800���2400 cal yr BP, dry conditions from ca. 2400���2000 calyr B"; paleoData_variableName updated; paleoData_summaryStatistic has been standardized; paleoData_units updated ))) "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized /// "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized' has been replaced by '"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized'
precipitation (WEBb3fd19e6): paleoData_notes: '"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized' has been replaced by '((( "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380���730 nm) and instrumental precipitation record (1912���2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100���2800 cal yr BP, wet conditions from ca. 2800���2400 cal yr BP, dry conditions from ca. 2400���2000 calyr B"; paleoData_variableName updated; paleoData_summaryStatistic has been standardized; paleoData_units updated ))) "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized /// "the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized'
Updated lipdverse database entry with a changed file.
geo_elevation: '' has been replaced by '8'
age (WEB10e844f9): paleoData_datum: '' has been replaced by '1950'
age (WEB10e844f9): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (WEB10e844f9): paleoData_units: 'BP' has been replaced by 'yr BP'
age (WEB10e844f9): paleoData_isPrimary: '' has been replaced by 'TRUE'
depth (WEB1fd237c5): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
depth (WEB1fd237c5): paleoData_isPrimary: '' has been replaced by 'TRUE'
year (WEB426560af): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized'
year (WEB426560af): paleoData_units: 'AD' has been replaced by 'yr AD'
year (WEB426560af): paleoData_variableName: 'age_CE' has been replaced by 'year'
year (WEB426560af): paleoData_isPrimary: '' has been replaced by 'FALSE'
precipitation (WEBb3fd19e6): paleoData_notes: '"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"' has been replaced by '"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"; paleoData_summaryStatistic has been standardized'
precipitation (WEBb3fd19e6): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
precipitation (WEBb3fd19e6): paleoData_variableName: 'precip5yr' has been replaced by 'precipitation'
precipitation (WEBb3fd19e6): paleoData_summaryStatistic: '' has been replaced by '5 year average'
age (WEBc942e4aa): paleoData_datum: '' has been replaced by '1950'
age (WEBc942e4aa): paleoData_notes: '' has been replaced by 'NA; paleoData_isPrimary has been standardized; paleoData_datum has been standardized'
age (WEBc942e4aa): paleoData_units: 'BP' has been replaced by 'yr BP'
age (WEBc942e4aa): paleoData_isPrimary: '' has been replaced by 'TRUE'
precipitation (WEBde2fb2ab): paleoData_notes: '' has been replaced by 'NA; paleoData_summaryStatistic has been standardized'
precipitation (WEBde2fb2ab): paleoData_units: 'mm/a' has been replaced by 'mm/yr'
precipitation (WEBde2fb2ab): paleoData_variableName: 'precip51yr' has been replaced by 'precipitation'
precipitation (WEBde2fb2ab): paleoData_summaryStatistic: '' has been replaced by '51 year average'
reflectance (WEBfea4f498): paleoData_units: 'R660_670' has been replaced by 'ratio'
precipitation (WEBb3fd19e6): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
precipitation (WEBb3fd19e6): interpretation1_variable: 'P' has been replaced by 'precipitation'
precipitation (WEBde2fb2ab): interpretation1_seasonality: '1,2,3,4,5,6,7,8,9,10,11,12' has been replaced by 'Annual'
precipitation (WEBde2fb2ab): interpretation1_variable: 'P' has been replaced by 'precipitation'
geo_elevation: '8' has been replaced by ''
originalDataUrl: '' has been replaced by 'https://www.ncei.noaa.gov/access/paleo-search/study/22416'
geo_gcmdLocation: '' has been replaced by 'Australia/New Zealand>Australia'
precip5yr (WEBb3fd19e6): paleoData_datum: '' has been replaced by 'abs'
precip5yr (WEBb3fd19e6): paleoData_notes: '' has been replaced by '"the relationship between scanning reflectance spectroscopy measurements of sediment cores in the visible spectrum (380–730 nm) and instrumental precipitation record (1912–2009) was used to develop a model to reconstruct precipitation back in time...Second, this calibration-in-time model was used to reconstruct late Holocene precipitation changes over the last ~3000 years. This showed relatively dry conditions from ca. 3100–2800 cal yr BP, wet conditions from ca. 2800–2400 cal yr BP, dry conditions from ca. 2400–2000 calyr B"'
precip5yr (WEBb3fd19e6): paleoData_proxyGeneral: '' has been replaced by 'biophysical'
precip5yr (WEBb3fd19e6): paleoData_QCCertification: '' has been replaced by 'CH'
precip5yr (WEBb3fd19e6): paleoData_QCnotes: '' has been replaced by 'Length < 4000yrs but in region of limited coverage'
precip51yr (WEBde2fb2ab): paleoData_proxyGeneral: '' has been replaced by 'biophysical'
precip5yr (WEBb3fd19e6): interpretation1_seasonalityGeneral: '' has been replaced by 'Annual'
reflectance (WEBfea4f498): interpretation1_scope: '' has been replaced by 'climate'
age (WEB10e844f9): paleoData_units: 'cal yr BP' has been replaced by 'BP'
age (WEB10e844f9): paleoData_unitsOriginal: '' has been replaced by 'cal yr BP'
age_CE (WEB426560af): paleoData_units: 'CE' has been replaced by 'AD'
age_CE (WEB426560af): paleoData_unitsOriginal: '' has been replaced by 'CE'
precip5yr (WEBb3fd19e6): paleoData_proxy: 'Reflectance' has been replaced by 'reflectance'
precip5yr (WEBb3fd19e6): paleoData_proxyLumps: '' has been replaced by 'biophysical'
precip5yr (WEBb3fd19e6): paleoData_proxyLumpsOriginal: '' has been replaced by 'reflectance'
precip5yr (WEBb3fd19e6): paleoData_proxyOriginal: '' has been replaced by 'Reflectance'
age (WEBc942e4aa): paleoData_units: 'cal yr BP' has been replaced by 'BP'
age (WEBc942e4aa): paleoData_unitsOriginal: '' has been replaced by 'cal yr BP'
precip51yr (WEBde2fb2ab): paleoData_proxy: 'Reflectance' has been replaced by 'reflectance'
precip51yr (WEBde2fb2ab): paleoData_proxyLumps: '' has been replaced by 'biophysical'
precip51yr (WEBde2fb2ab): paleoData_proxyLumpsOriginal: '' has been replaced by 'reflectance'
precip51yr (WEBde2fb2ab): paleoData_proxyOriginal: '' has been replaced by 'Reflectance'
precip5yr (WEBb3fd19e6): interpretation1_variableGroup: '' has been replaced by 'P'
precip51yr (WEBde2fb2ab): interpretation1_variableGroup: '' has been replaced by 'P'
reflectance (WEBfea4f498): interpretation1_scope: 'climate' has been replaced by ''
pub1_author: 'list(list(name = "Saunders, K.M."), list(name = "Kamenik, C."), list(name = "Hodgson, D.A."), list(name = "Hunziker, S."), list(name = "Siffert, L."), list(name = "Fischer, D."), list(name = "Fujak, M."), list(name = "Gibson, J.A.E."), list(name = "Grosjean, M."))' has been replaced by 'Saunders, K.M.'
Late Holocene changes in precipitation in northwest Tasmania and their potential links to shifts in the Southern Hemisphere westerly winds