# North American Hydroclimate Synthesis (NAHS) from multi-proxy hydroclimate records over the Common Era #----------------------------------------------------------------------- # World Data Service for Paleoclimatology, Boulder # and # NOAA Paleoclimatology Program #----------------------------------------------------------------------- # Template Version 3.0 # Encoding: UTF-8 # NOTE: Please cite original publication, online resource and date accessed when using this data. # If there is no publication information, please cite Investigator, title, online resource and date accessed. # # Description/Documentation lines begin with # # Data lines have no # # # Online_Resource: https://www.ncdc.noaa.gov/paleo/study/24910 # Description: NOAA Landing Page # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/reconstructions/rodysill2018/rodysill2018-fig13.txt # Description: NOAA location of the template # Online_Resource: http://www1.ncdc.noaa.gov/pub/data/paleo/reconstructions/rodysill2018/rodysill2018-RecordsUsed_Metadata.txt # Description: NOAA location of the Records Used metadata template # # Archive: Climate Reconstructions # # Dataset_DOI: # # Parameter_Keywords: precipitation #--------------------------------------- # Contribution_Date # Date: 2018-08-20 #--------------------------------------- # File_Last_Modified_Date # Date: 2018-08-20 #--------------------------------------- # Title # Study_Name: North American Hydroclimate Synthesis (NAHS) from multi-proxy hydroclimate records over the Common Era #--------------------------------------- # Investigators # Investigators: Rodysill, Jessica R.; Anderson, Lesleigh; Cronin, Thomas M.; Jones, Miriam C.; Thompson, Robert S.; Wahl, David B.; Willard, Debra A.; Addison, Jason A.; Alder, Jay R.; Anderson, Katherine H.; Anderson, Lysanna; Barron, John A.; Bernhardt, Christopher E.; Hostetler, Steven W.; Kehrwald, Natalie M.; Khan, Nicole S.; Richey, Julie N.; Starratt, Scott W.; Strickland, Laura E.; Toomey, Michael R.; Treat, Claire C.; Wingard, G. Lynn #--------------------------------------- # Description_Notes_and_Keywords # Description: North American multi-proxy hydroclimate records are synthesized with new chronologies. Hydroclimate reconstructions document clear regional trends during the Common Era. Regionally asynchronous spatial variability occurred at centennial timescales. Widespread North American drought coincided with warm N. Hemisphere temperatures. Wet and dry climates occurred during both warm and cool climates. # Provided Keywords: precipitation, ground water, lake level, salinity, vegetation, lake salinity #--------------------------------------- # Publication # Authors: Rodysill, Jessica R.; Anderson, Lesleigh; Cronin, Thomas M.; Jones, Miriam C.; Thompson, Robert S.; Wahl, David B.; Willard, Debra A.; Addison, Jason A.; Alder, Jay R.; Anderson, Katherine H.; Anderson, Lysanna; Barron, John A.; Bernhardt, Christopher E.; Hostetler, Steven W.; Kehrwald, Natalie M.; Khan, Nicole S.; Richey, Julie N.; Starratt, Scott W.; Strickland, Laura E.; Toomey, Michael R.; Treat, Claire C.; Wingard, G. Lynn # Published_Date_or_Year: 2018 # Published_Title: A North American Hydroclimate Synthesis (NAHS) of the Common Era # Journal_Name: Global and Planetary Change # Volume: 162 # Edition: # Issue: # Pages: 175-198 # Report_Number: # DOI: 10.1016/j.gloplacha.2017.12.025 # Online_Resource: www.sciencedirect.com/science/article/pii/S0921818117304174 # Full_Citation: # Abstract: This study presents a synthesis of century-scale hydroclimate variations in North America for the Common Era (last 2000 years) using new age models of previously published multiple proxy-based paleoclimate data. This North American Hydroclimate Synthesis (NAHS) examines regional hydroclimate patterns and related environmental indicators, including vegetation, lake water elevation, stream flow and runoff, cave drip rates, biological productivity, assemblages of living organisms, and salinity. Centennial-scale hydroclimate anomalies are obtained by iteratively sampling the proxy data on each of thousands of age model realizations and determining the fractions of possible time series indicating that the century-smoothed data was anomalously wet or dry relative to the 100 BCE to 1900 CE mean. Results suggest regionally asynchronous wet and dry periods over multidecadal to centennial timescales and frequent periods of extended regional drought. Most sites indicate drying during previously documented multicentennial periods of warmer Northern Hemisphere temperatures, particularly in the western U.S., central U.S., and Canada. Two widespread droughts were documented by the NAHS: from 50 BCE to 450 CE and from 800 to 1100 CE. Major hydroclimate reorganizations occurred out of sync with Northern Hemisphere temperature variations and widespread wet and dry anomalies occurred during both warm and cool periods. We present a broad assessment of paleoclimate relationships that highlights the potential influences of internal variability and external forcing and supports a prominent role for Pacific and Atlantic Ocean dynamics on century-scale continental hydroclimate. #--------------------------------------- # Funding_Agency # Funding_Agency_Name: U.S. Geological Survey Climate and Land Use Change Research and Development Program # Grant: #--------------------------------------- # Site_Information # Site_Name: North America # Location: North America # Country: United States, Canada, Mexico # Northernmost_Latitude: 74.89164 # Southernmost_Latitude: 17.4 # Easternmost_Longitude: -63.5392 # Westernmost_Longitude: -159.4316 # Elevation: #--------------------------------------- # Data_Collection # Collection_Name: NAHS 200yr fraction fig13 Rodysill2018 # First_Year: -100 # Last_Year: 1900 # Time_Unit: CE # Core_Length: # Notes: Data used for Figure 13. More information in publication- Methods Section 3.5 #--------------------------------------- # Chronology_Information # Chronology: #--------------------------------------- # Variables # Data variables follow that are preceded by "##" in columns one and two. # Variables list, one per line, shortname-tab-longname components (9 components: what, material, error, units, seasonality, archive, detail, method, C or N for Character or Numeric data) ## 200yr_window_start_CE age,,,year Common Era,,climate reconstructions,,,N,start year of 200-year bin ## 200yr_window_end_CE age,,,year Common Era,,climate reconstructions,,,N,end year of 200-year bin ## 1-AguadaXcaamal_d18O moisture index,gastropod,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 2-Baie_testate_amoeb_assemblage moisture index,testate amoebae assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a testate amoebae assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 3-BearLake_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage calculated across all age model iterations exported from Bacon; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 4-BlueLake_varve moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of varve thickness; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 5-BuckeyeCreekCave_d18O moisture index,calcium carbonate,,dimensionless,,speleothems; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 6-CastorLime_Dd18O moisture index,,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the difference between Castor Lake aragonite d18O (VPDB) and Lime Lake calcite d18O (VPDB); negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 7-ChesapeakeBay_MD03-2661_d18O moisture index,benthic foraminifera (Elphidium selseyense),,dimensionless,,paleoceanography; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 8-ChesapeakeBay_pollen_assemblage moisture index,,,dimensionless,,paleoceanography; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 9-ClelandLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 10-ColdwaterLake_salinity moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from salinity proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 11-CrystalCave_d18O moisture index,stalagmite,,dimensionless,,speleothems; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 12-DavisPond_lakelevel moisture index,lake level,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 13-DeepPond_lakelevel moisture index,lake level,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 14-DixieLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 15-DuneLake_d13C moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d13C proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 16-EastLake_grain size moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of particle diameter of 98th percentile of grain size distribution; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 17-ELALake239_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 18-ELALake442_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 19-ElkLake_%Al moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of aluminum abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 20-FoyLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 21-FoyLake_benthic_diatom_abundance moisture index,diatom,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of benthic diatom abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 22-GallLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 23-GreatHeath_SVR moisture index,peat n-alkanes,,dimensionless,,pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the ratio of Sphagnum to vascular plants; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 24-GreatSaltLake_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 25-HiddenLake_lake level moisture index,,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 26-HobartLake_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 27-HorsetrailFen_macrofossil_assemblage moisture index,,,dimensionless,,paleolimnology; plant macrofossils; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a plant macrofossil assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 28-IrwinSmithBog_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 29-JenningsCave_d13C moisture index,fulvic acid,,dimensionless,,speleothems; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d13C proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 30-JuxtlahuacaCave_d18O moisture index,stalagmite,,dimensionless,,speleothems; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 31-KecheLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 32-KirmanLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 32-KirmanLake_salinity moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred salinitie; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 33-KiteLake_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 34-LacLeCaron_plant macrofossil_assemblage moisture index,,,dimensionless,,paleolimnology; plant macrofossils; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a plant macrofossil assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 35-LagunadeAljojuca_%Al2O3 moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from aluminum oxide abundance by mass proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 35-LagunadeAljojuca_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 36-LagunadeJuanacatlan_Ti moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of titanium abundance normalized to incoherent peak area; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 37-LakeChichancanab_density moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of bulk density; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 38-LakeElsinore_%sand moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of sand abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 39-LakeoftheWoods_lakelevel moisture index,,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 40-Lebel_testate amoebae_assemblage moisture index,testate amoebae assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a testate amoebae assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 41-LittleRaleighLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 42-LowerBearLake_LOI950C moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from mass lost on ignition at 950°C proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 43-MarcellaJelly_Dd18O moisture index,Characean algae (Chara) encrustations,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the difference between Marcella Lake Chara d18O (VPDB) and Jellybean Lake carbonate d18O (VPDB); negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 44-MartinLake_lithics moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of lithic abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 44-MartinLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 45-MB01_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 46-MeekinLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 47-MindenBog_amoebae_tabledepth moisture index,testate amoebae assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from testate amoebae-inferred water table depth proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 48-MonoLake_lakelevel moisture index,,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 49-MoonLake_salinity moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of diatom-inferred salinity; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 50-Morts_testate amoebae_assemblage moisture index,testate amoebae assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a testate amoebae assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 51-NewLongPond_lakelevel moisture index,lake level,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from lake levels; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 52-OngokeLake_diatom_waterdepth moisture index,diatom assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from diatom-inferred water depth; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 53-OregonCaves_d13C moisture index,stalagmite,,dimensionless,,speleothems; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d13C proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 54-ParadiseLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 55-PathLake_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 56-Plaine_testate amoebae_assemblage moisture index,testate amoebae assemblage,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a testate amoebae assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 57-PuntaLaguna_d18O moisture index,ostracod,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 58-RiceLake_MgCa moisture index,ostracod,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from magnesium to calcium ratio proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 59-RoeIsland_d13C_salinity moisture index,delta 13C,,dimensionless,,paleoceanography; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from d13C-based salinity estimates; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 60-SchellingsBogSB70_%pseudotsuga moisture index,pollen,,dimensionless,,pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of Pseudotsuga menziesii abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 60-SchellingsBogSB70_%quercus moisture index,pollen,,dimensionless,,pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of Quercus chrysolepis abundance; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 61-Site4_pollen_assemblage moisture index,,,dimensionless,,paleolimnology; pollen; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a pollen assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 62-SouthBay_d13C-d18O_salinity moisture index,delta 13C; delta 18O,,dimensionless,,paleoceanography; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from d13C- and d18O-based salinity estimates; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 63-SteelLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 64-Sugluk_macrofossil_assemblage moisture index,,,dimensionless,,paleolimnology; plant macrofossils; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a plant macrofossil assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 65-UpperPinto_macrofossil_assemblage moisture index,,,dimensionless,,paleolimnology; plant macrofossils; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from an assemblage-based hydroclimate interpretation time series from a plant macrofossil assemblage; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 66-WalkerLake_d18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from d18O proxy data; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 67-WolverineLake_MineralMAR moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of mineral mass accumulation rate (recalculated after applying new Bacon age model); negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 68-YellowBison_Dd18O moisture index,carbonate,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the difference between Yellow Lake carbonate d18O (VPDB) and Bison Lake carbonate d18O (VPDB); negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 ## 69-ZacaLake_%coarse moisture index,sediment,,dimensionless,,paleolimnology; climate reconstructions,,,N,Fraction representing the difference between the number of chronologies indicating wet anomalies and the number of chronologies indicating dry anomalies relative to the total number of chronologies exported from Bacon in a given 200-year window. Hydroclimate interpretations are derived from the natural log of abundance of coarse particles with grain diameters between 125 microns and 2000 microns; negative: more chronologies indicate drier than average than wetter than average; positive: more chronologies indicate wetter than average than drier than average; Methods Section 3.5 #------------------------ # Data: # Data lines follow (have no #) # Data line format - tab-delimited text, variable short name as header # Missing_Values: 200yr_window_start_CE 200yr_window_end_CE 1-AguadaXcaamal_d18O 2-Baie_testate_amoeb_assemblage 3-BearLake_pollen_assemblage 4-BlueLake_varve 5-BuckeyeCreekCave_d18O 6-CastorLime_?d18O 7-ChesapeakeBay_MD03-2661_d18O 8-ChesapeakeBay_pollen_assemblage 9-ClelandLake_d18O 10-ColdwaterLake_salinity 11-CrystalCave_d18O 12-DavisPond_lakelevel 13-DeepPond_lakelevel 14-DixieLake_diatom_waterdepth 15-DuneLake_d13C 16-EastLake_grain size 17-ELALake239_diatom_waterdepth 18-ELALake442_diatom_waterdepth 19-ElkLake_%Al 20-FoyLake_d18O 21-FoyLake_benthic_diatom_abundance 22-GallLake_diatom_waterdepth 23-GreatHeath_SVR 24-GreatSaltLake_pollen_assemblage 25-HiddenLake_lake level 26-HobartLake_pollen_assemblage 27-HorsetrailFen_macrofossil_assemblage 28-IrwinSmithBog_pollen_assemblage 29-JenningsCave_d13C 30-JuxtlahuacaCave_d18O 31-KecheLake_d18O 32-KirmanLake_diatom_waterdepth 32-KirmanLake_salinity 33-KiteLake_pollen_assemblage 34-LacLeCaron_plant macrofossil_assemblage 35-LagunadeAljojuca_%Al2O3 35-LagunadeAljojuca_d18O 36-LagunadeJuanacatlan_Ti 37-LakeChichancanab_density 38-LakeElsinore_%sand 39-LakeoftheWoods_lakelevel 40-Lebel_testate amoebae_assemblage 41-LittleRaleighLake_diatom_waterdepth 42-LowerBearLake_LOI950C 43-MarcellaJelly_?d18O 44-MartinLake_lithics 44-MartinLake_d18O 45-MB01_pollen_assemblage 46-MeekinLake_diatom_waterdepth 47-MindenBog_amoebae_tabledepth 48-MonoLake_lakelevel 49-MoonLake_salinity 50-Morts_testate amoebae_assemblage 51-NewLongPond_lakelevel 52-OngokeLake_diatom_waterdepth 53-OregonCaves_d13C 54-ParadiseLake_d18O 55-PathLake_pollen_assemblage 56-Plaine_testate amoebae_assemblage 57-PuntaLaguna_d18O 58-RiceLake_MgCa 59-RoeIsland_d13C_salinity 60-SchellingsBogSB70_%pseudotsuga 60-SchellingsBogSB70_%quercus 61-Site4_pollen_assemblage 62-SouthBay_d13C-d18O_salinity 63-SteelLake_d18O 64-Sugluk_macrofossil_assemblage 65-UpperPinto_macrofossil_assemblage 66-WalkerLake_d18O 67-WolverineLake_MineralMAR 68-YellowBison_?d18O 69-ZacaLake_%coarse ZacaLake_CA_grainsize 100 300 0 -0.10869 -0.58938 1 -0.01238 0.024093 0.036386 -0.9999 -0.02476 -0.3462 -0.42959 -0.99983 0.837385 -0.001 0.363409 1 -0.68823 -0.01266 1 1 -1 -0.0584 -0.06987 0.915748 -0.77034 0.999832 -0.69276 0.501514 -0.06351 0.852283 -0.21075 0.323512 0.008505 -0.00066 -0.94776 0.007619 0.087619 -0.38889 0 -0.80097 -0.96862 -0.00478 0.048736 0.058074 0.034248 0.001252 0.026109 0.113337 0.001419 -0.12813 -0.63842 -0.13446 -1 -0.89119 -0.78485 0.572738 -0.00173 -0.0083 -1 0.159844 -0.09844 -0.23594 -0.42975 -0.57412 0 -0.91961 -0.645 1 0.568638 -0.48692 0.143858 -0.41291 -0.06897 500 700 0 0 -1 0.999 0.023357 -0.18648 -0.09398 -0.0001 0.10861 -0.00233 0.103684 -1 0.99646 0.121138 0.005639 -1 0.692627 0.579569 0.997 -1 0 0.010741 -0.10228 -1 -0.97628 1 0.960616 0.0185 0.453893 -0.15331 -0.54612 0.000304 0.313791 -0.27653 0.371015 0.018095 -0.33762 -0.02212 -0.02637 -0.1774 -0.9818 0 0.000524 -0.54065 -0.05211 0.067239 0.110873 0.794886 0.080613 0.472428 -0.01469 -0.89065 1 0.996143 -0.09068 -0.16524 0.278596 0.920463 -1 -0.78235 0.476738 -0.97487 0.112763 -0.05093 -0.06438 -0.76867 1 1 -1 0.031729 0.007184 0.000151 -0.19868 1000 1200 0.259349 0.9998 0.77015 -1 0.180234 0.365457 -0.18762 -0.97522 -0.21947 0.975612 0.515152 -1 0.999056 -0.99989 0.075188 0 0.015259 0.588153 0 0 0 -0.98 0.856182 -0.99706 -1 1 0.988503 -0.99529 0.735199 0 -0.00183 -0.80407 -0.88609 -0.99978 -0.10041 -0.99905 -1 -0.26524 -0.24143 -0.2887 0.677126 0 -0.92349 0.05133 -0.08617 -0.55204 -0.3083 -0.86033 -0.84956 -0.12392 -0.38627 0.454093 1 0.999196 0.569857 -0.22046 -0.724 0.981081 0.818463 -0.05475 0.148936 0.750299 -0.17013 0.006639 -0.98229 0.812544 0 0.04261 -1 0.631326 -0.95977 -0.00682 0.006598 1100 1300 0.198208 1 0.999712 -0.749 0.881123 0.315394 -0.45059 -0.78865 -0.10805 0.971901 0.310458 -1 0.99528 -0.997 0.224311 0 0.232788 0.980864 -0.869 0 0 -0.79481 0.941657 -0.84864 -1 0.988431 0.802348 -1 0.952817 0 0.018632 -0.78706 -0.76306 -1 0.999719 -0.96143 -0.99905 0.002458 -0.00293 -0.02333 0.999629 0 -0.7258 0.625703 0.124471 -0.84871 -0.75 -0.98836 -0.26213 -0.66373 -0.45086 0.865419 1 0.999679 0.4292 -0.00998 -0.44584 0.969305 0.999558 0.115239 -0.01374 -0.25054 0.005945 0.074118 -0.95934 -0.1577 -1 0.890948 -1 0.008048 -0.34896 -0.08467 0.011328