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Köhler, Peter; van de Wal, Roderik S W (2020): Northern hemispheric land ice distribution outside of Greenland during the Quaternary [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.914483

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Abstract:
From the combination of orbital theory with benthic δ18O it has been suggested which obliquity cycles led to interglacials during the Quaternary. Here, we use a model-based deconvolution of this benthic δ18O record to calculate northern hemispheric land ice outside of Greenland, from which an alternative distribution of glacial and interglacial periods is defined.
Model output is compared with independent reconstructions of δ18O_seawater, sea level and atmospheric CO2 concentrations.
All data plotted in the figures of the article:
Köhler, P. & van de Wal, R. S. W. Interglacials of the Quaternary defined by northern hemispheric land ice distribution outside of Greenland, Nature Communications, 2020, 11, 5124, doi:10.1038/s41467-020-18897-5.
are compiled here.
Keyword(s):
benthic δ18O; land ice volume; Model; Quaternary
Supplement to:
Köhler, Peter; van de Wal, Roderik S W (2020): Interglacials of the Quaternary defined by northern hemispheric land ice distribution outside of Greenland. Nature Communications, 11, 5124, https://doi.org/10.1038/s41467-020-18897-5
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
File contentContentKöhler, Peter
File nameFile nameKöhler, Peter
File formatFile formatKöhler, Peter
File sizeFile sizekByteKöhler, Peter
Uniform resource locator/link to fileURL fileKöhler, Peter
Size:
165 data points

Data

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fig1a datafig1a__obliquity_2600kyr_withheaderDAT25.203fig1a__obliquity_2600kyr_withheader.dat
fig1b datafig1b__lr04d18Ostack_2600kyr_withheaderDAT31.677fig1b__lr04d18Ostack_2600kyr_withheader.dat
fig2a1 datafig2a1_onset_ig_ctrl_withheaderDAT0.797fig2a1_onset_ig_ctrl_withheader.dat
fig2a2 datafig2a2_skipped_terminations_withheaderDAT0.349fig2a2_skipped_terminations_withheader.dat
fig2a datafig2a__delta_icevol_nam_eur_2600kyr_withheaderDAT18.223fig2a__delta_icevol_nam_eur_2600kyr_withheader.dat
fig2b datafig2b__latitude_icevol_nam_eur_2600kyr_withheaderDAT75.595fig2b__latitude_icevol_nam_eur_2600kyr_withheader.dat
fig2c1 datafig2c1__fraction_icevol_nam_eur__global_2600kyr_withheaderDAT22.328fig2c1__fraction_icevol_nam_eur__global_2600kyr_withheader.dat
fig2c2 datafig2c2__fraction_icevol_nam_eur__global_2600kyr_runnmean_41k_withheaderDAT21.954fig2c2__fraction_icevol_nam_eur__global_2600kyr_runnmean_41k_withheader.dat
fig2d1 datafig2d1__ratio_d18Osw_d18Ob_runnmean_2k_2600kyr_withheaderDAT454.845fig2d1__ratio_d18Osw_d18Ob_runnmean_2k_2600kyr_withheader.dat
fig2d2 datafig2d2__ratio_d18Osw_d18Ob_runnmean_41k_2600kyr_withheaderDAT451.609fig2d2__ratio_d18Osw_d18Ob_runnmean_41k_2600kyr_withheader.dat
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fig3bo datafig3b_onset_ig_v2_withheaderDAT0.764fig3b_onset_ig_v2_withheader.dat
fig3co datafig3c_onset_ig_v3_withheaderDAT0.775fig3c_onset_ig_v3_withheader.dat
fig4a datafig4a__delta_icevol_nam_eur_2600kyr_withheaderDAT18.223fig4a__delta_icevol_nam_eur_2600kyr_withheader.dat
fig4b datafig4b__lr04d18Ostack_detrendlr04_2600kyr_withheaderDAT47.515fig4b__lr04d18Ostack_detrendlr04_2600kyr_withheader.dat
fig4c1 datafig4c1__sealevel_deboer2014nc_2600kyr_withheaderDAT17.461fig4c1__sealevel_deboer2014nc_2600kyr_withheader.dat
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fig4e6 datafig4e6__drco2_paleosol_2600kyr_withheaderDAT2.583fig4e6__drco2_paleosol_2600kyr_withheader.dat
fig4e7 datafig4e7__drco2_simulations_2600kyr_withheaderDAT43.631fig4e7__drco2_simulations_2600kyr_withheader.dat
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fig5b2 datafig5b2__normalized__lr04d18Ostack_detrendendlr04_2600kyr_runnmean_41k_withheaderDAT35.894fig5b2__normalized__lr04d18Ostack_detrendendlr04_2600kyr_runnmean_41k_withheader.dat
fig5b3 datafig5b3_glacial_index_2600kyr_runnmean_41k_withheaderDAT38.823fig5b3_glacial_index_2600kyr_runnmean_41k_withheader.dat