Extended Data Fig. 5: Time-series analysis algorithm tests. | Nature

Extended Data Fig. 5: Time-series analysis algorithm tests.

From: Antarctic icebergs reorganize ocean circulation during Pleistocene glacials

Extended Data Fig. 5

a, b, Testing the peak-lag algorithm to detect relationships in a series of surrogate time series with known lags applied. The ‘actual lag’ axes represent the known lag time imposed between pairs of the surrogate series and the ‘calculated lag’ axes show the lag estimated by the algorithm. A perfect performance would manifest as a 1:1 straight line through the scatter points. In b, the violin plots show the mean, median and kernel probability-density estimates of calculated lags from 104 iterations of the test. c, Results of the ‘glacial accumulation’ algorithm with each shaded curve representing IRDMAR (green) and δ18Obenthic (purple) integrated and normalized to 100% within each glacial cycle. Above, the δ18Obenthic record is shown (purple solid line) with green triangles denoting the peak interglacials identified and the dashed black line showing the δ18Obenthic threshold above which the transitions from glacial to interglacial conditions are defined. d, Gaussian kernel-based cross-correlation (gXCF)86 function for APcomp IRDMAR versus δ13Obenthic and δ13Cbenthic. The horizontal lines show the 95% Monte Carlo confidence levels for significant cross-correlation.

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