R: Temperature anomalies from δ15N fitting using the Schwander et al. (1997) firn model with the three accumulation rate scenarios (dataset Q)

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• Holocene temperature anomalies (0.07...11.5 kyr b2k) of Greenland Summit from firn model inversions of GISP2 δ15N, δ40Ar and δ15Nexcess data and GISP2 accumulation rates (0.02...35kyr b2k)
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