# Corrigendum to "Influence of ablation-related processes in the build-up of simulated Northern Hemisphere ice sheets during the last glacial cycle" published in The Cryosphere, 7, 681-698, 2013

S. Charbit, C. Dumas, M. Kageyama, D. M. Roche, C. Ritz

► To cite this version:

S. Charbit, C. Dumas, M. Kageyama, D. M. Roche, C. Ritz. Corrigendum to "Influence of ablation-related processes in the build-up of simulated Northern Hemisphere ice sheets during the last glacial cycle" published in The Cryosphere, 7, 681-698, 2013. The Cryosphere, 2013, 7, pp.933-934. 10.5194/tc-7-933-2013. hal-04114071

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Submitted on 2 Jun 2023

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Corrigendum to

“Influence of ablation-related processes in the build-up of simulated
Northern Hemisphere ice sheets during the last glacial cycle”
published in The Cryosphere, 7, 681–698, 2013

S. Charbit<fnref n="1" />, C. Dumas<fnref n="1" />, M. Kageyama<fnref n="1" />, D. M. Roche<fnref n="1" />, and C. Ritz<fnref n="2" />

Correspondence to: S. Charbit (sylvie.charbit@lsce.ipsl.fr)

We regret to have found errors in our manuscript entitled “In-
fluence of ablation-related processes in the build-up of simu-
lated Northern Hemisphere ice sheets during the last glacial
cycle” (The Cryosphere, 7, 681–698, doi:10.5194/tc-7-681-
2013, 2013), in Fig. 1, Fig. 6 caption and in the list of refer-
ences.

In Fig. 1, the top and bottom panels have been inverted.
The corrected figure is on the next page.

The corrected caption of Fig. 6 is the following:

"Simulated ice thickness difference (in meters) when substituting the TP02 refreezing scheme in the FST09 model (top panels: FST09 with TP02 refreezing – FST09; run 24) and when allowing the FST09 model a fixed portion (i.e. Pmax = 60 %) of meltwater to produce superimposed ice (bottom panels: FST09 with RH91 refreezing – FST09; run 25). Left panels refer to the 115 ka period and right panels refer to the LGM (i.e. 21 ka). The thick black lines represent the contour of the continents and thin ones display the isocontours of surface elevation (from 1000 to 5000 m).

The exact reference for Braithwaite (1984) is:

References

Braithwaithe, R. J.: Calculation of degree-days for glacier-climate research, Zeitschrift für Gletscherkunde und Glazialgeologie, 20, 1–8, 1984.

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The publication of this article
is financed by CNRS-INSU.

<footnote n="1">¹IPSL/Laboratoire des sciences du climat et de l'environnement, UMR CEA-CNRS-UVSQ 8212, CE Saclay,
Orme des Merisiers, Bât. 701, 91191 Gif-sur-Yvette cedex, France</footnote>

<footnote n="2">²UJF – Grenoble 1/CNRS, Laboratoire de glaciologie et de géophysique de l'environnement, UMR 5183,
Grenoble, 38041, France</footnote>
<figure><img src="image_5.png" /><figcaption>**Fig. 1.** Simulated ice thickness (in meters) at 116 ka (left panels) and 21 ka (right panels) produced by the three standard fully coupled experiments with the RH91 (run 1, top panels), TP02 (run 2, middle) and FST09 (run 3, bottom) PDD models. Thick black lines represent the coastline and thin black lines display the iso-contours of surface elevation (from 1000 to 5000 m). The thick red lines in the right panels represent the areal extent of the ICE-5G LGM ice sheets (Peltier, 2004).</figcaption></figure>