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Articles | Volume 15, issue 5
https://doi.org/10.5194/tc-15-2251-2021
https://doi.org/10.5194/tc-15-2251-2021
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17 May 2021
Comment/reply | Highlight paper |  | 17 May 2021

Comment on “Exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream” by Smith-Johnsen et al. (2020)

Paul D. Bons, Tamara de Riese, Steven Franke, Maria-Gema Llorens, Till Sachau, Nicolas Stoll, Ilka Weikusat, Julien Westhoff, and Yu Zhang

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Cited articles

Artemieva, I. M.: Lithosphere thermal thickness and geothermal heat flux in Greenland from a new thermal isostasy method, Earth-Scie. Rev., 188, 469–481, https://doi.org/10.1016/j.earscirev.2018.10.015, 2019. 
Aschwanden, A., Fahnestock, M., and Truffer, M.: Complex Greenland outlet glacier flow captured, Nat. Com., 7, 10524, https://doi.org/10.1038/ncomms10524, 2016. 
Bartels, A., Nilsson, M. K. M., Klausen, M. B., and Söderlund, U.: Mesoproterozoic dykes in the Timmiarmiit area, Southeast Greenland: evidence for a continuous Gardar dyke swarm across Greenland's North Atlantic Craton, GFF, 138, 255–275, https://doi.org/10.1080/11035897.2015.1125386, 2016. 
Blackwell, D. D. and Richards, M.: Geothermal Map of North America, AAPG Map, scale 1 : 6 500 000, 2004. 
Bons, P. D.: The formation of large quartz veins by rapid ascent of fluids in mobile hydrofractures, Tectonophys., 336, 1–17, https://doi.org/10.1016/S0040-1951(01)00090-7, 2001. 
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The modelling of Smith-Johnson et al. (The Cryosphere, 14, 841–854, 2020) suggests that a very...