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Journal Article
J. P. Briner, Young, ásE., Goehring, B. M., and Schaefer, J. M., Constraining Holocene 10Be production rates in Greenland, Journal of Quaternary Science, vol. 27, no. 1, pp. 2 - 6, 2012.
J. P. Briner, åkansson, L., and Bennike, O., The deglaciation and neoglaciation of Upernavik Isstrøm, Greenland, Quaternary Research, vol. 80, no. 03, pp. 459 - 467, 2013.
A. D. Schweinsberg, Briner, J. P., Miller, G. H., Lifton, N. A., Bennike, O., and Graham, B. L., Holocene mountain glacier history in the Sukkertoppen Iskappe area, southwest Greenland, Quaternary Science Reviews, vol. 197, pp. 142 - 161, 2018.
Y. Axford, Losee, S., Briner, J. P., Francis, D. R., Langdon, P. G., and Walker, I. R., Holocene temperature history at the western Greenland Ice Sheet margin reconstructed from lake sediments, Quaternary Science Reviews, vol. 59, pp. 87 - 100, 2013.
S. A. M. U. E. L. E. KELLEY, Briner, J. P., and ZIMMERMAN, S. U. S. A. N. R. H., The influence of ice marginal setting on early Holocene retreat rates in central West Greenland, Journal of Quaternary Science, vol. 30, no. 3, pp. 271 - 280, 2015.
A. D. Schweinsberg, Briner, J. P., Miller, G. H., Bennike, O., and Thomas, E. K., Local glaciation in West Greenland linked to North Atlantic Ocean circulation during the Holocene, Geology, vol. 45, no. 3, pp. 195 - 198, 2017.
E. K. Thomas, Briner, J. P., Ryan-Henry, J. J., and Huang, Y., A major increase in winter snowfall during the middle Holocene on western Greenland caused by reduced sea ice in Baffin Bay and the Labrador Sea, Geophysical Research Letters, vol. 45, no. 3, pp. 5302 - 5308, 2016.
A. D. Schweinsberg, Briner, J. P., Licciardi, J. M., Bennike, O., Lifton, N. A., Graham, B. L., Young, N. E., Schaefer, J. M., and Zimmerman, S. H., Multiple independent records of local glacier variability on Nuussuaq, West Greenland, during the Holocene, Quaternary Science Reviews, vol. 215, pp. 253 - 271, 2019.
ásE. Young, Briner, J. P., Axford, Y., Csatho, B., Babonis, G. S., Rood, D. H., and Finkel, R. C., Response of a marine-terminating Greenland outlet glacier to abrupt cooling 8200 and 9300 years ago, Geophysical Research Letters, vol. 38, no. 24, p. n/a - n/a, 2011.