Publications

[12] Keisling B.A., Schaefer J.M., DeConto R.M., Briner J.P., Young N.E., Walcott-George C.K., Winckler G., Balter-Kennedy A., Anandakrishnan S., An ice-sheet modelling framework to determine vulnerable regions of the Greenland Ice Sheet in the past. The Cryosphere, 20, 2961–2976.
[11] Walcott-George C.K., Brown N.D., Briner J.P., Balter-Kennedy A., Young N.E., Kuhl T., Moravec E., Anandakrishnan S., Stevens N.T., Keisling B., et al., Deglaciation of the Prudhoe Dome in northwestern Greenland in response to Holocene warming. Nature Geoscience, 1–6.

[10] Anderson J.T., Young N.E., Balter-Kennedy A., Prince K.K., Walcott-George C.K., Graham B.L., Charton J., Briner J.P., Schaefer J.M., East Greenland Ice Sheet retreat history from Scoresby Sund and Storstrømmen Glacier during the last deglaciation. Climate of the Past, 21, 2263–2281.
[9] Bromley G.R., Balco G., Jackson M.S., Balter-Kennedy A., Thomas H., East Antarctic Ice Sheet variability in the central Transantarctic Mountains since the mid Miocene. Climate of the Past, 21, 145–160.
[8] Walcott-George C.K., Balter-Kennedy A., Briner J.P., Schaefer J.M., Young N.E., Glacial erosion and history of Inglefield Land, northwestern Greenland. The Cryosphere, 19, 2067–2086.

[7] Balter-Kennedy A., Schaefer J.M., Balco G., Kelly M.A., Kaplan M.R., Schwartz R., Oakley B., Young N.E., Hanley J., Varuolo-Clarke A.M., The Laurentide Ice Sheet in southern New England and New York during and at the end of the Last Glacial Maximum: a cosmogenic-nuclide chronology. Climate of the Past, 20, 2167–2190.

[6] Balter-Kennedy A., Schaefer J.M., Schwartz R., Lamp J.L., Penrose L., Middleton J., Hanley J., Tibari B., Blard P., Winckler G., et al., Cosmogenic ¹⁰Be in pyroxene: laboratory progress, production rate systematics, and application of the ¹⁰Be-³He nuclide pair in the Antarctic Dry Valleys. Geochronology, 5, 301–321.
[5] Bromley G., Putnam A., Hall B., Rademaker K., Thomas H., Balter-Kennedy A., Barker S., Rice D., Lateglacial shifts in seasonality reconcile conflicting North Atlantic temperature signals. Journal of Geophysical Research: Earth Surface, 128, e2022JF006951.
[4] Graham B.L., Briner J.P., Young N.E., Balter-Kennedy A., Koppes M., Schaefer J.M., Poinar K., Thomas E.K., In situ ¹⁰Be modeling and terrain analysis constrain subglacial quarrying and abrasion rates at Sermeq Kujalleq (Jakobshavn Isbrae), Greenland. The Cryosphere, 17, 4535–4547.

[3] Balter-Kennedy A., Young N., Briner J., Graham B., Schaefer J., Centennial-and orbital-scale erosion beneath the Greenland ice sheet near Jakobshavn Isbrae. Journal of Geophysical Research: Earth Surface, 126, e2021JF006429.
[2] Young N.E., Lesnek A.J., Cuzzone J.K., Briner J.P., Badgeley J.A., Balter-Kennedy A., Graham B.L., Cluett A., Lamp J.L., Schwartz R., et al., In situ cosmogenic ¹⁰Be-¹⁴C-²⁶Al measurements from recently deglaciated bedrock as a new tool to decipher changes in Greenland Ice Sheet size. Climate of the Past, 17, 419–450.

[1] Balter-Kennedy A., Bromley G., Balco G., Thomas H., Jackson M.S., A 14.5-million-year record of East Antarctic Ice Sheet fluctuations from the central Transantarctic Mountains, constrained with cosmogenic ³He, ¹⁰Be, ²¹Ne, and ²⁶Al. The Cryosphere, 14, 2647–2672.