Published in academic journals:
*Starred names are supervised undergraduate or graduate students
Published in academic journals:
*Starred names are supervised undergraduate or graduate students
[10] *Allen, H.T., Kaufman, D.S., McKay, N.P., Schiefer, E.B., Larocca, L.J., Jensen, B.J., Bolton, M.S., North, K., Praet, N., Van Daele, M., De Batist, M., and Żarczyński, M. 2026. Holocene glacier fluctuations at Eklutna Lake, Chugach Mountains, south-central Alaska. Quaternary Science Reviews, 390, p.110107.
[9] Larocca, L. J., Kaufman, D. S., Erb, M. P., *Schultz, T. M., McKay, N. P., Brooks, J. P., & Carrivick, J. L. 2026. Glacier equilibrium-line altitude change across Alaska and adjacent Canada indicates a cold, dry little ice age and weaker Aleutian low. Geophysical Research Letters, 53, e2025GL119840.
[6] Larocca, L.J., Twinning-Ward, M., Axford, Y., Schweinsberg, A., Larsen, S.H., Westergaard-Nielsen, A., Luetzenburg, G., Briner, J.P., Kjeldssen, K.K., and Bjørk, A.A. 2023. Greenland-wide accelerated retreat of peripheral glaciers in the twenty-first century. Nature Climate Change 13, 1324-1328.
[3] Larocca, L.J., Axford, Y., Woodroffe, S.A., Lasher, G.E, and Gawin, B. 2020. Holocene glacier and ice cap fluctuations in southwest Greenland inferred from two lake records. Quaternary Science Reviews, 246, p.106529.
[2] Larocca, L.J., Axford, Y., Bjørk, A., Lasher, G.E., and *Brooks, J.P. 2020. Local glaciers record delayed peak Holocene warmth in South Greenland. Quaternary Science Reviews, 241, p.106421.
[1] Lasher, G.E., Axford, Y., Masterson, A.L., Berman, K. and Larocca, L.J. 2020. Holocene temperature and landscape history of southwest Greenland inferred from isotope and geochemical lake sediment proxies. Quaternary Science Reviews, 239, p.106358.
In review:
*Starred names are supervised undergraduate or graduate students
[2] Lamantia, K.A., Larocca, L.J., Aberle, R., Lea, J.M. A Google Earth Engine tool for mapping key metrics of glacier health from space.
[1] Peng, C., Tan, S., Rouillard, A., and others. Post-glacial soil development shapes microbial succession and warming-sensitive carbon release across Greenland.