G. Milne

Bassett, S. ., Milne, G. A., Mitrovica, J. ., & Clark, P. . (2005). Ice Sheet and Solid Earth Influences on Far-Field Sea-Level Histories. Science, 309, 925–928. http://doi.org/10.1126/science.1111575 (Original work published August 2005)

Wake, L. ., Milne, G. A., & Leuliette, E. W. (2006). 20th Century sea-level change along the eastern US: Unravelling the contributions from steric changes, Greenland ice sheet mass balance and Late Pleistocene glacial loading. Earth and Planetary Science Letters, 250, 572–580. http://doi.org/10.1016/j.epsl.2006.08.006 (Original work published October 2006)

Bassett, S. ., Milne, G. A., Bentley, M. ., & Huybrechts, P. . (2007). Modelling Antarctic sea-level data to explore the possibility of a dominant Antarctic contribution to meltwater pulse IA. Quaternary Science Reviews, 26, 2113–2127. http://doi.org/10.1016/j.quascirev.2007.06.011 (Original work published September 2007)

Milne, G. A., & Mitrovica, J. . (2008). Searching for eustasy in deglacial sea-level histories. Quaternary Science Reviews, 27, 2292–2302. http://doi.org/10.1016/j.quascirev.2008.08.018 (Original work published December 2008)

Edwards, R. ., Brooks, A. ., Shennan, I. ., Milne, G. A., & Bradley, S. . (2008). Reply: Postglacial relative sea-level observations from Ireland and their role in glacial rebound modelling. Journal of Quaternary Science, 23, 821–825. http://doi.org/10.1002/jqs.1162 (Original work published December 2008)

Long, A. J., Woodroffe, S. A., Milne, G. A., Bryant, C. ., & Wake, L. M. (2010). Relative sea level change in west Greenland during the last millennium. Quaternary Science Reviews, 29, 367–383. http://doi.org/10.1016/j.quascirev.2009.09.010 (Original work published February 2010)

Milne, G. A., Gehrels, W. R., Hughes, C. W., & Tamisiea, M. . (2009). Identifying the causes of sea-level change. Nature Geoscience, 2, 471–478. http://doi.org/10.1038/ngeo544 (Original work published July 2009)

Simpson, M. J. R., Milne, G. A., Huybrechts, P. ., & Long, A. J. (2009). Calibrating a glaciological model of the Greenland ice sheet from the Last Glacial Maximum to present-day using field observations of relative sea level and ice extent. Quaternary Science Reviews, 28, 1631–1657. http://doi.org/10.1016/j.quascirev.2009.03.004 (Original work published August 2009)