Maclennan ITGC:042
Maclennan, M. L. and J. T. M. Lenaerts. 2021. Large-Scale Atmospheric Drivers of Snowfall Over Thwaites Glacier, Antarctica. Geophysical Research Letters 48:17 e2021GL093644.
Maclennan, M. L. and J. T. M. Lenaerts. 2021. Large-Scale Atmospheric Drivers of Snowfall Over Thwaites Glacier, Antarctica. Geophysical Research Letters 48:17 e2021GL093644.
Eayrs, C., Li, X., Raphael, M.N. et al. 2021. Rapid decline in Antarctic sea ice in recent years hints at future change. Nat. Geosci. 14, 460–464 (2021).
Bevan, S. L., A. J. Luckman, D. I. Benn, S. Adusumilli, and A. Crawford. 2021. Brief Communication: Thwaites Glacier cavity evolution. The Cryosphere Discussions 2021-66.
Zheng, Y., Heywood, K.J., Webber, B.G.M. et al. 2021. Winter seal-based observations reveal glacial meltwater surfacing in the southeastern Amundsen Sea. Commun Earth Environ 2, 40 (2021).
Benn, D. I. and D. E. Sugden. 2021. West Antarctic ice sheet and CO2 greenhouse effect: a threat of disaster. Scottish Geographical Journal 136, 2020 issue 1-4.
Thiago Dias dos Santos, Jowan M. Barnes, Daniel N. Goldberg, G. Hilmar Gudmundsson, Mathieu Morlighem. 2021. Drivers of Change of Thwaites Glacier, West Antarctica, Between 1995 and 2015. Geophysical Research Letters 48:20 e2021GL093102.
Ultee, L. and J. N. Bassis. 2020. SERMeQ Model Produces a Realistic Upper Bound on Calving Retreat for 155 Greenland Outlet Glaciers. Geophysical Research Letters 47:21. e2020GL090213.
Boehme, L. and I. Rosso. 2021. Classifying Oceanographic Structures in the Amundsen Sea, Antarctica. Geophysical Research Letters 48:5, e2020GL089412.
Goldberg, D. N., T. A. Smith, S. HK Narayanan, et al. 2020. Bathymetric influences on Antarctic ice-shelf melt rates. ESS Open Archive: October 22, 2020.
Nearly 60 scientists and support staff are on their way to Thwaites Glacier in Antarctica as part of the ambitious international effort to understand the glacier and surrounding ocean system to determine its future contributions to global sea-level rise. This season represents the fourth of five planned field seasons for the research.