Surface elevations (digital elevation models and GPS data) for three ice rises (Blåskimen Land, Kupol Ciolkovskogo and Kupol Moskovskij) in Western Dronning Maud Land observed in 2012-14 V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2018.b951f760

In-situ tempetatures in the top 20 m of firn near the summit of Blåskimen Island, Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2017.3845e964

4. Shallow sounding (400MHz) radar profiles over three ice rises (Blåskimen Land, Kupol Ciolkovskogo and Kupol Moskovskij) in Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2016.925d72c7

Deep sounding (2MHz) radar profiles over three ice rises (Blåskimen Land, Kupol Ciolkovskogo and Kupol Moskovskij) in Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2016.e12eb5f5

Surface density measured using 3-m-deep firn cores over Blåskimen Island, Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2018.77fd5bda

Ice thickness and bed topography maps derived from radar and GPS profiles over Blåskimen Island in Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2018.65c6b172

Surface mass balance in 2005–2012 derived using shallow radar stratigraphy over Blåskimen Island, Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2018.8a025b8a

Surface mass balance derived using stake height measurements over Blåskimen Island, Western Dronning Maud Land V. Goel, J. Brown, and K. Matsuoka https://doi.org/10.21334/npolar.2018.5a60f2fd