Climate and surface mass balance of coastal West Antarctica resolved by regional climate modelling

• Published in: Annals of Glaciology
• Main Authors: Jan T. M. Lenaerts, Stefan R. M. Ligtenberg, Brooke Medley, Willem Jan Van de Berg, Hannes Konrad, Julien P. Nicolas, J. Melchior Van Wessem, Luke D. Trusel, Robert Mulvaney, Rebecca J. Tuckwell, Anna E. Hogg, Elizabeth R. Thomas
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2018
• Subjects: accumulation; Antarctic glaciology; ice/atmosphere interactions; snow/ice surface processes; surface mass budget; Meteorology. Climatology; QC851-999; Antarctic; West Antarctic Ice Sheet; West Antarctica; Annals of Glaciology; Antarc*; Antarctica; ice core; Ice Sheet; Ice Shelf
• Online Access: https://doi.org/10.1017/aog.2017.42; https://doaj.org/article/1170a321cb504e068377d99257e81bb6

West Antarctic climate and surface mass balance (SMB) records are sparse. To fill this gap, regional atmospheric climate modelling is useful, providing that such models are employed at sufficiently high horizontal resolution and coupled with a snow model. Here we present the results of a high-resolution (5.5 km) regional atmospheric climate model (RACMO2) simulation of coastal West Antarctica for the period 1979–2015. We evaluate the results with available in situ weather observations, remote-sensing estimates of surface melt, and SMB estimates derived from radar and firn cores. Moreover, results are compared with those from a lower-resolution version, to assess the added value of the resolution. The high-resolution model resolves small-scale climate variability invoked by topography, such as the relatively warm conditions over ice-shelf grounding zones, and local wind speed accelerations. Surface melt and SMB are well reproduced by RACMO2. This dataset will prove useful for picking ice core locations, converting elevation changes to mass changes, for driving ocean, ice-sheet and coupled models, and for attributing changes in the West Antarctic Ice Sheet and shelves to changes in atmospheric forcing.