Satellite-based estimates of Antarctic surface meltwater fluxes

• Main Authors: Trusel, L.D., Frey, K.E., Das, S.B., Kuipers Munneke, P., van den Broeke, M.R., Dijkstra, H.A.
• Other Authors: Marine and Atmospheric Research, Sub Dynamics Meteorology, Sub Physical Oceanography
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2013
• Subjects: Antarctic; Kuipers; Antarc*; Ice Shelf
• Online Access: https://dspace.library.uu.nl/handle/1874/290634

This study generates novel satellite-derived estimates of Antarctic-wide annual (1999–2009) surface meltwater production using an empirical relationship between radar backscatter from the QuikSCAT (QSCAT) satellite and melt calculated from in situ energy balance observations. The resulting QSCAT-derived melt fluxes significantly agree with output from the regional climate model RACMO2.1 and with independent ground-based observations. The highresolution (4.45 km) QSCAT-based melt fluxes uniquely detect interannually persistent and intense melt (>400mm water equivalent (w.e.) year 1) on interior Larsen C Ice Shelf that is not simulated by RACMO2.1. This supports a growing understanding of the importance of a föhn effect in this region and quantifies the resulting locally enhanced melting that is spatially consistent with recently observed Larsen C thinning. These new results highlight important cryosphere-climate interactions and processes that are presently not fully captured by the coarser-resolution (27 km) regional climate model. Citation: Trusel, L. D., K. E. Frey, S. B. Das, P. Kuipers Munneke, and M. R. van den Broeke (2013), Satellite-based estimates of Antarctic surface meltwater fluxes, Geophys. Res. Lett., 40, 6148–6153, doi:10.1002/2013GL058138.