accumulation, B (positive for melting), and the dif-ference in ice ßux between the two gates per unit area,]H /]t 5 A 2 B 1 (fGL 2 fDG)/ISA, where fGL and fDG are the ice ßux for the GL and the DG, respectively. Under steady-state conditions,]H /]t 5 0, and neglecting surface melt and accumula-tion...

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Main Authors: R. H. Thomas, J. Glaciol, H. H. Hellmer, S. S. Jacobs, A. Jenkins, Antarct Res, W. R. Peltier, A. Lambrecht, C. Mayer, H. Oerter, U. Nixdorf, M. Frezzotti, I. E. Tabacco, A. Zirizzotti, Ann Glaciol, J. R. Potter, J. G. Paren, Antarct Res Ser, D. R. Macayeal, J. Geophys Res, G. Wendler, K. Ahlnas, C. S. Lingle, K. W. Nicholls, K. Makinson, M. R. John, W. F. Budd, B. J. Mcinnes, D. Jenssen, I. N. Smith
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.662.5023
http://palumbi.stanford.edu/manuscripts/VollmerandPalumbi296.pdf