The mean annual accumulation rate decreases from about 440mm water equivalent at the western sites T9 and T13 to about 250mm at the central positions T41 and Crete. Most of the prominant inter-annual changes of the surface mass balance appear to be well preserved over the area investigated. -from Authors
CITATION STYLE
Anklin, M., Stauffer, B., Geis, K., & Wagenbach, D. (1994). Pattern of annual snow accumulation along a west Greenland flow line: no significant change observed during recent decades. Tellus, Series B, 46 B(4), 294–303. https://doi.org/10.3402/tellusb.v46i4.15804
Mendeley helps you to discover research relevant for your work.