Hmmm...... The first article, which you quote, Code, is a blog, obviously not by a scientists, totally filled with lies and half truths.
The second citation just demostrates that Walleyes is incapable of understanding anything that he reads.
Higher surface mass balance of the Greenland ice sheet revealed by high-resolution climate modeling
Higher surface mass balance of the Greenland ice sheet revealed by high-resolution climate modeling
Higher surface mass balance of the Greenland ice sheet revealed by high-resolution climate modeling
Janneke Ettema
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, Netherlands
Michiel R. van den Broeke
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, Netherlands
Erik van Meijgaard
Royal Netherlands Meteorological Institute, De Bilt, Netherlands
Willem Jan van de Berg
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, Netherlands
Jonathan L. Bamber
Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, Bristol, UK
Jason E. Box
Department of Geography, Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA
Roger C. Bales
Sierra Nevada Research Institute, University of California, Merced, California, USA
High-resolution (∼11 km) regional climate modeling shows total annual precipitation on the Greenland ice sheet for 1958–2007 to be up to 24% and surface mass balance up to 63% higher than previously thought. The largest differences occur in coastal southeast Greenland, where the much higher resolution facilitates capturing snow accumulation peaks that past five-fold coarser resolution regional climate models missed.
The surface mass balance trend over the full 1958–2007 period reveals the classic pattern expected in a warming climate, with increased snowfall in the interior and enhanced runoff from the marginal ablation zone. In the period 1990–2007, total runoff increased significantly, 3% per year. The absolute increase in runoff is especially pronounced in the southeast, where several outlet glaciers have recently accelerated. This detailed knowledge of Greenland's surface mass balance provides the foundation for estimating and predicting the overall mass balance and freshwater discharge of the ice sheet.