Ablation triangles are placed in a sequence from regions that first lose their snow cover to regions where snow cover perists for a significant portion
of the ablation season.
Mass balance measurements are made on the same date each year in August and again in late September close to the end
of the ablation season.
Ablation measurement on nine North Cascade glaciers for twenty - nine discrete two to six week periods during this part
of the ablation season yield mean ablation rates of 0.036 m / day, 0.038 m / day and 0.028 m / day for July, August and September respectively.
Residual snow accumulation (final late snow balance: Mayo et al., 1972) at the end
of the ablation season is determined using probing and crevasse stratigraphy on the same date as ablation measurements are completed.
Measurements are made in late July and early August on Columbia Glacier, recording the ablation during the first three months
of the ablation season, for water resource assessment purposes and redrilling of the stakes when necessary.
In Glacier National Park, North Cascades, Helm Glacier and Place Glacier frequent loss of the entire snowcover by the end
of the ablation season has become commonplace (WGMS, 2005 The result is in net ablation throughout the accumulation area causing thinning of the glacier in the accumulation zone.
The exceptional extension
of the ablation season in 2010 in southern Greenland indicates the vulnerability of these areas to expanded melt regions (Box et al, 2010).
Measurements are made in late July and early August, recording the ablation during the first three months
of the ablation season, for water resource assessment purposes and redrilling of the stakes when necessary.
Not exact matches
Our November 2012 field
season to Alexander Island (
Ablation Point Massif and Fossil Bluff) operated out
of Rothera, a research station
of the British Antarctic Survey.
Ablation rates in May at the start
of the melt
season are widely variable from site to site, but fit within specific mean ranges based on elevation.
Revisiting each site through the
ablation season and measuring the emergence
of each stake identifies the
ablation rate.
Ablation is measured by emplacing stakes in the glacier at the end
of the previous melt
season or the beginning
of the melt
season.
This narrow range indicates that late in the
ablation season the density
of snowpack on North Cascade glaciers is uniform, and need not be measured to determine mass balance.
Accumulation and
ablation both primarily take place during the warm
season and the formation
of superimposed ice on this continental - type glacier is important.