Since 1984,
annual glacier mass balance measurements have been conducted on 8 glaciers by the North Cascades Glacier Climate Project (NCGCP).
The annual glacier mass balance record below indicates that the response of annual balance is quite similar for each glacier.
The map at right indicates the location of the glaciers (green circles) where we monitor
annual glacier mass balance.
Not exact matches
In a recent study, Mathias Trachsel (Dept. of Biology, University of Bergen) and Atle Nesje (Dept. of Earth Science, University of Bergen and Uni Research Climate) used simple statistical models to assess and quantify the relative importance of summer temperature and winter precipitation for
annual mass balances of eight Scandinavian
glaciers.
... tba... For additional information on the status of the
glacier and on data relating to
annual mass balance and other measurements, visit the WGMS Fluctuations of
Glaciers Browser.
This yields the
annual mass balance of the
glacier (Pelto, 1988; 1996 and Pelto and Riedel, 2001).
As predictors of
glacier mass balance positive MEI values, El Nino, and warm phase PDO's favor negative balances, and cool phase PDO's and negative MEI values, La Nina, favor positive
annual balances.
Pelto (1988) in examining the first several years of
mass balance data postulated that the variation in
annual balance between
glaciers is due to their different geographic characteristics.
Annual net balance on eight North Cascades
glaciers during the 1984 - 1994 period has been determined by measurement, of total
mass loss from firn and ice melt and, of residual snow depth at the end of the summer season.
To identify the impact of sampling density on determination of a
glacier's
annual mass balance, the North Cascade
Glacier Climate Project utilized a varying density of measurements to determine
annual mass balance on Columbia
Glacier, Washington and Lemon Creek
Glacier, Alaska.
To ascertain the
annual balance of a
glacier from a sparse network of observations is optimized by detailed mapping of
mass balance across the
glacier determined from a high - density measurement network during several years.
The graph for global
glacier mass change shows the estimated
annual cumulative balance for a set of global reference
glaciers with more than 30 continued observation years for the time - period 1960 - 2017.
Annual mass balance is typically assessed from a sparse network (0.5 - 50 points / km2) of sample locations that are not uniformly distributed across the
glacier (Pelto, 1996; Fountain and Vecchia, 1999).
Equilibrium line - The boundary between the region on a
glacier where there is a net
annual loss of ice
mass (ablation area) and that where there is a net
annual gain (accumulation area).
For information on the status of the
glacier and on data relating to
annual mass balance and other measurements, visit the WGMS Fluctuations of
Glaciers Browser.
It is the first study to directly link past glacial events with
annual data from ice cores — cylindrical samples drilled from the
glacier — extracted from the same ice
mass.
... tba... For information on the status of the
glacier and on data relating to
annual mass balance and other measurements, visit the WGMS Fluctuations of
Glaciers Browser.
The mean air temperature (1906 - 2005) measured at the climate station Vent (1906 m a.s.l) was -1.6 °C and the mean
annual lapse rate is 0.57 °C / 100 m. For additional information on the status of the
glacier and on data relating to
annual mass balance and other measurements, visit the WGMS Fluctuations of
Glaciers Browser.
Consistent
annual mass balance measurements over at least a 20 year period are available on 16
glaciers in North America.
The World Glacier Monitoring Service (WGMS) collects
annual mass balance data from alpine
glaciers around the world.
North Cascade
glaciers annual balance has averaged -0.54 m / a of water equivalent from 1984 - 2006, a cumulative loss of over 12.4 m in
glacier thickness or 20 - 40 % of their total volume since 1984 due to negative
mass balances.
A series of benchmark
glaciers around the world were chosen where
annual mass balance would be monitored.
Annual mass balance is the most sensitive annual glacier climate indi
Annual mass balance is the most sensitive
annual glacier climate indi
annual glacier climate indicator.
Annual mass balance is the most sensitive
glacier indicator of
glacier response to climate change.
Annual mass balance is the difference between winter snow and ice accumulation on a
glacier, and summer snow and ice loss from a
glacier during a given year.
The difference between the accumulation and ablation for a given year describes the
annual net
mass balance, which corresponds to the change in
glacier thickness and volume.
Marshall's work is part of the seasonal and
annual tracking of
glacier mass balance by the federal government to help determine future water supply in major rivers.
Both have been the key to maintaining the extensive
annual fieldwork program that is required to measured and report
glacier mass balance.
For additional information on the status of the
glacier and on data relating to
annual mass balance and other measurements, visit the WGMS Fluctuations of
Glaciers Browser.