Crevasse stratigraphy is used to determine
annual snow layer thickness.
Not exact matches
These
layers may be visible, related to the nature of the ice; or they may be chemical, related to differential transport in different seasons; or they may be isotopic, reflecting the
annual temperature signal (for example,
snow from colder periods has less of the heavier isotopes of H and O).
The first 110,000
annual layers of
snow in that ice core (GISP2) have been visually counted and corroborated by two to three different and independent methods as well as by correlation with volcanic eruptions and other datable events.
The ice sheet is made up of
annual layers of
snow that never melted and became compacted into ice over thousands of years.
Because a thin
layer of
snow is just as reflective as a thick
layer, the reflectivity effect depends more on the seasonal distribution of snowfall than the
annual average amount.
In a general sense, the thickness of each
annual layer tells how much
snow accumulated at that location during the year.
The gradually increasing weight of overlying
layers compresses deeply buried
snow into ice, but
annual bands remain.
They try to extract long cylinders of ice, ones that will show
annual layers of
snow and ice.
However, the more the ice compacts and the less that
snow accumulates, the harder it is to see these
annual layers.
Ice patches result from
layers of
annual snow that, until recently, remained frozen all year.