The Whitechuck Glacier has simply not been happy with the 1.4 o F warming the North Cascade region has experienced since the 19th century, and its reduced income in the form of reduced accumulation, and increased expenditures in the form of
increased ablation have led to a negative balance in its glacier ice savings account.
Increased ablation even in a single summer will cause thinning near the ice front.
The result of the failure to recapture meltwater as internal accumulation is
increased ablation and negative annual balances (Kaser and Osmaston, 2002)
Glacier mass balance modelling indicates that to compensate for
the increased ablation from a temperature rise of 1 °C a precipitation increase of 20 % (Oerlemans, 1981) or 35 % (Raper et al., 2000) would be required.
Still, there is no question that increased dust on snow
increases ablation (mass loss)(though if the dust / dirt cover becomes thick enough, it actually winds up lowering ablation rates through insulation).
The main way that a moderate change in the air temperature or any other term
increases ablation is by increasing the proportion of the day during which melting can occur.
Not exact matches
Researchers have attributed glacial decline to
increasing temperatures, which have reduced the period of glacial accumulation and extended the period of summer ice melting (
ablation).
Chris P. Jew, Chia - Shan Wu, Hao Sun, Jie Zhu, Jui - Yen Huang, Dinghui Yu, Nicholas J. Justice, Hui - Chen Lu (2013) «mGluR5
ablation in cortical glutamatergic neurons
increases novelty - induced locomotion», PLoS ONE, 8: e70415.
Satyanarayana, A., Klarmann, K.D., Gavrilova, O. & Keller, J.R.
Ablation of the transcriptional regulator Id1 enhances energy expenditure,
increases insulin sensitivity, and protects against age and diet induced insulin resistance, and hepatosteatosis.
Detailed studies of the energy balance and
ablation of the Zongo and Chacaltaya glaciers support the importance of air temperature
increase, and identify the
increase in downward infrared radiation as the main way that the effect of the warmer air is communicated to the glacier surface [Wagnon et al. 1999; Francou et al, 2003].
Therefore, if conditions allow the glacier surface to warm to 0 C, the amount of
ablation that can be sustained by a given energy input
increases dramatically.
Air temperature
increases similar to those observed aloft since 1960, amplified by associated
increases in humidity, account for a significant portion of the enhanced
ablation leading to this strongly negative mass balance, but the exact proportion is highly uncertain because of the short span of energy and mass balance observations.
There is a threshold of glacier extent reduction dependent on the magnitude of
ablation rate
increase, where glacier runoff declines, the few examples suggest this is in the 10 - 20 % areal extent loss.
The accumulation area decreased by 24.8 %, while
ablation area
increased by 17.7 % with nearly 6 %
increase in debris - cover surface in
ablation zone in 1958 to 2011.
Recent research indicates it may be related to
increasing friction at the base of the ice sheets slowing
ablation and allowing greater thicknesses.
In the North Cascades the warmer temperatures have
increased summer
ablation on the glaciers (Pelto, 2006).
The advance
increases the glaciers area at low elevation where
ablation is highest, returning the glacier to equilibrium.
This is their sensitivity Achilles Heel: relatively little
increases in melt can expand the
ablation zone appreciably given the low surface slopes and low accumulation rates.
The warming could, under certain circumstances,
increase the sublimation, but the effect of this on
ablation is generally small, because of the high energy required for sublimation.