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The boundary between the accumulation and ablation zones is called the equilibrium line.
In a generalized vertical differentiation framework, the equilibrium line is exactly the same as the first-best socially optimal line.
The elevation at which accumulation and melting of glacier ice are equal is known as the equilibrium line and is roughly equivalent to the snow line.
Our results also suggest that, in temperate regions, alpine glaciers are capable of eroding downward at faster rates than rivers above the equilibrium line altitude (ELA).
Results show that Equilibrium Line Altitude depressions (ΔELAs) associated to Younger Dryas and Early Holocene stadials are smaller than documented at most available sites in the northern Alps.
In Figure 1 this phenomenon is shown by the dashed line that, after beginning at h, dips below the equilibrium line and eventually meets it at a higher temperature.
Similar(16)
The corresponding equilibrium line-charge density is about a factor of two less than the classical predicted value from condensation theory of e/ l B ≈1100 (where e is the elementary charge and l B = 0.75 nm is the Bjerrum length) [ 33, 34].
This paper presents geomorphological evidence of glaciations on Mount Lovćen, along with a reconstruction of paleoglacier dimensions and estimations of the paleo-equilibrium line altitude.
The results allow the analysis of the patterns of glacial erosion and the estimation of the palaeo-Equilibrium Line Altitudes (ELA).
Last Glacial Maximum equilibrium-line altitudes and paleoclimate, northern Uinta Mountains, Utah, U.S.A. Journal of Glaciology, 48, 257 266].
Peak altitudes, hypsometry, geology, and former equilibrium-line altitudes (ELAs) are analysed across the Sredinny Mountains (Kamchatka).
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