3.1 WHITE (CANADA/HIGH ARCTIC)


COORDINATES: 79°27' N / 90°40' W

Photo taken by C.S.L. Ommanney (NHRI - Canadian Glacier Information Centre, date unknown)

White Glacier is a valley glacier occupying 38.7 km2 in the Expedition Fiord area of Axel Heiberg Island, N.W.T. It extends in elevation from 1782 m to 56 m a.s.l. Sea-level temperature in the Expedition Fiord area averages about -20 °C, but the glacier is known to have a bed which is partly unfrozen, at least beneath the valley tongue; ice thickness reaches or exceeds 400 m. Annual precipitation at sea level is very low, about 100 mm. Annual accumulation, however, is greater at higher altitudes, reaching 380 mm/a at 2000 m on the Mueller Ice Cap to the north of White Glacier. Annual ablation at the terminus of the glacier is typically 2000 - 4000 mm. The terminus appears to be retreating steadily at about 5 m/a.

The "normal" mass-balance for 29 years recorded, i.e., 1960 to 1991, was -100 +/-48 mm, with extreme annual values of -780 mm and 350 mm. The balance years 1993/94 (-314 mm) and 1994/95 (-362 mm) were more negative than normal by about 1 or 2 standard errors. The variation of mass balance with altitude was comparable with that observed in previous years, with a steep gradient and substantial small-scale variability at lower altitudes; the balance is comparatively much less variable, and smaller in magnitude, in the upper ablation area and in the accumulation area.

3.1.1 Topography and observational network

3.1.2 Net balance maps 1993/94 and 1994/95

3.1.3 Net balance versus altitude (1993/94 and 1994/95)

3.1.4 Accumulation area ratio (AAR) and equilibrium line altitude (ELA) versus specific net balance for the whole observation period