Jökull


Jökull - 01.01.2005, Side 156

Jökull - 01.01.2005, Side 156
Þröstur Þorsteinsson et al 0.591 0.592 0.593 0.594 0.595 0.596 7.068 7.069 7.07 7.071 7.072 7.073 MD00 MD02 MD03 MD05 MD06 MD07 MD08 MD09 MD10 MD11 MD12 MD13 MD14 Easting ( b ×106 m) N or th in g (× 10 6 m ) Figure 1. a) Location of the study area on the northern part of Mýrdalsjökull, S-Iceland. The area is about 4 km x 4 km (black box). b) Locations of the stakes in UTM coordinate system, in the 28N zone. – a) Staðsetning mælisvæðisins á norðanverðumMýrdalsjökli. b) Mælipunktarnir í UTM hnitakerfi, svæði 28N. in June was supposed to follow exactly the same pro- cedure as the survey in April, in order to allow an anal- ysis of baseline length change, yielding high accuracy strain rates. Unfortunately, bad weather, crevasses, and equipment failure made that impossible. Figure 2. Visiting the permanent stations in Septem- ber was tricky due to dirt cones and crevasses. The large amount of melting can be seen from the trian- gular platform that was 20 cm off the snow surface in June. – Dríli og sprungur gerðu leiðangursmönn- um erfitt fyrir að komast aðmælistöðvum í september. Á þríhyrningslagaða loftnetspallinum má glöggt sjá hversu mikill bráðnun hefur átt sér stað frá júní, en þá var hann 20 cm yfir yfirborði. The Icelandic Meteorological Office operates a permanent GPS station (SOHO) near the south termi- nus of Mýrdalsjökull, about 20 km south of the sur- vey area. Absolute base coordinates of the station are listed as 63.55247◦N, 19.24665◦W, at 791.6 m eleva- tion. Daily RINEX files are available on the Internet, eliminating the need for setting up a base station for this survey. Three of the marks, MD00, MD11, and MD12, were set up for semi-permanent recording (Figures 1– 4). In each case 3 poles were drilled to a depth of approximately 8 m and fitted with a wood plug at the bottom to prevent self-drilling. A triangular plywood platform served as the antenna-mounting surface atop the three poles (Figure 3). Rough solar panels mounts were constructed of wood. A 20 amp hr battery was used to power the three receivers. Solar panel mounts were hose clamped to a ∼30 cm long PVC tube that fit over one of the survey poles, allowing the panels to subside with the surface melting (Figure 4). The battery and receiver were tied to a similar tube or the mount itself, in hope that they too would subside with glacier surface ablation. A 10 m antenna cable was coiled under the platform; allowing the receiver box to subside relative to the fixed antenna as the surface melted. Melt rate during the April fieldwork was be- tween a few and up to 20 cm d−1. 156 JÖKULL No. 55, 2005
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