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and CNES, n.d.;
National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional
altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein
et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea
level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
). This can be helpful with respect to
finding a common structure in presenting as well in session reporting (for which angles
mentioned in the opening session statements of the Workshop participants can provide
checkpoints).”
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eftirtalda staði:
1. 66°22,7‘N – 21°18,2‘V (Þaðan lá ísröndin í r/v 60°)
2. 66°23,6‘N – 21°20,8‘V
3. 66°23,6‘N – 21°27,4‘V
4. 66°25,5‘N – 21°28,8‘V
5. 66°26,5‘N – 21°41,9‘V (Þaðan lá ísröndin í norð, norðaustur)
Var ísinn ca 7-9/10 að þéttleika þar sem ísröndin var en stöku smájakar í ca 1-2 sjm. út frá ísröndinni. Á
svæðinu var þónokkur þoka eða u.þ.b. 1-2 sjm. skyggni og því ekki gott að gera
/media/hafis/skyrslur_lhg/Isskyrsla_20100116_rett.pdf
lágu frá aðal ísnum og náðum að meta
þéttleikann þar. Ekki sáust neinir borgarísjakar né stakir ísjakar í þessu flugi.
Aðalrönd íssins lá í gegnum eftirtalda punkta (tekið með radar). Að sjá var ísinn samfrosta 10/10
1. 66°13,7‘N – 025°35,7‘V
2. 66°24,0‘N – 024°26.0‘V
3. 66°50,1‘N – 023°44,1‘V
4. 67°03,1‘N – 023°31,0‘V
5. 67°00,7‘N – 023°11,3‘V
6. 66°58,7‘N – 022°39,7‘V
7. 66°55,8‘N – 022°23,5‘V
/media/hafis/skyrslur_lhg/Isskyrsla_06Jan_2010.pdf
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