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• 21. Sea ice in March 2007

  was well within the median and closest to shore, about 50n.m. NW off Straumsnes and 60n.m. W off Barði. The ice-edge density was extensively 4/10 or less than 7-9/10 north off 67°20'N. A considerable diagenis was discovered in the southernmost part of the exploratory territory. No other dispatches were made during the month. Easterly and later northeasterly winds were common in the Greenland /sea-ice/monthly/2007/nr/2300

• 22. Sea ice in July 2007

  in the month. One dispatch was received, regarding ice scattering and iceberg quite off shore, or 67°05N and 30°18W and south to 66°33N and 30°09W. Slow northeasterly or variable winds were predominant in the Greenland strait in the month and the ice appeared, according to satellite information, to reduce as the month progressed /sea-ice/monthly/2007/nr/2304

• 23. Sea ice in November 2010

  WNW of Straumnes and the ice was scattered. Two observations from ships were received 29th November, on a strip at location 66°50´N - 24°36´W and at 67°00´N - 24°02´W. Wind directions were mostly from the northeast and the east, however southwesterlies occurred for a few days at the Greenland Strait /sea-ice/monthly/2010/nr/2346

• 24. Kok_JGEC658_2009

  the values of the relationships was based on information from these and other studies, using a mix between classifying and ranking. Relationships were classified in ranked groups, within which relationships were ranked again. This ranking was further refined by a paired comparison analysis. Scouvart’s study was particularly helpful to exclude a large number of possible combinations. A final step /media/loftslag/Kok_JGEC658_2009.pdf

• 25. ved-eng-2009

  at individual stations and ranking (1 = warmest, 3 = third warmest etc.). station temperature anomaly rank of Reykjavík (SW) 5.55 1.24 10 139 Stykkishólmur (W) 4.70 1.22 14 165 Bolungarvík (NW) 3.87 0.93 20 113 Grímsey (N) 3.69 1.25 10 136 Akureyri (N) 4.06 0.77 31 129 Grímsstaðir (NE) 1.62 1.12 20 103 Egilsstaðir (E) 3.92 0.98 17 60 Dalatangi (E) 5.02 1.29 4 72 Teigarhorn (E) 4.89 1.17 /media/vedurstofan/utgafa/skylduskil/ved-eng-2009.pdf

• 26. Sea ice in October 2008

  but somewhat of icebergs and one dispatch regarding a possible iceberg was received on October 9th at 67°24N and 25°41W. On the 21st sea ice was clearly noticable on satellitepictures, which by then had moved into the Greenland Strait and bordered the Blosseville coast of Greenland. Sea ice was considerably more than average for October. Harsh northerly winds were on the Greenland Strait until /sea-ice/monthly/2008/nr/2319

• 27. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 28. isskyrsla_14122010

  Hafísskýrsla TF-SIF 14. desember 2010 Flug nr. 17610.025 Óformleg ískönnun 14. desember 2010 Óformleg ískönnun var gerð og kom eftirfarandi í ljós. Ísröndin samkvæmt ratsjá TF-SIF 1) 68 03.0N 17 19.0W 2) 67 41.0N 18 19.0W 3) 67 36.0N 19 09.0W 4) 67 21.0N 19 43.0W 5) 66 53.0N 20 21.0W 6) 66 45.0N 19 58.0W 7) 66 38.0N 20 42.0W 8) 67 02.0N 21 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 29. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 30. Kok_and_Veldkamp_editorial_ES-2011-4160

  a wealth of scaling techniques and models in the search for appropriate disciplinary scales to detect relevant levels of organization. The shift toward more integrated theory and practice was initiated by the inclusion of the human factor. As a result, levels of organization became clearer, systems became more complex, and interdisciplinarity a necessity. This culminated in a new research paradigm /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf