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  • 1
    Publication Date: 2023-01-30
    Description: This dataset contains the observations of air temperature in the ship's crow's nest as conducted during the Norwegian North Polar Expedition in 1893-1896 onboard the drifting vessel Fram. Observations were obtained on an irregular schedule during the expedition. Temperatures were measured under the lead of S. Scott-Hansen. Surface air temperatures at the same points in time were measured in a weather hut placed on the ice at an approximate height of 1.5m. Data was digitized by C. Katlein manually from a scan of pages 497 and following of The Norwegian North Polar Expedition Scientific Results vol. 6 (1905) Section number 12 Meteorology compiled by H. Mohn. The scanned original is available unter https://archive.org/details/norwegiannorthpo06nans (ark:/13960/t9m333v0g). The respective full set of meteorological observations containing the geographic positions of these observations are archived at the National Snow and Ice Data Center (NSIDC): Environmental Working Group. Edited by F. Fetterer and V. F. Radionov. 2000. Environmental Working Group Arctic Meteorology and Climate Atlas, Version 1. [Fram]. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center. doi:10.7265/N5MS3QNJ.
    Keywords: air temperature; crow's nest; CT; DATE/TIME; FRAM; FRAM_Nansen-track; Nansen; Temperature, air; Temperature, difference; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 141 data points
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  • 2
    Publication Date: 2023-01-30
    Description: This dataset contains the observations of sea ice temperature conducted during the Norwegian North Polar Expedition in 1893-1896 onboard the drifting vessel Fram. Observations were obtained mostly daily during large parts of the expedition, after the method was established by F. Nansen. Temperatures were measured under the lead of S. Scott-Hansen in two or four inch wide boreholes using thermometers mounted to wooden poles, that mostly remained positioned in the ice and were pulled up for measurements. Air exchange in the holes was limited by muffs of reindeer skin wound around the wooden poles. Due to ice deformation and other influences, the thermometers needed to be moved several times and did not remain at the same site. The quality of the dataset was questioned already in 1927 by Finn Malmgren in his dissertation "On the Properties of Sea Ice" referring to systematic measurement errors. Data was digitized by C. Katlein manually from a scan of "The Norwegian North Polar Expedition Scientific Results vol. 6 (1905)" Section number 12 "Meteorology" compiled by H. Mohn. The scanned original is available unter https://archive.org/details/norwegiannorthpo06nans (ark:/13960/t9m333v0g). The respective meteorological observations containing the geographic positions of these observations are archived at the National Snow and Ice Data Center (NSIDC): Environmental Working Group. Edited by F. Fetterer and V. F. Radionov. 2000. Environmental Working Group Arctic Meteorology and Climate Atlas, Version 1. [Fram]. Boulder, Colorado USA. NSIDC: National Snow and Ice Data Center. doi: https://doi.org/10.7265/N5MS3QNJ.
    Keywords: CT; DATE/TIME; DEPTH, ice/snow; FRAM; FRAM_Nansen-track; Nansen; Sea ice; Temperature; Temperature, ice/snow; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 3070 data points
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  • 3
    Publication Date: 1994-01-01
    Description: The geometry and kinematic evolution of a frontal ramp section associated with the Tertiary West Spitsbergen Orogenic Belt has been investigated in a small area (Lappdalen) north of Isfjorden. The previously recognized thrust front corresponds to a complex step or ramp in the position of the sole-thrust in the area. The sole-thrust is localized to the evaporites of the Permian Gipshuken Formation to the west of the footwall ramp, whereas to the east it continues as a bedding-parallel thrust in Triassic shales (Sassendalen Group). The area to the west of the footwall ramp is characterized by large scale thrusts and folds involving the Permian Gipshuken and Kapp Starostin formations and the lower part of the Triassic Sassendalen Group. East of the footwall ramp both Permian and Triassic strata are sub-horizontal and apparently undeformed. Three major thrust sheets are recognized. Based on the geometric relationship between folds and faults in the area, both fault-bend and fault-propogation mechanisms of folding are inferred. Restoration of the Kapp Starostin Formation to its pre-deformational state indicates a minimum of 35% shortening. Structural observations within the Sassendalen Group in the study area and on Dickson Land suggest that some of this shortening is transmitted eastwards along one or more bedding parallel thrusts in the Sassendalen Group.
    Print ISSN: 0016-7568
    Electronic ISSN: 1469-5081
    Topics: Geosciences
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  • 4
    Call number: K 1991.13458(9/10) /
    In: Kortserie
    Type of Medium: Map available for loan
    Pages: [2 Bl.] + 2 Kt. + 2 Beil
    Edition: Oplag 1000
    ISBN: 8788640396
    Series Statement: Kortserie / Danmarks Geologiske Undersøgelse, Miljøministeriet
    Location: Upper compact magazine
    Branch Library: GFZ Library
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