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  • 1
    Type of Medium: Book
    Series Statement: Rit Fiskideildar 12,3
    Language: Undetermined
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Journal of the European Academy of Dermatology and Venereology 3 (1994), S. 0 
    ISSN: 1468-3083
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Medicine
    Notes: Objective To investigate if bathing in a unique thermal lagoon in Iceland has a therapeutic effect on psoriasis.Design An open study where twenty-seven psoriasis patients bathed for three weeks in the lagoon. Psoriasis Area and Severity Index (PASI) was used to evaluate the severity of the disease before during and after bathing.Results The mean PASI score decreased from 16.1 to 8.1 (p= 0.01). The PASI score decreased most in the first week. The area of the lesions did not diminish but scaling erythema and infiltration decreased. Only very limited UV-radiation was observed during the bathing period.Conclusions Bathing in the lagoon has a favourable effect on psoriasis although in some cases it may not be sufficient as a single treatment. Further studies over longer period are needed.
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. Macroinvertebrate assemblages were studied in the glacial river West-Jökulsá, originating from the Hofsjökull Ice Cap in central Iceland at an altitude of 860 m. Sampling sites were distributed from the source to 45 km downstream at 160 m a.s.l. Comparative studies were carried out on non-glacial rivers and tributaries in the area, at similar altitudes and distances from the glacial source.2. Detrended correspondence analysis (DCA) demonstrated that species composition of benthic macroinvertebrates was related to the distance from the glacier. Assemblages at sampling sites furthest from the glacier were similar in species composition to sites in non-glacial rivers. Temporal variation was small compared with longitudinal zonation.3. Based on canonical correspondence analysis (CCA) of data from the main glacial river, distance from the glacier, altitude, bryophyte biomass and the Pfankuch Index of channel stability were the measured explanatory variables having a significant effect on the structure of macroinvertebrate assemblages, accounting for 31% of the total variation in the data set. When data from all the rivers were analysed, altitude, bryophyte biomass, channel slope, suspended sediment concentration and maximum water temperature explained 21% of the variance.4. Macroinvertebrate communities were in general agreement with the predictions of the conceptual model of Milner & Petts (1994) for the upstream reaches. The assemblages consisted mainly of Orthocladiinae and Diamesinae (Chironomidae), although other taxa such as Simuliidae, Plecoptera and Trichoptera were also found in low numbers. Shredders were lacking from the benthic communities, apparently because of continued glacial influence in the river even 45 km downstream from the glacier and lack of allochthononus inputs from riparian vegetation.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. The influence of 11 environmental variables on benthic macroinvertebrate communities was examined in seven glacier-fed European streams ranging from Svalbard in the north to the Pyrenees in the south. Between 4 and 11 near-pristine reaches were studied on each stream in 1996–97.2. Taxonomic richness, measured at the family or subfamily (for Chironomidae) levels for insects and higher levels for non-insects, increased with latitude from Svalbard (3 taxa) to the Pyrenees (29 taxa).3. A Generalized Additive Model (GAM) incorporating channel stability [Pfankuch Index (PFAN)], tractive force, Froude number (FROU), water conductivity (COND), suspended solids (SUSP) concentration, and maximum temperature explained 79% of the total deviance of the taxonomic richness per reach. Water temperature and the PFAN of stability made the highest contribution to this deviance. In the model, richness response to temperature was positive linear, whereas the response to the PFAN was bell-shaped with an optimum at an intermediate level of stability.4. Generalized Additive Models calculated for the 16 most frequent taxa explained between 25 (Tipulidae) and 79% (Heptageniidae) of the deviance. In 10 models, more than 50% of the deviance was explained and 11 models had cross-validation correlation ratios above 0.5. Maximum temperature, the PFAN, SUSP and tractive force (TRAC) were the most frequently incorporated explanatory variables. Season and substrate characteristics were very rarely incorporated.5. Our results highlight the strong deterministic nature of zoobenthic communities in glacier-fed streams and the prominent role of water temperature and substrate stability in determining longitudinal patterns of macroinvertebrate community structure. The GAMs are proposed as a tool for predicting changes of zoobenthic communities in glacier-fed streams under climate or hydrological change scenarios.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1546-1718
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] Hair, skin and eye colors are highly heritable and visible traits in humans. We carried out a genome-wide association scan for variants associated with hair and eye pigmentation, skin sensitivity to sun and freckling among 2,986 Icelanders. We then tested the most closely associated SNPs from six ...
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 255 (1975), S. 138-141 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The eruption on Heimaey, the largest of the Westman Islands, started on January 23, 1973, and lasted about five months, during which a substantial fraction of the volcanics was deposited in the sea6. Although the eruption did not occur under the sea it provided an opportunity to observe ...
    Type of Medium: Electronic Resource
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  • 7
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    Arctic Monitoring and Assessment Programme (AMAP)
    In:  Arctic Monitoring and Assessment Programme (AMAP), Oslo, Norway, vii, 99 pp. ISBN 978-82-7971-082-0
    Publication Date: 2013-12-18
    Type: Book , NonPeerReviewed
    Format: text
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  • 8
    Publication Date: 2024-02-07
    Description: We evaluate the decadal evolution of ventilation and anthropogenic carbon (C-ant) in the Nordic Seas between 1982 and the 2010s. Ventilation changes on decadal timescale are identified by evaluating decadal changes in mean ages and apparent oxygen utilization in each of the four main basins of the Nordic Seas (the Greenland and Iceland Seas, and the Norwegian and Lofoten Basins). The ages are derived from the transient time distribution approach, based on the transient tracers chlorofluorocarbon-12 (CFC-12) and sulfur hexafluoride (SF6). The different decades show different phases in ventilation, with the 2000s being overall better ventilated than the 1990s in all basins. For the Greenland Sea, we also show that the 2010s are better ventilated than the 2000s, with a clear shift in hydrographic properties. The evolution of concentrations and inventory of C-ant is linked to the ventilation state. The deep waters get progressively older over the analyzed period, which is connected to the increased fraction of deep water from the Arctic Ocean.Plain Language Summary The ocean region between Greenland, Iceland, and Norway, called the Nordic Seas, is a main site of deep-water formation. This process produces dense waters and brings surface waters to larger depths, thereby ventilating the water below. This transports, among other things, man-made CO2 (anthropogenic carbon; C-ant) and oxygen from the atmosphere into the interior ocean, thereby reducing the amount of CO2 stored in the atmosphere. This study investigates how the ventilation has changed in the Nordic Seas from 1982 to the 2010s. We find that the ventilation has changed with time, from a rather well-ventilated state in 1982, to a reduced ventilation in the 1990s, and then a restrengthened ventilation from the 2000s.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2009. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 114 (2009): C05020, doi:10.1029/2008JC004808.
    Description: The freshwater composition of waters on the southeast Greenland shelf and slope are described using a set of high-resolution transects occupied in summer 2004, which included hydrographic, velocity, nutrient, and chemical tracer measurements. The nutrient and tracer data are used to quantify the fractions of Pacific Water, sea ice melt, and meteoric water present in the upper layers of the East Greenland Current (EGC) and East Greenland Coastal Current (EGCC). The EGC/EGCC system dominates the circulation of this region and strongly influences the observed distribution of the three freshwater types. Sea ice melt and meteoric water fractions are surface intensified, reflecting their sources, and generally increase southward from Denmark Strait to Cape Farewell, as well as shoreward. Significant fractions of Pacific Water are found in the subsurface layers of the EGCC, supporting the idea that this inner shelf branch is directly linked to the EGC and thus to the Arctic Ocean. A set of historical sections is examined to investigate the variability of Pacific Water content in the EGC and EGCC from 1984 to 2004 in the vicinity of Denmark Strait. The fraction of Pacific Water increased substantially in the late 1990s and subsequently declined to low levels in 2002 and 2004, mirroring the reduction in Pacific Water content reported previously at Fram Strait. This variability is found to correlate significantly with the Arctic Oscillation index, lagged by 9 years, suggesting that the Arctic Ocean circulation patterns bring varying amounts of Pacific Water to the North Atlantic via the EGC/EGCC.
    Description: This work was funded by National Science Foundation grant OCE- 0450658. D. Sutherland also received support from the Woods Hole Oceanographic Institution Academic Programs Office.
    Keywords: Pacific Water ; East Greenland current ; Arctic Oscillation ; Freshwater composition ; Cape Farewell ; Denmark Strait
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 10
    Publication Date: 2023-05-12
    Description: The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.
    Keywords: 1; 10; 101; 11; 12; 13; 14; 15; 16; 162; 17; 18; 19; 2; 20; 21; 22; 23; 24; 25; 26; 262; 27; 28; 29; 3; 30; 31; 32; 33; 34; 35; 36; 362; 37; 38; 39; 4; 40; 41; 42; 43; 44; 45; 46; 462; 47; 48; 49; 5; 50; 51; 52; 53; 54; 55; 56; 57; 58; 59; 6; 60; 61; 62; 63; 64; 65; 66; 67; 68; 69; 7; 70; 71; 72; 73; 74; 75; 76; 77; 78; 79; 8; 80; 81; 82; 83; 84; 85; 87; 88; 89; 9; 90; 91; 92; 93; ARK-XIII/3; B02/98; B02/98-1001; B02/98-1011; B02/98-1021; B02/98-1031; B02/98-1061; B02/98-1062; B02/98-1071; B02/98-1081; B02/98-1101; B02/98-1111; B02/98-1121; B02/98-1131; B02/98-1141; B02/98-1151; B02/98-1181; B02/98-1191; B02/98-1221; B02/98-1222; B02/98-1231; B02/98-1241; B02/98-1251; B02/98-1261; B02/98-1271; B02/98-1281; B02/98-1291; B02/98-1292; B02/98-1293; B02/98-1301; B02/98-1311; B02/98-1321; B02/98-1361; B02/98-1371; B02/98-1381; B02/98-1391; B02/98-1401; B02/98-1411; B02/98-1421; B02/98-1431; B02/98-1441; B02/98-1451; B02/98-1461; B02/98-1471; B02/98-1481; B02/98-1491; B02/98-1501; B02/98-1511; B02/98-1521; B02/98-1531; B02/98-1541; B02/98-1551; B02/98-1561; B02/98-1571; B02/98-1581; B02/98-1591; B02/98-1601; B02/98-1611; B02/98-1622; B02/98-531; B02/98-541; B02/98-551; B02/98-561; B02/98-571; B02/98-581; B02/98-591; B02/98-601; B02/98-621; B02/98-622; B02/98-631; B02/98-641; B02/98-651; B02/98-661; B02/98-671; B02/98-681; B02/98-691; B02/98-701; B02/98-711; B02/98-721; B02/98-731; B02/98-751; B02/98-761; B02/98-771; B02/98-781; B02/98-791; B02/98-801; B02/98-811; B02/98-821; B02/98-831; B02/98-843; B02/98-845; B02/98-851; B02/98-861; B02/98-891; B02/98-901; B02/98-911; B02/98-921; B02/98-931; B02/98-941; B02/98-961; B02/98-971; B02/98-972; B02/98-973; B02/98-981; B02/98-991; B03/97; B03/97-531; B03/97-532; B03/97-551; B03/97-552; B03/97-711; B03/97-712; B03/97-751; B03/97-752; B03/97-753; B03/97-771; B03/97-772; B03/97-781; B03/97-782; B03/97-931; B03/97-932; B05/96; B05/96-1252; B05/96-252; B05/96-253; B05/96-254; B05/96-263; B05/96-278; B05/96-293-2; B06/97; B06/97-1431; B06/97-1441; B06/97-1451; B06/97-1461; B06/97-1471; B06/97-1481; B06/97-1492; B06/97-1501; B06/97-1511; B06/97-1512; B06/97-1513; B06/97-1521; B06/97-1531; B06/97-1541; B06/97-1551; B06/97-1561; B06/97-1571; B06/97-1581; B06/97-1591; B06/97-1601; B06/97-1611; B06/97-1621; B06/97-1631; B06/97-1643; B06/97-1644; B06/97-1651; B06/97-1661; B06/97-1671; B06/97-1681; B06/97-1691; B06/97-1701; B06/97-1711; B06/97-1721; B06/97-1731; B06/97-1741; B06/97-1751; B06/97-1761; B06/97-1772; B06/97-1773; B06/97-1781; B06/97-1791; B06/97-1801; B06/97-1811; B06/97-1821; B06/97-1831; B06/97-1841; B06/97-1851; B06/97-1861; B06/97-1871; B06/97-1881; B06/97-1891; B06/97-1901; B06/97-1911; B06/97-1912; B06/97-1921; B06/97-1931; B06/97-1941; B06/97-1951; B06/97-1971; B06/97-1981; B06/97-1991; B06/97-2001; B06/97-2011; B06/97-2021; B06/97-2031; B06/97-2041; B06/97-2051; B06/97-2061; B06/97-2071; B06/97-2081; B06/97-2091; B06/97-2101; B06/97-2121; B06/97-2122; B06/97-2131; B06/97-2141; B06/97-2142; B06/97-2151; B06/97-2161; B06/97-2171; B06/97-2181; B06/97-2191; B06/97-2211; B06/97-2221; B06/97-2231; B06/97-2241; B06/97-2251; B06/97-2261; B06/97-2271; B06/97-2281; B06/97-2291; B06/97-2301; B06/97-2311; B06/97-2321; B06/97-2331; B06/97-2341; B06/97-2351; B06/97-2361; B06/97-2371; B06/97-2381; B06/97-2391; B06/97-2401; B06/97-2411; B06/97-2421; B06/97-2431; B06/97-2441; B06/97-2451; B06/97-2461; B06/98; B06/98-2531; B06/98-2541; B06/98-2551; B06/98-2561; B06/98-2571; B06/98-2581; B06/98-2582; B06/98-2591; B06/98-2592; B06/98-2601; B06/98-2611; B06/98-2612; B06/98-2621; B06/98-2631; B06/98-2641; B06/98-2642; B06/98-2651; B06/98-2652; B06/98-2661; B06/98-2671; B06/98-2672; B06/98-2681; B06/98-2691; B06/98-2701; B06/98-2711; B06/98-2721; B06/98-2741; B06/98-2751; B06/98-2761; B06/98-2771; B06/98-2781; B06/98-2791; B06/98-2801; B06/98-2811; B06/98-2821; B06/98-2831; B06/98-2841; B06/98-2851; B06/98-2861; B06/98-2871; B06/98-2881; B06/98-2891; B06/98-2901; B06/98-2911; B06/98-2921; B06/98-2931; B06/98-2941; B06/98-2951; B06/98-2961; B06/98-2971; B06/98-2981; B06/98-2991; B06/98-3001; B06/98-3002; B06/98-3003; B06/98-3004; B06/98-3011; B06/98-3012; B06/98-3021; B06/98-3031; B06/98-3041; B06/98-3051; B06/98-3081; B06/98-3101; B06/98-3102; B06/98-3103; B06/98-3104; B06/98-3121; B06/98-3141; B06/98-3142; B06/98-3143; B06/98-3144; B06/98-3161; B06/98-3171; B06/98-3181; B06/98-3191; B06/98-3201; B06/98-3211; B06/98-3221; B06/98-3231; B06/98-3241; B06/98-3251; B06/98-3261; B06/98-3271; B06/98-3321; B06/98-3331; B06/98-3341; B06/98-3351; B06/98-3361; B06/98-3371; B06/98-3381; B06/98-3391; B06/98-3401; B06/98-3441; B06/98-3451; B06/98-3461; B06/98-3481; B06/98-3482; B06/98-3483; B06/98-3511; B06/98-3522; B06/98-3531; B06/98-3541; B06/98-3551; B06/98-3561; B06/98-3581; B06/98-3591; B06/98-3611; B06/98-3621; B06/98-3631; B06/98-3641; B06/98-3651; B06/98-3661; B06/98-3671; B06/98-3681; B06/98-3691; B06/98-3701; B06/98-3711; B06/98-3731; B06/98-3741; B06/98-3751; B06/98-3761; B06/98-3771; B06/98-3781; B06/98-3791; B09/96; B09/96-5311; B09/96-5312; B09/96-5321; B09/96-5322; B09/96-5351; B09/96-5352; B09/96-5353; B09/96-5451; B09/96-5452; B09/96-5481; B09/96-5482; B09/96-5511; B09/96-5512; B09/96-5521; B09/96-5522; B09/96-5531; B09/96-5532; B09/98; B09/98-5432; B09/98-5433; B09/98-5434; B09/98-5441; B09/98-5451; B09/98-5461; B09/98-5471; B09/98-5481; B09/98-5491; B09/98-5501; B09/98-5511; B09/98-5531; B09/98-5541; B09/98-5551; B09/98-5561; B09/98-5581; B09/98-5601; B09/98-5631; B09/98-5641; B09/98-5651; B09/98-5661; B09/98-5671; B09/98-5681; B09/98-5711; B09/98-5731; B09/98-5732; B09/98-5741; B09/98-5751; B09/98-5771; B09/98-5791; B09/98-5792; B09/98-5801; B09/98-5804; B09/98-5805; B10/97; B10/97-3601; B10/97-3602; B10/97-3851; B10/97-3871; B10/97-3881; B10/97-3891; B10/97-3892; B10/97-3911; B10/97-3912; B10/97-3921; B10/97-3922; B10/97-3923; B10/97-3931; B10/97-3932; B10/97-3941; B10/97-4011; B10/97-4012; B10/97-4031; B10/97-4032; B10/97-4041; B10/97-4042; B12/96; B12/96-7210; B12/96-7220; B12/96-7230; B12/96-7240; B12/96-8520; B12/96-8540; B12/96-8550; B12/98; B12/98-7811; B12/98-7812; B12/98-7813; B12/98-8391; B12/98-8392; B12/98-8393; B12/98-8394; B12/98-8621; B12/98-8622; B15/97; B15/97-6761; B15/97-6771; B15/97-6781; B15/97-6791; B15/97-6801; B15/97-6811; B15/97-6821; B15/97-6831; B15/97-6841; B15/97-6851; B15/97-6861; B15/97-6871; B15/97-6881; B15/97-6891; B15/97-6892; B15/97-6901; B15/97-6902; B15/97-6912; B15/97-6921; B15/97-6931; B15/97-6951; B15/97-6961; B15/97-6971; B15/97-6981; B15/97-6991; B15/97-7001; B15/97-7011; B15/97-7021; B15/97-7031; B15/97-7041; B15/97-7051; B15/97-7061; B15/97-7071; B15/97-7081; B15/97-7091; B15/97-7101; B15/97-7111; B15/97-7121; B15/97-7131; B15/97-7141; B15/97-7151; B15/97-7161; B15/97-7171; B15/97-7181; B15/97-7182; B15/97-7191; B15/97-7201; B15/97-7211; B15/97-7221; B15/97-7231; B15/97-7241; B15/97-7251; B15/97-7261; B15/97-7271; B15/97-7281; B15/97-7291; B15/97-7301; B15/97-7311; B15/97-7321; B15/97-7331; B15/97-7341; B15/97-7351; B15/97-7361; B15/97-7371; B15/97-7381; B15/97-7391; B15/97-7401; B15/97-7411; B15/97-7421; B15/97-7431; B15/97-7441; B15/97-7451; B15/97-7461; B15/97-7471; B15/97-7481; B15/97-7491; B15/97-7501; B15/97-7511; B15/97-7512; B15/97-7513; B15/97-7521; B15/97-7531; B15/97-7532; B15/97-7533; B15/97-7541; B15/97-7551; B15/97-7561; B15/97-7571; B15/97-7581; B15/97-7591; B15/97-7601; B15/97-7611; B15/97-7621; B15/97-7631; B15/97-7641; B15/97-7651; B15/97-7661; B15/97-7671; B15/97-7681; B15/97-7691; B15/97-7692; B15/97-7701; B15/97-7711; B15/97-7721; B15/97-7731; B15/97-7741; B15/97-7751; Bjarni Saemundsson; CARDEEP1/93; CARDEEP1/93-161; CARDEEP1/93-162; CARDEEP1/93-171; CARDEEP1/93-181; CARDEEP1/93-182; CARDEEP1/93-201; CARDEEP1/93-211; CARDEEP1/93-212; CARDEEP1/93-231; CARDEEP1/93-232; CARDEEP1/93-261; CARDEEP1/93-271; CARDEEP1/93-281; CARDEEP1/93-291; CARDEEP1/93-301; CARDEEP1/93-311; CARDEEP1/93-312; CARDEEP1/93-331; CARDEEP1/93-341; CARDEEP1/93-351; CARDEEP1/93-361;
    Type: Dataset
    Format: application/zip, 51 datasets
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