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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 272 (1975), S. 143-145 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Using the atomic beam magnetic resonance method the Zeeman interactions of12C in the3 P 1 and3 P 2 states at magnetic fields of about 3.4 kOe have been measured. The measured quantities areg J (3 P 1)−gJ(3 P 2)=15.4(1.0)·10−6 g J (3 P 2)=1.5010616 (50), from which the following value for gJ(3P1) can be calculated:g J (3 P 1)=1.5010770 (50). The experimental results are in moderate agreement with theoretical calculations.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-0533
    Keywords: Key words Hereditary neuropathy with liability to ; pressure palsy ; Charcot-Marie-Tooth disease type 1 ; Peripheral myelin protein 22 ; Archival nerve biopsies ; Quantitative polymerase chain reaction
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Chromosomal imbalance of the peripheral myelin protein-22 gene (PMP22) is known to be the most frequent genetic abnormality in Charcot-Marie-Tooth disease type 1 (CMT1) and hereditary neuropathy with liability to pressure palsy (HNPP). We applied a new quantitative PCR method, the direct-double-differential PCR (dddPCR), to the gene dosage determination of PMP22. The method allows the quantification of the PMP22 gene copy number independently from DNA fragmentation, even in highly degraded DNA from up to 12-year-old sural nerve biopsy samples. Chromosomal imbalance of the PMP22 gene, which had been detected by examination of four microsatellites located directly adjacent to the PMP22 gene, between the CMT1A-repetition (CMT1A-REP) elements was reliably confirmed by the dddPCR. Using this method we unexpectedly identified two cases with PMP22 imbalance, although morphologically the neuropathies were of a neuronal or axonal type and not of a demyelinating type as usual. One sural nerve biopsy was from a 58-year-old male diabetes mellitus patient with a disproportionately severe polyneuropathy showing a heterozygous duplication of PMP22. The second biopsy exhibiting a heterozygous deletion of PMP22 was from a 58-year-old female patient with a more axonal than demyelinating type of neuropathy without typical tomaculous changes seemingly altered by exogenous, possibly traumatic factors other than diabetes mellitus. Thus, the dddPCR provides a fast and reliable diagnostic tool for the screening and identification of CMT1A and HNPP cases, which is fast and may be essential even when nerve biopsies show morphologically atypical changes.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
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    In:  EPIC3Geophysical Research Letters, 28(15), pp. 2927-2930, ISSN: 0094-8276
    Publication Date: 2019-07-16
    Description: The importance of deep and bottom water formed in the Southern Ocean to the ventilation of theworld ocean abyss has been accepted by the oceanographic community. Uncertainties, however,exist about rate and exact location of dense water mass sinking around Antarctica. Based on watermass analysis, the Weddell Sea in the Atlantic sector has long been identified as being the majorsource for bottom water. The contribution of the Ross Sea in the western Pacific sector, althoughwith similar if not more favorable ingredients for dense bottom water formation, seemed to be minor.Observations and recent tracer analysis indicate that the Indian-Pacific sector might host sourceswhich together can compete with their Atlantic counterpart. Our numerical model results support asplitting of the Atlantic and Indian-Pacific contributions into roughly equal parts but for bottomwaters of different density. The observationally derived formation rate for dense Antarctic BottomWater on the order of 10 Sv (1 Sv = 10^6 m^3/s) is confirmed but doubles if the lighter componentof the Indian-Pacific sector is included. This places southern and northern hemisphere sources asequal contributors to the ventilation of the world ocean.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
    Publication Date: 2019-07-17
    Description: The Antarctic Circumpolar Wave is now a well-known feature that can bedetected in atmospheric, oceanic mixed layer, and sea ice data. Inour coupled ice-ocean model driven by 40 years of daily atmosphericforcing data it represents a significant part of the interannualvariability, linking the sea ice and water mass formation processes inthe Weddell Sea with other areas in the Antarctic water ring. Inaddition our model results show a decadal-period wavelike anomalypattern near the coast of Antarctica, propagating westward at about 2cm/s. This coastally trapped, bottom-intensified phenomenonseems to have important effects on the dense water formation rate inthe Weddell Sea and even the occurrence of the Weddell polynya.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 6
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    In:  EPIC3Exchanges : newsletter of the Climate Variability and Predictability Programme (CLIVAR), 6(4). {http://www.clivar.org/publications/exchanges/ex22/ex22.pdf}, 28
    Publication Date: 2019-07-16
    Description: Recent numerical model results focussed on the Southern Ocean meridionaloverturning support the observationally derived formation rate of denseAntarctic Bottom Water (AABW) of the order of 10 Sv, mainly confined tothe Atlantic sector of the Southern Ocean. The numerically derived ratedoubles if a slightly lighter component of the Indian-Pacific (IP) sector isincluded, supporting the hypothesis that the sources in the southern andnorthern hemisphere contribute equally to the ventilation of the worldocean abyss. Most of the estimates based on observations, however,repesent long-term means which do not reflect the seasonal andinterannual variability inherent to the bottom water formation process.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev
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  • 7
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 8
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 9
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    In:  EPIC3Antarctic Science, 15(1), pp. 41-46
    Publication Date: 2019-07-16
    Description: In certain regions of the Southern Ocean, tidal energy is believed to foster the mixing of differentwater masses, which eventually contribute to the formation of deep and bottom waters. The RossSea is one of the major ventilation sites of the global ocean abyss and a region of sparse tidalobservations. We investigated tidal dynamics in the Ross Sea using a three-dimensional sigmacoordinate model, the Regional Ocean Model Systems (ROMS). Realistic topography andhydrography from existing observational data were used with a single tidal constituent, thesemi-diurnal M2. The model fields faithfully reproduced the major features of the tidal circulationand had reasonable agreement with ten existing tidal elevation observations and forty-twoexisting tidal current measurements. The differences were attributed primarily to topographic errors.Internal tides were generated at the continental shelf/slope break and other areas of steeptopography. Strong vertical shears in the horizontal velocities occurred under and at the edges ofthe Ross Ice Shelf and along the continental shelf/slope break. Estimates of lead formation basedon divergence of baroclinic velocities were significantly higher than those based on barotropicvelocities, reaching over 10% at the continental shelf/slope break.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 10
    Publication Date: 2019-07-17
    Description: Within the high nutrient --- low chlorophyll regime of the Antarctic Circumpolar Current (ACC), high phytoplankton concentrations are frequently observed in the vicinity of the Antarctic Polar Front (APF).As is typical for frontal systems, hydrography in this region is characterized by meanders and eddies as well as up- and downwelling cells which redistribute nutrients and influence the depth of the euphotic zone.To study the processes leading to the observed phytoplankton distribution, a coupled ocean plankton model for ecosystem studies in the ACC has been developed.The ocean component is an eddy-resolving version of the s-Coordinate Primitive Equation Model (SPEM).The model has a horizontal resolution of 1/12$^\circ$ and a vertical resolution increased near the surface.The biological model (BIMAP) comprises two biogeochemical cycles - silica and nitrogen - and a prognostic iron compartment to include possible effects of micronutrient limitation.Model results indicate that part of the ecosystem's regionalvariability can be attributed to the effect of vertical and horizontal advection.However, frontal dynamics alone cannot explain the observed enhanced concentrations of phytoplankton biomass near the APF and the minima in the northern and southern ACC.Simulations which neglect possible effects of iron limitation cannot reproduce the observed large scale phytoplankton distribution.Only when iron limitation is taken into account, the model simulates plankton concentrations in close agreement with observations during the SO-JGOFS cruises.While in the northern ACC phytoplankton growth is limited by silicate, primary production is limited by iron limitation south of the APF.Near the APF, mesoscale iron upwelling enhances primary production, leading to increased phyto- and zooplankton biomass.The meridional structure with two plankton maxima is closely linked to the cross-front overturning circulation.This double-cell circulation with two upwelling branches is caused by the northward sloping large scale bottom topography.keywords: Antarctic Polar Front, ocean-plankton model, phytoplankton distribution, iron limitation
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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