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  • 1
    Book
    Book
    Zur Kinematik eines stochastischen Feldes interner Wellen in einer Scherströmung (1981)
    Kiel : Institut für Meereskunde, Abt. Meeresphysik
    Details Availability
    Type of Medium: Book
    Pages: 117 S , graph. Darst , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 82
    Language: German
    Note: Zugl.: Kiel, Univ., Math.-naturwiss. Fak., Diss., 1981
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  • 2
    Book
    Book
    GATE : CTD data measured on the F.R.G. ships ; shipboard operations, calibration, editing ; technical report (1976)
    Kiel : Inst. für Meereskunde
    Details Availability
    Description / Table of Contents: The primary aim of this report is to inform the interested GATE scientist about the complete procedures of gaining, calibrating and editing the CTD data from the three FRG research vessels involved in GATE. It is thought to be an integral part of the data sets, and will form part of the documentation sent with the data to the data centers. This report was written according to the recommendations given by the US GATE/C-Scale Workshop at Miami, Fl, 19760202 - 19760206. The user of the data should note that in several respects both the instruments and the ship-board procedures were non-standard. This situation led to special routines for editing the data. Attention should also be given to the comments on the data quality. However, the process of data validation is not finished. An investigation about the interconsistency of the C-scale CTD data is presently underway. (MOD)
    Type of Medium: Book
    Pages: 16, [12] Bl , 15 graph. Darst , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 22
    Language: English
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  • 3
    Online Resource
    Online Resource
    GATE : CTD data measured on the F.R.G. ships shipboard operations - calibration - editing : technical report (2017)
    Kiel : Inst. für Meereskunde
    Details Availability
    Type of Medium: Online Resource
    Pages: Online-Ressource , Diagramme
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 22
    URL: https://oceanrep.geomar.de/13685/
    URL: http://dx.doi.org/10.3289/IFM_BER_22
    DOI: 10.3289/IFM_BER_22
    Language: English
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  • 4
    Online Resource
    Online Resource
    Die Ausbreitung der Wassermassen der Banc D'Arguin im Auftriebsgebiet vor der Nordmauretanischen Küste (1973)
    Kiel
    Details Availability
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (108 Seiten = 9 MB) , Illustrationen, Graphen, Karten
    URL: http://oceanrep.geomar.de/46724/
    Language: German
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  • 5
    Online Resource
    Online Resource
    Zur Kinematik eines stochastischen Feldes interner Wellen in einer Scherströmung (2017)
    Kiel : Institut für Meereskunde, Abt. Meeresphysik
    Details Availability
    Type of Medium: Online Resource
    Pages: 117 S , graph. Darst , 30 cm
    Series Statement: Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel 82
    URL: http://oceanrep.geomar.de/20740/
    URL: http://dx.doi.org/10.3289/ifm_ber_82
    DOI: 10.3289/ifm_ber_82
    Language: German
    Note: Also available as printed version , Zugl.: Kiel, Univ., Math.-naturwiss. Fak., Diss., 1981 , Systemvoraussetzungen: Acrobat reader.
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  • 6
    Electronic Resource
    Electronic Resource
    Mutations in the gene encoding c-Abl-binding protein SH3BP2 cause cherubism (2001)
    [s.l.] : Nature Publishing Group
    Nature genetics 28 (2001), S. 125-126 
    Details
    ISSN: 1546-1718
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] Cherubism (MIM 118400) is an autosomal dominant inherited syndrome characterized by excessive bone degradation of the upper and lower jaws followed by development of fibrous tissue masses, which causes a characteristic facial swelling. Here we describe seven mutations in the SH3-binding protein ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/88832
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  • 7
    Electronic Resource
    Electronic Resource
    Two recurrent nonsense mutations and a 4 bp deletion in a quasi-symmetric element in exon 37 of the NF1 gene (1995)
    Springer
    Human genetics 〈Berlin〉 96 (1995), S. 95-98 
    Details
    ISSN: 1432-1203
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Abstract We screened a total of 92 unrelated patients with neurofibromatosis type 1 (NF1) for mutations in exon 37 of the NF1 gene, by using temperature gradient gel electrophoresis. Two novel mutations were found: a 4 bp deletion in a so-called quasi-symmetric element (6789delTTAC) and a recurrent nonsense mutation, which was identified in two unrelated patients, at codon 2264 (C6792A). The independent origin of the latter mutation in two families was confirmed by haplotype analysis. The nonsense mutation and the 4 bp deletion are both predicted to lead to a truncated protein product lacking the Cterminal 20% (aproximately) of its sequence. The occurrence of three independent mutations among 92 NF1 patients at codons 2263–2264 (exon 37) suggests that a specific search for mutations in this area should be undertaken in screening programs for NF1 mutations.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00214193
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  • 8
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    Mixing and entrainment in the Red Sea outflow plume. Part I : plume structure (2010)
    American Meteorological Society
    Details
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2005. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 35 (2005): 569–583, doi:10.1175/JPO2679.1.
    Description: When the salty and heavy water of the Red Sea exits from the Strait of Bab el Mandeb, it continues downslope into the Gulf of Aden mainly along two channels. The 130-km-long “Northern Channel” (NC) is topographically confined and is typically only 5 km wide. In it, the Red Sea plume shows unanticipated patterns of vertical structure, turbulent mixing, and entrainment. Above the seafloor a 25–120-m-thick weakly stratified layer shows little dilution along the channel. Hence this bottom layer undergoes only weak entrainment. In contrast, a 35–285-m-thick interfacial layer shows stronger entrainment and is shown in a companion paper to undergo vigorous turbulent mixing. It is thus the interface that exhibits the bulk of entrainment of the Red Sea plume in the NC. The interfacial layer also carries most of the overall plume transport, increasingly so with downstream distance. The “Southern Channel” (SC) is wider than the NC and is accessed from the latter by a sill about 33 m above the floor of the NC. Entrainment into the bottom layer of the SC is diagnosed to be strong near the entry into the SC such that the near-bottom density and salinity are smaller in the SC than in the NC at the same distance from Bab el Mandeb. In comparison with winter conditions, the authors encountered weaker outflow with shallower equilibration depths during the summer cruise. Bulk Froude numbers computed for the whole plume varied within the range 0.2–1. Local maxima occurred in relatively steep channel sections and coincided with locations of significant entrainment.
    Description: The Red Sea Outflow Experiment was funded by the National Science Foundation under Contracts OCE-9819506 and OCE-9818464. Additional support was provided to the “Climate Process Team Gravity Currents” under OCE-0336799.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 9
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    A regional modeling study of the entraining Mediterranean outflow (2010)
    American Geophysical Union
    Details
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2007. 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 112 (2007): C12005, doi:10.1029/2007JC004145.
    Description: We have evaluated a regional-scale simulation of the Mediterranean outflow by comparison with field data obtained in the 1988 Gulf of Cádiz Expedition. Our ocean model is based upon the Hybrid Coordinate Ocean Model (HYCOM) and includes the Richardson number–dependent entrainment parameterization of Xu et al. (2006). Given realistic topography and sufficient resolution, the model reproduces naturally the major, observed features of the Mediterranean outflow in the Gulf of Cádiz: the downstream evolution of temperature, salinity, and velocity profiles, the mean path and the spreading of the outflow plume, and most importantly, the localized, strong entrainment that has been observed to occur just west of the Strait of Gibraltar. As in all numerical solutions, there is some sensitivity to horizontal and vertical resolution. When the resolution is made coarser, the simulated currents are less vigorous and there is consequently less entrainment. Our Richardson number–dependent entrainment parameterization is therefore not recommended for direct application in coarse-resolution climate models. We have used the high-resolution regional model to investigate the response of the Mediterranean outflow to a change in the freshwater balance over the Mediterranean basin. The results are found in close agreement with the marginal sea boundary condition (MSBC): A more saline and dense Mediterranean deep water generates a significantly greater volume transport of the Mediterranean product water having only very slightly greater salinity.
    Description: National Science Foundation via grant OCE0336799 and the National Ocean Partnership Program (NOPP) via award N000140410676.
    Keywords: Mediterranean outflow ; Entrainment parameterization ; Climate
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 10
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    Equilibration and circulation of Red Sea Outflow water in the western Gulf of Aden (2010)
    American Meteorological Society
    Details
    Publication Date: 2022-05-25
    Description: Author Posting. © American Meteorological Society, 2005. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 35 (2005): 1963–1985, doi:10.1175/JPO2787.1.
    Description: Hydrographic, direct velocity, and subsurface float observations from the 2001 Red Sea Outflow Experiment (REDSOX) are analyzed to investigate the gravitational and dynamical adjustment of the Red Sea Outflow Water (RSOW) where it is injected into the open ocean in the western Gulf of Aden. During the winter REDSOX cruise, when outflow transport was large, several intermediate-depth salinity maxima (product waters) were formed from various bathymetrically confined branches of the outflow plume, ranging in depth from 400 to 800 m and in potential density from 27.0 to 27.5 σθ, a result of different mixing intensity along each branch. The outflow product waters were not dense enough to sink to the seafloor during either the summer or winter REDSOX cruises, but analysis of previous hydrographic and mooring data and results from a one-dimensional plume model suggest that they may be so during wintertime surges of strong outflow currents, or about 20% of the time during winter. Once vertically equilibrated in the Gulf of Aden, the shallowest RSOW was strongly influenced by mesoscale eddies that swept it farther into the gulf. The deeper RSOW was initially more confined by the walls of the Tadjura Rift, but eventually it escaped from the rift and was advected mainly southward along the continental slope. There was no evidence of a continuous boundary undercurrent of RSOW similar to the Mediterranean Undercurrent in the Gulf of Cadiz. This is explained by considering 1) the variability in outflow transport and 2) several different criteria for separation of a jet at a sharp corner, which indicate that the outflow currents should separate from the boundary where they are injected into the gulf.
    Description: This work was supported by the U.S. National Science Foundation under Grants OCE-9818464 (WHOI) and OCE-9819506 (RSMAS).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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