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  • 2010-2014  (40)
  • 2005-2009  (274)
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  • 1
    Digitale Medien
    Digitale Medien
    s.l. ; Stafa-Zurich, Switzerland
    Advances in science and technology Vol. 45 (Oct. 2006), p. 1351-1354 
    ISSN: 1662-0356
    Quelle: Scientific.Net: Materials Science & Technology / Trans Tech Publications Archiv 1984-2008
    Thema: Allgemeine Naturwissenschaft , Technik allgemein
    Notizen: In-situ and ex-situ spectroscopic ellipsometry (SE), atomic force microscopy (AFM),transmission electron microscopy (TEM), and time of flight medium energy backscattering (ToFMEBS), are used to investigate the properties of 30 and 60 Å ZrO2 films deposited at differenttemperatures on hydrogen terminated silicon (H-Si) and native silicon oxide surfaces. Resultsshow that the initial-stage deposition of ZrO2 on H-Si and native silicon oxide surfaces aredifferent. A 3-dimesional (3D) type nucleation process of ZrO2 on H-Si leads to high surfaceroughness films, while layer-by-layer deposition on native silicon oxide surfaces leads tosmooth, uniform ZrO2 films. An interfacial layer, between the substrate and the metal oxide, isformed through two independent mechanisms: reaction between the starting surfaces and ZTB orits decomposition intermediates, and diffusion of reactive oxidants through the forming ZrO2interfacial stack layer to react with the substrate
    Materialart: Digitale Medien
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    facet.materialart.
    Unbekannt
    AGU (American Geophysical Union) | Wiley
    In:  Journal of Geophysical Research: Oceans, 119 (2). pp. 1068-1083.
    Publikationsdatum: 2019-09-23
    Beschreibung: In the tropical eastern South Pacific the Stratus Ocean Reference Station (ORS) (∼20°S, 85.5°W) is located in the transition zone between the oxygen minimum zone (OMZ) and the well-oxygenated subtropical gyre. In February/March 2012, extremely anomalous water mass properties were observed in the thermocline at the Stratus ORS. The available eddy oxygen anomaly was −10.5 × 1016 µmol. This anomalous water was contained in an anticyclonic mode-water eddy crossing the mooring site. This eddy was absorbed at that time by an anticyclonic feature located south of the Stratus mooring. This was the largest water property anomaly observed at the mooring during the 13.5 month deployment period. The sea surface height anomaly (SSHA) of the strong mode-water eddy in February/March 2012 was weak, and while the lowest and highest SSHA were related to weak eddies, SSHA is found not to be sufficient to specify the eddy strength for subsurface-intensified eddies. Still, the anticyclonic eddy, and its related water mass characteristics, could be tracked backward in time in SSHA satellite data to a formation region in April 2011 off the Chilean coast. The resulting mean westward propagation velocity was 5.5 cm s−1. This extremely long-lived eddy carried the water characteristics from the near-coastal Chilean water to the open ocean. The water mass stayed isolated during the 11 month travel time due to high rotational speed of about 20 cm s−1 leading to almost zero oxygen in the subsurface layer of the anticyclonic mode-water eddy with indications of high primary production just below the mixed layer.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 88 (C14). pp. 9689-9705.
    Publikationsdatum: 2019-04-04
    Beschreibung: During the Joint Air-Sea Interaction (JASIN) experiment conducted in the northern Rockall Trough in the summer of 1978, oceanographic moorings with surface buoys carrying wind recorders were deployed in an array designed to investigate the variability of the near-surface wind field at scales of from 2 to 200 km. The wind records together with observations taken on board the research vessels participating in JASIN have provided ground truth measurements for the sea surface wind velocity sensors on the Seasat satellite. During most of the experiment the wind field was characterized by spatial scales large in comparison with the separations between the buoys. On several occasions, spatial differences associated with cold fronts were identified, and it was possible to track the passage of the front through the array. However, quantitative analysis of the variability of the wind field was complicated both by a lack of data due to mechanical failures of some instruments and by significant differences in the performance of the diverse types of wind recorders. Reevaluation of the instruments used in JASIN and recent comparison of some of these instruments with more conventional sets of wind sensors confirm the possibility that there is significant error in the JASIN wind measurements made from the buoys. In particular, the vector-averaging wind recorder on W2, which was one of the few instruments to recover a full length record and which was chosen during a Seasat-JASIN workshop as the JASIN standard, had performance characteristics that were among the most difficult to explain.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    facet.materialart.
    Unbekannt
    Elsevier
    In:  Deep Sea Research Part I: Oceanographic Research Papers, 52 (5). pp. 749-765.
    Publikationsdatum: 2021-03-23
    Beschreibung: Surface meteorology, upper ocean current, and hydrographic measurements, collected along a repeated survey pattern and from a central mooring in the western equatorial Pacific during late 1992 to early 1993, were used to analyse upper ocean momentum balances on the intraseasonal time scale. Wind stresses derived from meteorological measurements were compared with numerical weather prediction products. Advection terms in the momentum equations were estimated by planar fits to the current and hydrographic data. Pressure gradient terms were derived from planar fits to the dynamic heights calculated from the hydrographic data, referenced by balancing the momentum equation in a selected layer below the mixed layer. Under prevailing westerly winds, westward pressure gradient forcings of 2 x 10 -7 ms -2 were set up in the western equatorial Pacific, countering the surface wind, while the total advection tended to accelerate the eastward momentum in the surface layer. During both calm wind and westerly wind burst periods, zonal turbulent momentum fluxes estimated from the ocean budgets were comparable with those estimated from microstructure dissipation rate measurements and with zonal wind stresses, so that the zonal momentum could be balanced within error bars. The meridional momentum balances were noisier, which might be due to the fact that the short meridional length scale of the equatorial inertial-gravity waves could contaminate the dynamic signals in the mixed temporal/spatial sampling data, so that the meridional gradient estimates from the planar fits could be biased.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; Current direction; Current meter, vector measuring; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; VMCM; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 91830 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; Current direction; Current meter, vector measuring; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; VMCM; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 122370 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; Temperature recorder, Brancker; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 23744 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; Current direction; Current meter, vector measuring; Current velocity, east-west; Current velocity, horizontal; Current velocity, north-south; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; VMCM; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 122370 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; Temperature recorder, Brancker; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 23744 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Publikationsdatum: 2023-02-24
    Schlagwort(e): ACM25/26; ACM25/26_Northeast_3; DATE/TIME; DEPTH, water; MOOR; Mooring; Temperature, water; Temperature recorder, Brancker; WOCE; World Ocean Circulation Experiment
    Materialart: Dataset
    Format: text/tab-separated-values, 23744 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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