439 resultados para Reinhold
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Reinhold Lewin
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Reinhold Lewin
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von Carl Leonhard Reinhold
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Von Johann Christoph Schwab, Karl Leonhard Reinhold und Johann Heinrich Abicht
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Briefe zwischen Theodor W. Adorno, Gretel Adorno und Max Horkheimer; 1 Brief der Bank of America (Los Angeles) an Theodor W. Adorno, 24.12.1959; 1 Brief von Theodor W. Adorno an Herrn Ratza (Verband der Heimkehrer), 04.11.1959; 1 Brief von Max Horkheimer und Theodor W. Adorno an Herrn Becker (Rechtsanwalt), [1959]; 1 Brief von Hans-Joachim Lieber an Theodor W. Adorno, 06.05.1959; 1 Brief von Theodor W. Adorno an L. Herschel, 25.04.1959; 1 Brief von Theodor W. Adorno an Felix Weil, 25.03.1959; 1 Brief von Reinhold Baer an Max Horkheimer, 22.01.1959; 1 Brief von Theodor W. Adorno an Reinhold Baer, 06.02.1959; 1 Brief von Theodor W. Adorno an Paul Massing, 23.01.1959; 1 anoymer Propagandabrief von I. Maschner; 1 Stellungnahme zum Propagandabrief, 12.11.1960; 1 Brief von Theodor W. Adorno an I. Maschner, 01.12.1960; 1 Brief von Theodor W. Adorno an Hubert Habicht, 11.11.1960; 1 Brief von der Deutschen Forschungsgemeinschaft an die Europäische Verlangsanstalt (Frankfurt a. M.), 05.10.1960; 1 Brief an Theodor W. Adorno von der Europäischen Verlagsanstalt, 12.10.1960; 1 Brief von der Deutschen Forschungsgemeinschaft an Theodor W. Adorno, 09.02.1960; 1 Brief von H.-J. Schüring an Theodor W. Adorno, 28.08.1960; 1 Brief von Theodor W. Adorno an Adolf Allwohn, 27.07.1960; 1 Brief von der Deutschen Kriminologischen Gesellschaft (Buchschlag) an Max Horkheimer, 06.07.1960; 1 Brief von Arno Peters an Theodor W. Adorno, 10.02.1960; 1 Brief von den Literaturfreunden Barranquilla an Theodor W. Adorno, 06.02.1960; 2 Briefe von Siegfried Cohn an den AUFBAU New York, 1959/1960; 1 Brief vom AUFBAU an Werner Siegfried Cohn, [1960]; 1 Brief von Wilhelm Bernsdorf an Theodor W. Adorno, 21.01.1960; 1 Brief von Hans Achinger an Theodor W. Adorno, 11.01.1960;
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von R. Grundemann
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Signatur des Originals: S 36/F09638
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von Reinhold Lewin
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This article presents and technically describes a new field spectro-goniometer system for the ground-based characterization of the surface reflectance anisotropy under natural illumination conditions developed at the Alfred Wegener Institute (AWI). The spectro-goniometer consists of a Manual Transportable Instrument platform for ground-based Spectro-directional observations (ManTIS), and a hyperspectral sensor system. The presented measurement strategy shows that the AWI ManTIS field spectro-goniometer can deliver high quality hemispherical conical reflectance factor (HCRF) measurements with a pointing accuracy of ±6 cm within the constant observation center. The sampling of a ManTIS hemisphere (up to 30° viewing zenith, 360° viewing azimuth) needs approx. 18 min. The developed data processing chain in combination with the software used for the semi-automatic control provides a reliable method to reduce temporal effects during the measurements. The presented visualization and analysis approaches of the HCRF data of an Arctic low growing vegetation showcase prove the high quality of spectro-goniometer measurements. The patented low-cost and lightweight ManTIS instrument platform can be customized for various research needs and is available for purchase.
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ODP Hole 735B located on the Southwest Indian Ridge at 57°E is an in situ sampled long, continuous section of lower oceanic crust. Oxygen isotope compositions of constituent minerals of Leg 176 gabbros have been measured by UV-laser oxygen isotope microprobe. Together with existing data from Leg 118, a complete oxygen isotope profile through the lower oceanic crust has been obtained. Most clinopyroxenes and olivines have normal mantle values of ~5.5 per mil and ~5.2 per mil, respectively, while plagioclases show slight d18O enrichment relative to its mantle value of 6.1per mil. Down-hole variations of Hole 735B gabbro indicate a downward decreasing d18O profile, with a kink at a depth of about 800 m below sea floor. Above this depth, gabbros are depleted in 18O relative to unaltered basalts, while below ~800 m they show nearly unmodified d18O values. Abundant seawater penetration appears to be limited to the upper part of the lower crust at ODP site 735 (~800 m into the gabbroic layer and ~2-2.5 km into the oceanic crust from the top of pillow basalts). Mass balance calculations show that the lower crust formed under this ultra-slow-spreading ridge has an average d18O value of 5.5 per mil. The whole crust at Site 735 has an overall 18O enrichment with d18O values of 6.0 per mil to 7.8 per mil, depending on the possible variation of the d18O values of the upper pillow basalts and sheeted dykes. The apparent difference in oxygen isotope compositions of ocean crusts formed with different spreading rates has important implications on the buffering of ocean water over geological time, as well as on the oxygen recycling between crust and mantle through subduction. The difference of seawater penetration between fast- and slow-spreading ridges could be related to their particular magmatic-tectonic history during the formation and aging of the crust. However, more analyses on continuous sections through oceanic and ophiolitic crust in different tectonic settings are required to derive any predictive models.
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hyDRaCAT Spectral Reflectance Library for tundra provides the surface reflectance data and the bidirectional reflectance distribution function (BRDF) of important Arctic tundra vegetation communities at representative Siberian and Alaskan tundra sites. The aim of this dataset is the hyperspectral and spectro-directional reflectance characterization as basis for the extraction of vegetation parameters, and the normalization of BRDF effects in off-nadir and multi-temporal remote sensing data. The spectroscopic and field spectro-goniometric measurements were undertaken on the YAMAL2011 expedition of representative Siberian vegetation fields and on the North American Arctic Transect NAAT2012 expedition of Alaskan vegetation fields both belonging to the Greening-of-the-Arctic (GOA) program. For the field spectroscopy each 100 m2 vegetation study grid was divided into quadrats of 1 × 1 m. The averaged reflectance of all quadrats represents the spectral reflectance at the scale of the whole grid at the 10 × 10 m scale. For the surface radiometric measurements two GER1500 portable field spectroradiometers (Spectra Vista Corporation, Poughkeepsie, NY, USA) were used. The GER1500 measures radiance across the wavelength range of 350-1,050 nm, with sampling intervals of 1.5 nm and a radiance accuracy of 1.2 × 10**-1 W/cm**2/nm/sr. In order to increase the signal-to-noise ratio, 32 individual measurements were averaged per one target scan. To minimize variations in the target reflectance due to sun zenith angle changes, all measurements at one study location have been performed under similar sun zenith angles and during clear-sky conditions. The field spectrometer measurements were carried out with a GER1500 UV-VIS spectrometer The spectrogoniometer measurements were carried out with a self-designed spectro-goniometer: the Manual Transportable Instrument platform for ground-based Spectro-directional observations (ManTIS, patent publication number: DE 10 2011 117 713.A1). The ManTIS was equipped with the GER1500 spectrometer allowing spectro-directional measurements with up to 30° viewing zenith angle by full 360° viewing azimuth angles. Measurements in central Yamal (Siberia) at the research site 'Vaskiny Dachi' were carried out in the late summer phenological state from August 12 2011 to August 28 2011. All measurements in Alaska along the North South transect on the North Slope were taken between 29 June and 11 July 2012, ensuring that the vegetation was in the same phenological state near peak growing season.