Fragm. lat. VII 90 - De bello Iudaico (L. VII c. 61 - 66)

Trägerband: Q 16/109; Vorbesitzer: Philippus Jacobus Otto

Die Wirkungen des Winters 90/91 an der Riviera

Paul Bräuer

Ms.Ff.F.Stoltze 3. 90 - Brief von Julius Gerlach an Friedrich Stoltze

Reaktion auf Stoltzes Homburg-Gedicht, Schudt, Emanuel Geibel

Ms.Ff.F.Stoltze 3. 594 - Brief von Heinrich Stoltze an Friedrich Stoltze und Marie Stoltze

Arbeitssuche, Abenteuer, Berufspläne

Na 1 Nachlass Max Horkheimer, 594 - Korrespondenzen mit Friedrich (Frederick) Pollock (p. VI 40, 1-260)

2 Briefe zwischen Gilbert Lazerus und Max Horkheimer, 1960; 1 Brief von dem NDR Studio (Berlin) an Max Horkheimer, 05.09.1960; 1 Brief von Frederick Pollock an H. Meng, 19.05.1960; 1 Brief von Max Horkheimer an die University of Chicago, [1960]; 1 Brief von Max Horkheimer an die Hermann Weil Memorial Foundation (New York), 01.04.1960;

Mus Hs 90 - Prometheus und die Oceaniden : Concertouverture

von Ferdinand Hiller

Ms. lat. qu. 90 - [Sammelband in 2 Teilen: Konvolut aus Altem Druck und Handschrift]

Vorbesitzer: Michelangelo Gualandi

Ms. lat. oct. 90 - De imposturis religionum

Vorbesitzer: Staab

Ms. lat. oct. 152 - Quaestiones de sacramentis (Qu. 84 - 90)

Vorbesitzer: Johannes Bartholomaei;

Physical oceanography from the TRACTOR project

Primary Objectives - Describe and quantify the present strength and variability of the circulation and oceanic processes of the Nordic Seas regions using primarily observations of the long term spread of a tracer purposefully released into the Greenland Sea Gyre in 1996. - Improve our understanding of ocean processes critical to the thermaholine circulation in the Nordic Seas regions so as to be able to predict how this region may respond to climate change. - Assess the role of mixing and ageing of water masses on the carbon transport and the role of the thermohaline circulation in carbon storage using water transports and mixing coefficients derived from the tracer distribution. Specific Objectives Perform annual hydrographic, chemical and SF6 tracer surveys into the Nordic regions in order to: - Measure lateral and diapycnal mixing rates in the Greenland Sea Gyre and in the surrounding regions. - Document the depth and rates of convective mixing in the Greenland Sea using the SF6 and the water masses characteristics. - Measure the transit time and transport of water from the Greenland Sea to surrounding seas and outflows. Document processes of water mass transformation and entrainment occurring to water emanating from the central Greenland Sea. - Measure diapycnal mixing rates in the bottom and margins of the Greenland Sea basin using the SF6 signal observed there. Quantify the potential role of bottom boundary-layer mixing in the ventilation of the Greenland Sea Deep Water in absence of deep convection. Monitor the variability of the entrainment of water from the Greenland Sea using time series auto-sampler moorings at strategic positions i.e., sill of the Denmark Strait, Labrador Sea, Jan Mayen fracture zone and Fram Strait. Relate the observed variability of the tracer signal in the outflows to convection events in the Greenland Sea and local wind stress events. Obtain a better description of deepwater overflow and entrainment processes in the Denmark Strait and Faeroe Bank Channel overflows and use these to improve modelling of deepwater overflows. Monitor the tracer invasion into the North Atlantic using opportunistic SF6 measurements from other cruises: we anticipate that a number of oceanographic cruises will take place in the north-east Atlantic and the Labrador Sea. It should be possible to get samples from some cruises for SF6 measurements. Use process models to describe the spread of the tracer to achieve better parameterisation for three-dimensional models. One reason that these are so resistant to prediction is that our best ocean models are as yet some distance from being good enough, to predict climate and climate change.

(Table 1) Activity of strontium-90 in waters of the Northeast Atlantic at the end of 1965 and the beginning of 1966

In 1965-1966 R/V Mikhail Lomonosov conducted studies on concentrations of artificial radioactive products in the Northeast Atlantic. Concentration of strontium-90 at the end of 1965 and the beginning of 1966 was higher than the average level for the ocean and reached about 53 dpm/100 l in the surface layer. The most intense transport of artificial radioactive products out of the Irish Sea was detected in the northern and northeastern directions along the Hebrides and the Orkneys. In addition to radioactive fission products from nuclear weapons tests, radioactive wastes of atomic industrial facilities discharged into the ocean are an important source of radioactive contamination of some regions of the world ocean.

Magnetic properties, grain sizes, XRF Scanner Data of sediment core GeoB9307-3

Geochemical and mineralogical proxies for paleoenvironmental conditions have the underlying assumption that climate variations have an impact on terrestrial weathering conditions. Varying properties of terrigenous sediments deposited at sea are therefore often interpreted in terms of paleoenvironmental change. Also in gravity core GeoB9307-3 (18° 33.99' S, 37° 22.89' E), located off the Zambezi River, environmental changes during Heinrich Stadial 1 (HS 1) and the Younger Dryas (YD) are accompanied by changing properties of the terrigenous sediment fraction. Our study focuses on the relationship of variability in the hydrological system and changes in the magnetic properties, major element geochemistry and granulometry of the sediments. We propose that changes in bulk sedimentary properties concur with environmental change, although not as a direct response of climate driven pedogenic processes. Spatial varying rainfall intensities on a sub-basin scale modify sediment export from different parts of the Zambezi River basin. During humid phases, such as HS 1 and the YD, sediment was mainly exported from the coastal areas, while during more arid phases sediments mirror the hinterland soil and lithological properties and are likely derived from the northern Shire sub-basin. We propose that a de-coupling of sedimentological and organic signals with variable discharge and erosional activity can occur.