Direct support and general support maintenance repair parts and special tools list for transmitter, radio T-1428/FRN (NSN 5895-01-099-3576), tuner, radio frequency TN-588/FRN (NSN 5895-01-107-2124), switching unit, power transfer ....

"5 July 1983."

Organizational maintenance repair parts and special tools list for transmitter, radio T-1428/FRN (NSN 5895-01-099-3576), tuner, radio frequency TN-588/FRN (NSN 5895-01-107-2124), switching unit, power transfer ....

"5 July 1983."

Organizational and direct support maintenance manual : aiming light, infrared AN/PAQ-4 (NSN 5855-01-107-5925).

"21 October 1981."

Organizational and direct support maintenance repair parts and special tools list for aiming light, infrared AN/PAQ-4 (NSN 5855-01-107-5925).

"23 October 1981."

Glee clubbers with Welsh girls, #107

23770

Symphony no. 5, D major (Reformation) op. 107.

Mode of access: Internet.

Particle size of Saharan dust in the Atlantic Ocean, from October 2012 to November 2013

Mineral dust has a large impact on regional and global climate, depending on its particle size. Especially in the Atlantic Ocean downwind of the Sahara, the largest dust source on earth, the effects can be substantial but are poorly understood. This study focuses on seasonal and spatial variations in particle size of Saharan dust deposition across the Atlantic Ocean, using an array of submarine sediment traps moored along a transect at 12° N. We show that the particle size decreases downwind with increased distance from the Saharan source, due to higher gravitational settling velocities of coarse particles in the atmosphere. Modal grain sizes vary between 4 and 33 µm throughout the different seasons and at five locations along the transect. This is much coarser than previously suggested and incorporated into climate models. In addition, seasonal changes are prominent, with coarser dust in summer, and finer dust in winter and spring. Such seasonal changes are caused by transport at higher altitudes and at greater wind velocities during summer than in winter. Also the latitudinal migration of the dust cloud, associated with the Intertropical Convergence Zone, causes seasonal differences in deposition as the summer dust cloud is located more to the north, and more directly above the sampled transect. Furthermore, increased precipitation and more frequent dust storms in summer coincide with coarser dust deposition. Our findings contribute to understanding Saharan dust transport and deposition relevant for the interpretation of sedimentary records for climate reconstructions, as well as for global and regional models for improved prediction of future climate.

Na 1 Nachlass Max Horkheimer, 804 - "Dialektik der Aufklärung" von Max Horkheimer und Theodor W. Adorno (p. XI 6.107 - XI 6.112)

107. - 110. Sammlung D: aus den "Aufzeichnungen"; englische Übersetzungen; 107. "Man and Animal":; 107a) Typoskript mit eigenen Korrekturen, 4 Blatt; 107b) Typoskript mit eigenen Korrekturen, 4 Blatt; 108. "Propaganda":; 108a) Typoskript, 2 Blatt; 108b) Typoskript mit eigenen Korrekturen, 2 Blatt; 109. "Philosophy and the Division of Labor". Typoskript mit eigenen Korrekturen, 3 Blatt; 110. ["Gezeichnet"]. Typoskript, 1 Blatt; 111. Buch-Prospekt zur "Dialektik der Aufklärung":; 111a) Typoskript, 3 Blatt; 111b) Typoskript, 3 Blatt; 111c) Typoskript mit handschriftlichen Korrekturen, 3 Blatt; 112. Zur "Dialektik der Aufklärung": Stichwörter für eine Kartei. 2 Blatt;

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

(Table 2, Page 106-107) Composition of the HCl-soluble fraction in Barents Sea iron-manganese deposits

Ferromanganese concretions from ten stations in the Barents Sea have been analysed for 24 elements. The deposits occur as discoidal and flat concretions and as coatings, in the latter case on lithified or detrital material or as extensive pavements on the Svalbard shelf. The concretions are compositionally similar to Baltic concretions but differ considerably from deep-ocean nodules, particularly in Cu, Ni and Co contents. Statistical analyses reveal distinct correlations between Mn, Na, Ba, Ni and Cu; the Mn-rich coatings showed enrichment of Mo, Zn and possibly Co in a Mn-phase. The iron phase holds high concretions of P and As. Two iron-rich concretions with high contents of P, Ca, Sr, Y, Yb and La were found east and northeast of Spitsbergen Banken, probably indicating upwelling of nutrient-rich, cold polar water along the Svalbard shelf.