Corpus juris militaris recognitum, ac multis ex partibus auctum; oder, Neuverbessertes und vermehrtes Kriegs-Recht, worinnen enthalten der Käysere Maximiliani II, und Ferdinandi III : höchstlöblichsten andenckens articuls-Brieffe mit 33. articuln auss Caroli V. Peinlichen Hals-Gerichts Ordnung gezogen, so dann Lud. XIII. Kön. in Franckreich Krigs-ordinance, königl. schwed. und Kön. dannemärckisches, köngl. polnisches und churf. brandenburgisches Krieges-Recht und Articuls-Brieff; nebenst dem holländischen und schweitzerischen Kriegs-Recht,

Mode of access: Internet.

Fact sheet : update on the 33 imprisoned and exiled members of the Soviet Helsinski groups /

Mode of access: Internet.

Selected chapters (1 and 24 to 33 of book 2) of Sir William Blackstone's commentaries on the laws of England ; together with Extracts from Darlington on personal property and Selected cases on fixtures /

"For the use of the students in the School of Law."

Essai sur les cryptogames des écorees exotiques officinales, précédé d'une Méthode lichénographique, et d'un Genera, avec des considérations sur la reproduction des agames; orné de 33 planches coloriées, donnant plus de 130 figures de plantes cryptogames nouvelles; dédié à l'Académie royale de médecine,

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.

Fragm. lat. I 47 - Homeliae I 2; I 5 (CC 122,7 Z. 5 - 8 Z. 50; Mt 1,23 - 25; CC 122,32 Z. 1 - 33 Z. 39)

Trägerband: Inc. qu. 1231; Vorbesitzer: Dominikanerkloster Frankfurt am Main