Historiettes; or, Tales of continental life.

v. 1. The regicide's family. A week at Tours.--v. 2. The fall of Bern.--v. 3. The German lottery. The Rhine. The castle of the Convent lake. L'envoi.

The Yellowplush papers /

Spine title: Yellowplush papers; Jeames' diary.

Burlesques.

v.1. Novels by eminent hands. The diary of C. Jeames de la Pluche, esq., with his letters. The tremendous adventures of Major Gahagan. The fatal boots. Little travels and roadside sketches.--v.2. Rebecca and Rowena. The history of the next French Revolution. Cox's diary. The Bedford-Row conspiracy. A little dinner at Timmins's. A legend of the Rhine.

Die rheinpreussischen landrechte.

No more published.

An Introduction to the art of fortification, containing draughts of all the common works used in military architecture, and of the machines and utensils necessary either in attacks or defences : also a military dictionary, wherein the said works and machines are not only more fully described, but all other technical terms and phrases made use of in the science of war are distictly [sic] explained.

A separate issue of the title appended to The theatre of the present war in the Netherlands and upon the Rhine (London : J. Brindley, 1745).

[Bulwer's novels] /

"Limited to one thousand copies"--on t.p. verso of each v.

(John L. Stoddard's) lectures; illustrated and embellished with views of the world's famous places and people ...

v. 1. Norway. Switzerland. Athens. Venice.--v. 2. Constantinople. Jerusalem. Egypt.--v. 3. Japan (two lectures) China.--v. 4. India (two lectures) The passion play.--v. 5. Paris. La belle France. Spain.--v. 6. Berlin. Vienna. St. Petersburg. Moscow.--v. 7. The Rhine. Belgium. Holland. Mexico.--v. 8. Florence. Naples. Rome.--v. 9. Scotland. England. London.--v. 10. Southern California. Grand Cañon of the Colorado river. Yellowstone national park.

Album of songs : for high voice /

For voice and piano.

Miscellanies : prose & verse.

v. 1 Great Hoggarty diamond; Book of snobs.--v. 2 Kickleburys abroad; Legend of the Rhine; Rebecca & Rowena; Second funeral of Napoleon; Chronicle of the drum.--v. 3 Tremendous adventures of Major Gahagan; Fatal boots; Ballads.--v. 4 Memoirs of Mr. Charles J. Yellowplush; Diary of C. Jeames de la Pluche, Esq.; Cox's diary.--v. 5 Sketches & travels in London; Novels by eminent hands; Character sketches.--v. 6 Memoirs of Barry Lyndon, Esq.--v. 7 Little dinner at Timmins's; Bedford-row conspiracy; Fitz-Boodle papers; Shabby genteel story.--v. 8 Men's wives.

Bulwer Lytton's novels.

Binder's title. Set arbitrarily numbered.

Der Archivar.

"Mitteilungsblatt für deutsches Archivwesen."

Convulsive ergotism: epidemics of the serotonin syndrome?

Between 1085 and 1927, epidemics of convulsive ergotism were widespread east of the Rhine in Europe due to consumption of grain contaminated with ergot, which is produced by the fungus Claviceps purpurea. West of the Rhine, consumption of ergot-contaminated food caused epidemics of gangrenous ergotism. The clinical features of convulsive ergotism-muscle twitching and spasms, changes in mental state, hallucinations, sweating, and fever lasting for several weeks-suggest serotonergic overstimulation of the CNS (ie, the serotonin syndrome). The ergot alkaloids are serotonin agonists. Dihydroergotamine binds to serotonin receptors in the dorsal horn of the spinal cord, which is the site of neuropathological changes in convulsive ergotism. Dihydroergotamine given to human beings can cause the serotonin syndrome. Ergots produced by different strains of Claviceps purpurea, and those growing in different soils, may have different ergot alkaloid compositions. An alkaloid, present in high concentrations in ergots from east of the Rhine, may have caused convulsive ergotism at a circulating concentration insufficient to produce peripheral ischaemia. The serotonin syndrome may, therefore, have been a public-health problem long before it was recognised as a complication of modem psychopharmacology.

Multi-year weather data in the remote semi-arid to arid mountain region of the Saharan flank of the Atlas Mountains

In 2001, a weather and climate monitoring network was established along the temperature and aridity gradient between the sub-humid Moroccan High Atlas Mountains and the former end lake of the Middle Drâa in a pre-Saharan environment. The highest Automated Weather Stations (AWS) was installed just below the M'Goun summit at 3850 m, the lowest station Lac Iriki was at 450 m. This network of 13 AWS stations was funded and maintained by the German IMPETUS (BMBF Grant 01LW06001A, North Rhine-Westphalia Grant 313-21200200) project and since 2011 five stations were further maintained by the GERMAN DFG Fennec project (FI 786/3-1), this way some stations of the AWS network provided data for almost 12 years from 2001-2012. Standard meteorological variables such as temperature, humidity, and wind were measured at an altitude of 2 m above ground. Other meteorological variables comprise precipitation, station pressure, solar irradiance, soil temperature at different depths and for high mountain station snow water equivalent. The stations produced data summaries for 5-minute-precipitation-data, 10- or 15-minute-data and a daily summary of all other variables. This network is a unique resource of multi-year weather data in the remote semi-arid to arid mountain region of the Saharan flank of the Atlas Mountains. The network is described in Schulz et al. (2010) and its further continuation until 2012 is briefly discussed in Redl et al. (2015, doi:10.1175/MWR-D-15-0223.1) and Redl et al. (2016, doi:10.1002/2015JD024443).

Results of analysis and model simulation of the bed profiles

Bedforms such as dunes and ripples are ubiquitous in rivers and coastal seas, and commonly described as triangular shapes from which height and length are calculated to estimate hydrodynamic and sediment dynamic parameters. Natural bedforms, however, present a far more complicated morphology; the difference between natural bedform shape and the often assumed triangular shape is usually neglected, and how this may affect the flow is unknown. This study investigates the shapes of natural bedforms and how they influence flow and shear stress, based on four datasets extracted from earlier studies on two rivers (the Rio Paraná in Argentina, and the Lower Rhine in The Netherlands). The most commonly occurring morphological elements are a sinusoidal stoss side made of one segment and a lee side made of two segments, a gently sloping upper lee side and a relatively steep (6 to 21°) slip face. A non-hydrostatic numerical model, set up using Delft3D, served to simulate the flow over fixed bedforms with various morphologies derived from the identified morphological elements. Both shear stress and turbulence increase with increasing slip face angle and are only marginally affected by the dimensions and positions of the upper and lower lee side. The average slip face angle determined from the bed profiles is 14°, over which there is no permanent flow separation. Shear stress and turbulence above natural bedforms are higher than above a flat bed but much lower than over the often assumed 30° lee side angle.

Pollen profile from Wurzacher Becken

Interglacial lacustrine sediments of 0.3-0.6 m thickness are found in the basin of Wurzach over a distance of about 9 km as detected by 5 borings. The interglacial bed is intercalated between lacustrine sediments of Würm (above) and glaciolacustrine sediments of the Younger Riss (below). Most of the Würmian sediments are silty-sandy, calcareous and varved deposits. They were deposited as bottom sediments of a delta, which had formed in the glacial lake filling the Wurzach basin during the Upper Würm. The terminal moraine of the Younger Riss is found in the N and S of the Reed of Wurzach. In the NE it is overlain by sediments of Würm and Holocene age. The pollen bearing part of the new profile represents the last interglacial period (except its earliest phases), the two Lower Würm interstadials, which are equivalents of the Brørup and Odderade interstadial phases, and a third interstadial, the Dürnten, known from other localities in the forelands of the Alps with a forest vegetation, which consisted mainly of spruce and larch trees, and the intercalated stadial phases. These interstadials are different from those described earlier by FILZER, which on the contrary represent cold periods with highly increased reworking of pollen. The equivalents of the Brørup, Odderade and Dürnten interstadials are the "Kiefer-Fichten-Kampfzeit" and part of the "Kiefernzeit mit Fichte" of FILZER. The characteristic series of climatic events known already from a great number of sites scattered all over Europe and again at Wurzach proves that the Riss/Würm- and the Eem interglacial periods are time-equivalents. Differing amounts of Carpinus and Abies at different places in the northern foreland of the Alps are related to the migration history of the two species during the last interglacial period and must not be used to distinguish different types of interglacials (type Zeifen, type Pfefferbichl).