Renewal of Religious Leadership According to an Ancient Model. Bishop Joseph Hubert Reinkens and Bishop Martin of Tours

Im Jahr 1866 verfasste der damals in Breslau lehrende römisch-katholische Kirchenhistoriker Joseph Hubert Reinkens eine der ersten historisch-kritischen Studien in deutscher Sprache über Martin von Tours, in der er sich u.a. mit Martins bischöflichem Leitungsdienst befasste. Nach dem Ersten Vatikanischen Konzil (1870) wurde Reinkens 1873 der erste Bischof für die Alt-Katholiken im Deutschen Reich. Der Beitrag beschreibt den Einfluss, den Reinkens' Martin-Rezeption auf sein theologisches und praktisches Verständnis des Bischofsamts hatte.

Notizen aus Dernschwams Tagebuch einer Reise nach Konstantinopel (1533/55)

Nathan Porges

Ausst. 322 - Ablaßbrief zum Besten des Dominikanerordens. Mainz, 25.VII.1481

Vorbesitzer: Agnes Bucheler[in]; Margarete Bucheler[in]; Magdalene Bucheler[in]

Girolamo Frescobalid, Brustbild

Signatur des Originals: S 36/F00471

Girolamo Frescobaldi, Brustbild

Signatur des Originals: S 36/G00852

Girolamo Frescobaldi, Brustbild

Signatur des Originals: S 36/G00853

Anna Bishop, Kniestück

Signatur des Originals: S 36/G02820

Girolamo Crescentini, Brustbild

Signatur des Originals: S 36/G02920

Girolamo Crescentini, Brustbild

Signatur des Originals: S 36/G02921

Girolamo Frescobaldi, Brustbild

Signatur des Originals: S 36/G03031

Inc. fragm. Löw. I - Prognosticatio auf das Jahr 1481, lat.

Vorbesitzer: Dominikanerkloster Frankfurt am Main;

Horizontal profiles of longwave and shortwave radiation components over sea ice near Barrow, Alaska during the 2011 melt

An integrated instrument package for measuring and understanding the surface radiation budget of sea ice is presented, along with results from its first deployment. The setup simultaneously measures broadband fluxes of upwelling and downwelling terrestrial and solar radiation (four components separately), spectral fluxes of incident and reflected solar radiation, and supporting data such as air temperature and humidity, surface temperature, and location (GPS), in addition to photographing the sky and observed surface during each measurement. The instruments are mounted on a small sled, allowing measurements of the radiation budget to be made at many locations in the study area to see the effect of small-scale surface processes on the large-scale radiation budget. Such observations have many applications, from calibration and validation of remote sensing products to improving our understanding of surface processes that affect atmosphere-snow-ice interactions and drive feedbacks, ultimately leading to the potential to improve climate modelling of ice-covered regions of the ocean. The photographs, spectral data, and other observations allow for improved analysis of the broadband data. An example of this is shown by using the observations made during a partly cloudy day, which show erratic variations due to passing clouds, and creating a careful estimate of what the radiation budget along the observed line would have been under uniform sky conditions, clear or overcast. Other data from the setup's first deployment, in June 2011 on fast ice near Point Barrow, Alaska, are also shown; these illustrate the rapid changes of the radiation budget during a cold period that led to refreezing and new snow well into the melt season.