Die Jüdische Gemeinde Bonn : Festschrift zur Einweihung ihrer neuen Synagoge am 31. Januar 1879

von Emanuel Schreiber

Aufruf zur Gründung eines "Talmud-Thoravereins" : gerichtet an die am 16. Mai 1878 abgehaltene isr. Generalversammlung zu Fünfkirchen

von A. Kohut

Per le solenni esequie di S. M. Vittorio Emanuele II. celebrate dagl' Israeliti di Ferrara nel tempio maggiore il di 7. Febbrajo 1878

[Verf.[[Elektronische Ressource]] : Benedetto Levi]

The wandering Jew: or the path of Israel through history : a lecture delivered before the Beth-El Congregation, Sunday, June 23d, 1878,

by K. Kohler. Publ. by the Beth-El Congregation

Cantate : Psalm 45 ; [Cantate aus Anlass der Feier der silbernen Hochzeit unseres ... Kaiserpaares ... Franz Joseph I. und ... Elisabeth Amalie Eugenia ; 24te April 1854 - 1879]

[in Musik gesetzt von] J[acob] Bachmann

Das jüdisch-theologische Seminar Fränckelsche Stiftung zu Breslau am Tage seines fünfundzwanzigjährigen Bestehens, den 10. August 1879

im Auftr. d. Curatoriums ...

Moses Mendelssohn und seine Verdienste um das Judenthum : Festrede, geh. bei der Feier d. 150-jähr. Geburtstages Mendelssohn's zu Bonn am 6. Sept. 1879

von Emanuel Schreiber

Bibliotheca geographica Palaestinae : chronologisches Verzeichnis der auf die Geographie des Heiligen Landes bezüglichen Literatur von 333 bis 1878 ; und Versuch einer Cartographie

hrsg. von Reinhold Röhricht

Die karäische Literatur der letzten dreissig Jahre : 1878 - 1908

von Samuel Poznanski

Arctic moisture source for Eurasian snow cover variations in autumn

Eurasian fall snow cover changes have been suggested as a driver for changes in the Arctic Oscillation and might provide a link between sea-ice decline in the Arctic during summer and atmospheric circulation in the following winter. However, the mechanism connecting snow cover in Eurasia to sea-ice decline in autumn is still under debate. Our analysis is based on snow observations from 820 Russian land stations, moisture transport using a Lagrangian approach derived from meteorological re-analyses. We show that declining sea-ice in the Barents and Kara Seas (BKS) acts as moisture source for the enhanced Western Siberian snow depth as a result of changed tropospheric moisture transport. Transient disturbances enter the continent from the BKS region related to anomalies in the planetary wave pattern and move southward along the Ural mountains where they merge into the extension of the Mediterranean storm track.

Herrn und Frau Heinrich Brisbois zur Goldenen Hochzeit : Dienstag den 27. August 1878

Friedrich Stoltze

Signatures of the 2-day wave and sudden stratospheric warmings in Arctic water vapour observed by ground-based microwave radiometry

The ground-based microwave radiometer MIAWARA-C recorded the upper stratospheric and lower mesospheric water vapour distribution continuously from June 2011 to March 2013 above the Arctic station of Sodankylä, Finland (67.4° N, 26.6° E) without major interruptions and offers water vapour profiles with temporal resolution of 1 h for average conditions. The water vapour time series of MIAWARA-C shows strong periodic variations in both summer and winter related to the quasi-2-day wave. Above 0.1 hPa the amplitudes are strongest in summer. The stratospheric wintertime 2-day wave is pronounced for both winters on altitudes below 0.1 hPa and reaches a maximum amplitude of 0.8 ppmv in November 2011. Over the measurement period, the instrument monitored the changes in water vapour linked to two sudden stratospheric warmings in early 2012 and 2013. Based on the water vapour measurements, the descent rate in the vortex after the warmings is 364 m d−1 for 2012 and 315 m d−1 for 2013.

Eine groizame gešichṭe : welche zich in Kališ am 23. juni 1878 tzugeṭragen haṭ

heroisgegeben fom Badḥan in Kališ

Impact of a Reduced Arctic Sea Ice Cover on Ocean and Atmospheric Properties

The Arctic sea ice cover declined over the last few decades and reached a record minimum in 2007, with a slight recovery thereafter. Inspired by this the authors investigate the response of atmospheric and oceanic properties to a 1-yr period of reduced sea ice cover. Two ensembles of equilibrium and transient simulations are produced with the Community Climate System Model. A sea ice change is induced through an albedo change of 1 yr. The sea ice area and thickness recover in both ensembles after 3 and 5 yr, respectively. The sea ice anomaly leads to changes in ocean temperature and salinity to a depth of about 200 m in the Arctic Basin. Further, the salinity and temperature changes in the surface layer trigger a “Great Salinity Anomaly” in the North Atlantic that takes roughly 8 yr to travel across the North Atlantic back to high latitudes. In the atmosphere the changes induced by the sea ice anomaly do not last as long as in the ocean. The response in the transient and equilibrium simulations, while similar overall, differs in specific regional and temporal details. The surface air temperature increases over the Arctic Basin and the anomaly extends through the whole atmospheric column, changing the geopotential height fields and thus the storm tracks. The patterns of warming and thus the position of the geopotential height changes vary in the two ensembles. While the equilibrium simulation shifts the storm tracks to the south over the eastern North Atlantic and Europe, the transient simulation shifts the storm tracks south over the western North Atlantic and North America. The authors propose that the overall reduction in sea ice cover is important for producing ocean anomalies; however, for atmospheric anomalies the regional location of the sea ice anomalies is more important. While observed trends in Arctic sea ice are large and exceed those simulated by comprehensive climate models, there is little evidence based on this particular model that the seasonal loss of sea ice (e.g., as occurred in 2007) would constitute a threshold after which the Arctic would exhibit nonlinear, irreversible, or strongly accelerated sea ice loss. Caution should be exerted when extrapolating short-term trends to future sea ice behavior.