Description historique et chronologique des monnaies de la République romaine vulgairement appelées monnaies consulaires /

A supplement to the original work was issued by M. Bahrfeldt under title: Nachträge und Berichtigungen zur Münzkunde der römischen Republik ... Wien, 1897-1900.

Soupis památek historických a uměleckých v Královstvi českém od pravěku do polovice XIX. stoleti.

A German translation was also issued with the title Topographie der historischen und kunstge-schichtlichen Denkmale in der Tschechoslowakischen Republik.

Nordische Reisen und Forschungen /

Vols. 7-10 and 12 are reprints. Vol. 7 has imprint: Bloomington : Indiana University, 1966. Vols. 8-10 and 12 have added imprint: Leipzig : Zentralantiquariat der Deutschen Demokratischen Republik, 1969.

Römische Geschichte,

1. Bd. Römische Geschichte im Zeitalter der Könige.--2. Bd. Römische Geschichte im Zeitalte des Kampfs der Stände. 1. Hälfte. Von der Gründung der Republik bis zum Decemvirat. 2. Hälfte. Vom ersten Decemvirat bis zu den licinischen Gesetzen. Nach des Verf. Tod hrsg. von F. F. Baur.

Srpska biblijografija za noviju književnost, 1741-1867 /

"Unveränd. fotomech. Nachdruck d. Originalausg., Zentralantiquariat der Deutschen Demokratischen Republik, Leipzig, 1967.

Nowaja Semlä in geographischer, naturhistorischer und volkswirthschaftlicher beziehung.

With this is bound: Fritsch, K. W. G. Reisebilder von den Canarischen inseln; Payer, Julius. Die westlichen Ortler-Alpen; Jeppe, Friedrich. Die Transvaal'sche oder Süd-Afrikanische republik-beschrieben; Rohlfs, Gerhard. Gerhard Rohlf's reise durch Nord-Afrika vom Mittelländischen meere bis zum busen von Guinea 1865 bis 1867 (Pt. 1)

Grammatik der tibetischen Sprache,

Mode of access: Internet.

Grammatik der mongolischen Sprache,

Mode of access: Internet.

Zeitschrift für Urologie und Nephrologie : organ der Gesellschaft für Urologie der DDR und der Gesellschaft für Nephrologie der DDR.

Title from cover.

Der Mai-Aufstand in Dresden : auszugsweise bearbeitet nach officiellen Quellen

Boberach: Behandelt werden die Straßenkämpfe, die bei einem Sieg der Revolutionäre zur roten Republik geführt hätten, die Dislokation der Truppen und die Unterdrückung der revolutionären Bewegung in Meißen, Freiberg und Zwickau. - Welsch (Projektbearbeiter): Der Verfasser war während des Aufstandes Adjutant des Kommandierenden Generals

Intertextualität und Vergangenheitsarbeit in Judith Hermanns ‚Sommerhaus, später‘

Dieser Beitrag versteht sich als Gegendarstellung zur verbreiteten Einschätzung von Judith Hermann als einer oberflächlichen Lifestyle-Autorin, die eine Auseinandersetzung mit sozio-historischen Zusammenhängen scheut. Es wird gezeigt, wie Hermann sich in deutsche Vergangenheitsdiskurse einschreibt und mithilfe einer komplexen Intertextualität eine deutsche Traditionslinie männlich-hegemonialer und antisemitischer Strukturen vom Kaiserreich über die NS-Zeit zur Berliner Republik nachzeichnet. Hermann demonstriert die Schwierigkeit einer sinnstiftenden Auseinandersetzung mit der deutschen Vergangenheit angesichts der selektiven Tradierung von Erinnerung und des andauernden privaten Schweigens auf Täterseite. Die daraus resultierenden Prozesse der diffizilen Identitätssuche im Nachwende-Deutschland umschreibt die Autorin durch den Einsatz einer polyvalenten Wassermetaphorik, welche die von der Fiktionalisierung der Vergangenheit geprägte Berliner Republik als ein terrain vague historischer und textueller Entwurzelung charakterisiert, das von der Abwesenheit gültiger Deutungsangebote geprägt ist. Durch diese Bewertung der deutschen Historizität heben sich Hermanns Erzählungen sowohl von der Nachkriegsliteratur als auch von den Werken anderer Gegenwartsautoren ab und nehmen im Kontext literarischer Vergangenheitsbewältigung eine noch unerforschte Sonderstellung ein.

The relationship between educational placement, instructional practices, and achievement gains of Black students with specific learning disabilities in secondary urban school settings

Black students, in general, are underserved academically (Darling-Hammond, 2000; Townsend, 2002) and overrepresented in special education (Donovan & Cross, 2002). Black students with disabilities are further overrepresented in more restrictive educational environments (Skiba, Poloni-Staudinger, Gallini, Simmons & Feggins-Azziz, 2006). Although the National Longitudinal Transition Study 2 (NLTS2) revealed that the academic performance of students with learning disabilities is positively related to the percentage of courses taken in the general education setting (Newman, 2006), the research specifically on placement of Black students with disabilities, particularly at the secondary level, as it relates to academic achievement is lacking. While previous studies have sought to determine which placement is better for students with disabilities, no study was found that specifically examined the impact of placement specific to Black students with specific learning disabilities (SLD) in urban settings (Fore, III, Hagan-Burke, Burke, Boon & Smith, 2008; Rea, McLaughlin & Walther-Thomas, 2002). This study examined educational placement, instructional best practices, and achievement gains of Black students with SLD in urban secondary settings using an ex post facto research design. Achievement, placement, and demographic data were collected and analyzed on approximately 314 Black eighth grade students with SLD. The Teacher Instructional Practices Survey was developed and used to collect and analyze data from the teachers of 78 of these students as it relates to instructional best practices. Results indicate no significant difference in reading but a significant difference in math gains of students served in inclusive settings as compared to resource settings with a small effect size. Also, no significant relationship was found between achievement gains and the reported use of instructional best practices. However, there was a relationship between educational placement and the use of instructional best practices. The results implied that there is a need for training with both general and special education teachers on instructional best practices for SWD and that there should be certain IEP team considerations when making placement decisions for this population of students with disabilities. It is recommended that future research in this area include classroom observations and factors other than test scores to measure growth in achievement.

Radiation fluxes, soil heat flux, air temperature, soil temperature, soil moisture and vegetation at dwarf shrubs and wet sedges in Kytalyk, NE Siberia

Vegetation changes, such as shrub encroachment and wetland expansion, have been observed in many Arctic tundra regions. These changes feed back to permafrost and climate. Permafrost can be protected by soil shading through vegetation as it reduces the amount of solar energy available for thawing. Regional climate can be affected by a reduction in surface albedo as more energy is available for atmospheric and soil heating. Here, we compared the shortwave radiation budget of two common Arctic tundra vegetation types dominated by dwarf shrubs (Betula nana) and wet sedges (Eriophorum angustifolium) in North-East Siberia. We measured time series of the shortwave and longwave radiation budget above the canopy and transmitted radiation below the canopy. Additionally, we quantified soil temperature and heat flux as well as active layer thickness. The mean growing season albedo of dwarf shrubs was 0.15 ± 0.01, for sedges it was higher (0.17 ± 0.02). Dwarf shrub transmittance was 0.36 ± 0.07 on average, and sedge transmittance was 0.28 ± 0.08. The standing dead leaves contributed strongly to the soil shading of wet sedges. Despite a lower albedo and less soil shading, the soil below dwarf shrubs conducted less heat resulting in a 17 cm shallower active layer as compared to sedges. This result was supported by additional, spatially distributed measurements of both vegetation types. Clouds were a major influencing factor for albedo and transmittance, particularly in sedge vegetation. Cloud cover reduced the albedo by 0.01 in dwarf shrubs and by 0.03 in sedges, while transmittance was increased by 0.08 and 0.10 in dwarf shrubs and sedges, respectively. Our results suggest that the observed deeper active layer below wet sedges is not primarily a result of the summer canopy radiation budget. Soil properties, such as soil albedo, moisture, and thermal conductivity, may be more influential, at least in our comparison between dwarf shrub vegetation on relatively dry patches and sedge vegetation with higher soil moisture.

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).

First-year and second-year snow properties on sea ice in the Weddell Sea during POLARSTERN cruise ANT-XXII/2 (ISPOL) during the drift

Observations of snow properties, superimposed ice, and atmospheric heat fluxes have been performed on first-year and second-year sea ice in the western Weddell Sea, Antarctica. Snow in this region is particular as it does usually survive summer ablation. Measurements were performed during Ice Station Polarstern (ISPOL), a 5-week drift station of the German icebreaker RV Polarstern. Net heat flux to the snowpack was 8 W/m**2, causing only 0.1 to 0.2 m of thinning of both snow cover types, thinner first-year and thicker second-year snow. Snow thinning was dominated by compaction and evaporation, whereas melt was of minor importance and occurred only internally at or close to the surface. Characteristic differences between snow on first-year and second-year ice were found in snow thickness, temperature, and stratigraphy. Snow on second-year ice was thicker, colder, denser, and more layered than on first-year ice. Metamorphism and ablation, and thus mass balance, were similar between both regimes, because they depend more on surface heat fluxes and less on underground properties. Ice freeboard was mostly negative, but flooding occurred mainly on first-year ice. Snow and ice interface temperature did not reach the melting point during the observation period. Nevertheless, formation of discontinuous superimposed ice was observed. Color tracer experiments suggest considerable meltwater percolation within the snow, despite below-melting temperatures of lower layers. Strong meridional gradients of snow and sea-ice properties were found in this region. They suggest similar gradients in atmospheric and oceanographic conditions and implicate their importance for melt processes and the location of the summer ice edge.