Šeërith Jisrael : of Lotgevallen der Joden in alle werelddeelen, van af de verwoesting des 2. tempels tot het jaar 1770

door Menachem Man ben Salomo Halevi... uit het Joodsch-Duitsch vertaald door L. Goudsmit ... verrijkt door G. I. Polak

Links between atmospheric carbon dioxide, the land carbon reservoir and climate over the past millennium

The stability of terrestrial carbon reservoirs is thought to be closely linked to variations in climate 1, but the magnitude of carbon–climate feedbacks has proved dificult to constrain for both modern 2–4 and millennial 5–13 timescales. Reconstructions of atmospheric CO2 concentrations for the past thousand years have shown fluctuations on multidecadal to centennial timescales 5–7, but the causes of these fluctuations are unclear. Here we report high-resolution carbon isotope measurements of CO2 trapped within the ice of the West Antarctic Ice Sheet Divide ice core for the past 1,000 years. We use a deconvolution approach 14 to show that changes in terrestrial organic carbon stores best explain the observed multidecadal variations in the 13 C of CO2 and in CO2 concentrations from 755 to 1850 CE. If significant long-term carbon emissions came from pre-industrial anthropogenic land-use changes over this interval, the emissions must have been offset by a natural terrestrial sink for 13 C-depleted carbon, such as peatlands. We find that on multidecadal timescales, carbon cycle changes seem to vary with reconstructed regional climate changes. We conclude that climate variability could be an important control of fluctuations in land carbon storage on these timescales.

[Nicht-ärztliches Tagebuch: Januar - Mai 1752]

Handschrift

[Nicht-ärztliches Tagebuch: Juni - Dezember 1752]

Handschrift

An di remišin keisrlichi oich in Germanien und tzu Jerušalajim kiniglichi maiśṭeṭ ... : kunkuluzum fon 7. nowembr ... 1752 ... tzu der zochin Dawid Me'ir Juda ... enṭgegin ... Lib Aizik un Ziskind Zamuel Šṭerin ...

Moše Ben- ... Sendr Broinšwaig

Der Aufstieg des Hauses Rothschild : 1770 - 1830 ; mit 24 Bildtafeln und einem Faksimile

Egon Caesar Conte Corti

Millennial changes in North American wildfire and soil activity over the last glacial cycle

Climate changes in the North Atlantic region during the last glacial cycle were dominated by the slow waxing and waning of the North American ice sheet as well as by intermittent, millennial-scale Dansgaard–Oeschger climate oscillations. However, prior to the last deglaciation, the responses of North American vegetation and biomass burning to these climate variations are uncertain. Ammonium in Greenland ice cores, a product from North American soil emissions and biomass burning events, can help to fill this gap. Here we use continuous, high-resolution measurements of ammonium concentrations between 110,000 to 10,000 years ago from the Greenland NGRIP and GRIP ice cores to reconstruct North American wildfire activity and soil ammonium emissions. We find that on orbital timescales soil emissions increased under warmer climate conditions when vegetation expanded northwards into previously ice-covered areas. For millennial-scale interstadial warm periods during Marine Isotope Stage 3, the fire recurrence rate increased in parallel to the rapid warmings, whereas soil emissions rose more slowly, reflecting slow ice shrinkage and delayed ecosystem changes. We conclude that sudden warming events had little impact on soil ammonium emissions and ammonium transport to Greenland, but did result in a substantial increase in the frequency of North American wildfires.

Newly detected ozone-depleting substances in the atmosphere

Ozone-depleting substances emitted through human activitiescause large-scale damage to the stratospheric ozone layer, and influence global climate. Consequently, the production of many of these substances has been phased out; prominent examples are the chlorofluorocarbons (CFCs), and their intermediate replacements, the hydrochlorofluorocarbons (HCFCs). So far, seven types of CFC and six types of HCFC have been shown to contribute to stratospheric ozone destruction 1,2. Here, we report the detection and quantification of a further three CFCs and one HCFC. We analysed the composition of unpolluted air samples collected in Tasmania between 1978 and 2012, and extracted from deep firn snow in Greenland in 2008, using gas chromatography with mass spectrometric detection. Using the firn data, we show that all four compounds started to emerge in the atmosphere in the 1960s. Two of the compounds continue to accumulate in the atmosphere. We estimate that, before 2012, emissions of all four compounds combined amounted to more than 74,000 tonnes. This is small compared with peak emissions of other CFCs in the 1980s of more than one million tonnes each year 2. However, the reported emissions are clearly contrary to the intentions behind the Montreal Protocol, and raise questions about the sources of these gases.

Nothgedrungene Rechtsbefugte Vorstellung, Beschwehrung und diverses unterthäniges Bitten unser Derer provisionaliter verordneten dreyen Casten-Meistern Contra Beer Löw Isaac und Süßkind Samuel Stern : Ad Decreta de 29. Octobr. 1751 & 7. Jan. und 1. Martii 1752 ; Cum Postscripto

[Jacob Ochs ; Beer Hertz Oppenheimer ; Moyses Benedickt Beyfuß] [[Elektronische Ressource]]