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Die Struktur moderner Videoclips ist nicht neu. Schon im 16. Jahrhundert versuchte man mit Instrumenten wie dem optischen Cembalo Optisches und Akustisches zu koppeln. Seit über einem halben Jahrhundert versuchen Künstler folglich Bild und Musik zu vereinen. Besonders in den so genannten Konzept-Videos der elektronischen Musik, bei denen Bild und Ton eine Synthese eingehen und die Musik sichtbar gemacht wird, steht der Satz „Ich sehe Musik“ Pate für die Übersetzung der Musik in Bilder. Neben dem Verschwinden des Interpreten aus dem elektronischen Musik-Video ist die Inszenierung von Körperlichkeit ein Thema der Elektroclips – Körper werden häufig in Rückgriff auf die Bilderwelten des Horror- und Rauschfilms visualisiert: dekonstruiert und deformiert. Dies hängt mit den ideologischen Implikationen der elektronischen Musik zusammen, die sich scheinbar am präzisesten innerhalb dieser Bilderwelten artikulieren lassen. Wie dies geschieht, soll hier anhand von Beispielvideos untersucht werden.
Full metal village
(2010)
Im schleswig-holsteinischen Dorf Wacken treffen einmal im Jahr für drei Tage mehr als 40.000 Heavy Metal Fans auf weniger als 1.800 Anwohner. Anlass ist das 1990 gegründete Wacken Open Air Festival (W:O:A), nach eigenem Bekunden das größte Metal-Open-Air-Festival der Welt. Dabei müssen kulturelle Differenzen und Konflikte zwischen Dorfbewohnern und Festivalbesuchern vorprogrammiert sein. Diesen Gedanken verfolgte anfangs auch die 1966 geborene koreanische Regisseurin von FULL METAL VILLAGE, Sung-Hyung Cho. Sie beschloss „aus Mangel an Alternativen“ (Cho), einen Dokumentarfilm zu drehen, der den Aufprall beider Welten darstellen sollte. Doch im weiteren Verlauf der Produktion änderte Cho ihr Konzept und es entstand ein Film, der es vermied, die Kontraste zu überspitzen, sondern der sich vielmehr auf die Dokumentation des Lebens der Dorfbewohner konzentriert – die das Festival fast ausnahmslos nicht als Einbruch einer fremden Subkultur wahrgenommen, sondern sich glänzend in die Durchführung und Realität des Festivals integriert haben.
Die Filme Ghostrider, Knowing und Next entfalten auf jeweils unterschiedliche Art und Weise die Problematik, wie vor einer nicht nur unbekannten, sondern auch sehr ernsthaft bedrohlichen Zukunft Entscheidungen zu treffen sind, die die sie angehenden moralischen Subjekte in ihren Handlungsoptionen allererst konstituieren. Die Formung der dargestellten Entscheidungsszenarien wäre nicht denkbar ohne unterschiedliche Zeitlichkeitsmodelle, deren Bedeutung in einer jedes moralische Subjekt betreffenden Möglichkeit liegt, sich gegen die Gegenwart zu wenden. Mögen die Filme als einzelne trivial oder allenfalls unterhaltsam erscheinen, so lässt sich in ihrer Konstellation zeigen, inwiefern jedes Handeln sich nicht so sehr für die Zukunft, sondern an der Gegenwart entscheidet.
A new, two-channel instrument for simultaneous NO3 and N2O5 monitoring was used to make the first comprehensive set of nocturnal NOx measurements (NO, NO2, NO3 and N2O5) at the Taunus Observatory, a rural mountain site (Kleiner Feldberg) in South-western Germany. In May 2008, NO3 and N2O5 mixing ratios were well above the instrumental detection limit (a few ppt) on all nights of the campaign and were characterised by large variability. The concentrations of NO3, N2O5 and NO2 were consistent with the equilibrium constant, K2, defining the rates of formation and thermal dissociation of N2O5. A steady-state lifetime analysis is consistent with the loss of nocturnal NOx being dominated by the reaction of NO3 with volatile organic compounds in this forested region, with N2O5 uptake to aerosols of secondary importance. Analysis of a limited dataset obtained at high relative humidity indicated that the loss of N2O5 by reaction with water vapour is less efficient (>factor 3) than derived using laboratory kinetic data. The fraction of NOx present as NO3 and N2O5 reached ~20% on some nights, with night-time losses of NOx competing with daytime losses.
Fractional release factors of long-lived halogenated organic compounds in the tropical stratosphere
(2010)
Fractional release factors (FRFs) of organic trace gases are time-independent quantities that influence the calculation of Global Warming Potentials and Ozone Depletion Potentials. We present the first set of vertically resolved FRFs for 15 long-lived halocarbons in the tropical stratosphere up to 34 km altitude. They were calculated from measurements on air samples collected on board balloons and a high altitude aircraft. We compare the derived dependencies of FRFs on the mean stratospheric transit times (the so-called mean ages of air) with similarly derived FRFs originating from measurements at higher latitudes and find significant differences. Moreover a comparison with averaged FRFs currently used by the World Meteorological Organisation revealed the limitations of these measures due to their observed vertical and latitudinal variability. The presented data set could be used to improve future ozone level and climate projections.
We synthesised observations of total particle number (CN) concentration from 36 sites around the world. We found that annual mean CN concentrations are typically 300–2000 cm -3 in the marine boundary layer and free troposphere (FT) and 1000–10 000 cm -3 in the continental boundary layer (BL). Many sites exhibit pronounced seasonality with summer time concentrations a factor of 2–10 greater than wintertime concentrations. We used these CN observations to evaluate primary and secondary sources of particle number in a global aerosol microphysics model. We found that emissions of primary particles can reasonably reproduce the spatial pattern of observed CN concentration (R2=0.46) but fail to explain the observed seasonal cycle (R2=0.1). The modeled CN concentration in the FT was biased low (normalised mean bias, NMB=& -88%) unless a secondary source of particles was included, for example from binary homogeneous nucleation of sulfuric acid and water (NMB= -25%). Simulated CN concentrations in the continental BL were also biased low (NMB= -74%) unless the number emission of anthropogenic primary particles was increased or a mechanism that results in particle formation in the BL was included. We ran a number of simulations where we included an empirical BL nucleation mechanism either using the activation-type mechanism (nucleation rate, J, proportional to gas-phase sulfuric acid concentration to the power one) or kinetic-type mechanism (J proportional to sulfuric acid to the power two) with a range of nucleation coefficients. We found that the seasonal CN cycle observed at continental BL sites was better simulated by BL particle formation (R2=0.3) than by increasing the number emission from primary anthropogenic sources (R2=0.18). The nucleation constants that resulted in best overall match between model and observed CN concentrations were consistent with values derived in previous studies from detailed case studies at individual sites. In our model, kinetic and activation-type nucleation parameterizations gave similar agreement with observed monthly mean CN concentrations.
River flow regimes, including long-term average flows, seasonality, low flows, high flows and other types of flow variability, play an important role for freshwater ecosystems. Thus, climate change affects freshwater ecosystems not only by increased temperatures but also by altered river flow regimes. However, with one exception, transferable quantitative relations between flow alterations and ecological responses have not yet been derived. While discharge decreases are generally considered to be detrimental for ecosystems, the effect of future discharge increases is unclear. As a first step towards a global-scale analysis of climate change impacts on freshwater ecosystems, we quantified the impact of climate change on five ecologically relevant river flow indicators, using the global water model WaterGAP 2.1g to simulate monthly time series of river discharge with a spatial resolution of 0.5 degrees. Four climate change scenarios based on two global climate models and two greenhouse gas emissions scenarios were evaluated. We compared the impact of climate change by the 2050s to the impact of water withdrawals and dams on natural flow regimes that had occurred by 2002. Climate change was computed to alter seasonal flow regimes significantly (i.e. by more than 10%) on 90% of the global land area (excluding Greenland and Antarctica), as compared to only one quarter of the land area that had suffered from significant seasonal flow regime alterations due to dams and water withdrawals. Due to climate change, the timing of the maximum mean monthly river discharge will be shifted by at least one month on one third on the global land area, more often towards earlier months (mainly due to earlier snowmelt). Dams and withdrawals had caused comparable shifts on less than 5% of the land area only. Long-term average annual river discharge is predicted to significantly increase on one half of the land area, and to significantly decrease on one quarter. Dams and withdrawals had led to significant decreases on one sixth of the land area, and nowhere to increases. Thus, by the 2050s, climate change may have impacted ecologically relevant river flow characteristics more strongly than dams and water withdrawals have up to now. The only exception refers to the decrease of the statistical low flow Q90, with significant decreases both by past water withdrawals and future climate change on one quarter of the land area. However, dam impacts are likely underestimated by our study. Considering long-term average river discharge, only a few regions, including Spain, Italy, Iraq, Southern India, Western China, the Australian Murray Darling Basin and the High Plains Aquifer in the USA, all of them with extensive irrigation, are expected to be less affected by climate change than by past anthropogenic flow alterations. In some of these regions, climate change will exacerbate the discharge reductions, while in others climate change provides opportunities for reducing past reductions. Emissions scenario B2 leads to only slightly reduced alterations of river flow regimes as compared to scenario A2 even though emissions are much smaller. The differences in alterations resulting from the two applied climate models are larger than those resulting from the two emissions scenarios. Based on general knowledge about ecosystem responses to flow alterations and data related to flow alterations by dams and water withdrawals, we expect that the computed climate change induced river flow alterations will impact freshwater ecosystems more strongly than past anthropogenic alterations.
This paper investigates the potential impact of secondary information on rainfall mapping applying Ordinary Kriging. Secondary information tested is a natural area indicator, which is a combination of topographic features and weather conditions. Cross validation shows that secondary information only marginally improves the final mapping, indicating that a one-day accumulation time is possibly too short.
Development of a Bioaerosol single particle detector (BIO IN) for the Fast Ice Nucleus CHamber FINCH
(2010)
In this work we present the setup and first tests of our new BIO IN detector. This detector was constructed to classify atmospheric ice nuclei (IN) for their biological content. It is designed to be coupled to the Fast Ice Nucleus CHamber FINCH. If one particle acts as an ice nucleus, it will be at least partly covered with ice at the end of the development section of the FINCH chamber. The device combines an auto-fluorescence detector and a circular depolarization detector for simultaneous detection of biological material and discrimination between water droplets, ice crystals and non activated large aerosol particles. The excitation of biological material with UV light and analysis of auto-fluorescence is a common principle used for flow cytometry, fluorescence microscopy, spectroscopy and imaging. The detection of auto-fluorescence of airborne single particles demands some more experimental effort. However, expensive commercial sensors are available for special purposes, e.g. size distribution measurements. But these sensors will not fit the specifications needed for the FINCH IN counter (e.g. high sample flow of up 10 LPM). The newly developed -low cost- BIO IN sensor uses a single high-power UV LED for the electronic excitation instead of much more expensive UV lasers. Other key advantages of the new sensor are the low weight, compact size, and the little effect on the aerosol sample, which allows it to be coupled with other instruments for further analysis. The instrument will be flown on one of the first missions of the new German research aircraft "HALO" (High Altitude and LOng range).
Processes occurring in the tropical upper troposphere (UT), the Tropical Transition Layer (TTL), and the lower stratosphere (LS) are of importance for the global climate, for stratospheric dynamics and air chemistry, and for their influence on the global distribution of water vapour, trace gases and aerosols. In this contribution we present aerosol and trace gas (in-situ) measurements from the tropical UT/LS over Southern Brazil, Northern Australia, and West Africa. The instruments were operated on board of the Russian high altitude research aircraft M-55 "Geophysica" and the DLR Falcon-20 during the campaigns TROCCINOX (Araçatuba, Brazil, February 2005), SCOUT-O3 (Darwin, Australia, December 2005), and SCOUT-AMMA (Ouagadougou, Burkina Faso, August 2006). The data cover submicron particle number densities and volatility from the COndensation PArticle counting System (COPAS), as well as relevant trace gases like N2O, ozone, and CO. We use these trace gas measurements to place the aerosol data into a broader atmospheric context. Also a juxtaposition of the submicron particle data with previous measurements over Costa Rica and other tropical locations between 1999 and 2007 (NASA DC-8 and NASA WB-57F) is provided. The submicron particle number densities, as a function of altitude, were found to be remarkably constant in the tropical UT/LS altitude band for the two decades after 1987. Thus, a parameterisation suitable for models can be extracted from these measurements. Compared to the average levels in the period between 1987 and 2007 a slight increase of particle abundances was found for 2005/2006 at altitudes with potential temperatures, theta, above 430 K. The origins of this increase are unknown except for increases measured during SCOUT-AMMA. Here the eruption of the Soufrière Hills volcano in the Caribbean caused elevated particle mixing ratios. The vertical profiles from Northern hemispheric mid-latitudes between 1999 and 2006 also are compact enough to derive a parameterisation. The tropical profiles all show a broad maximum of particle mixing ratios (between theta ~ 340 K and 390 K) which extends from below the TTL to above the thermal tropopause. Thus these particles are a "reservoir" for vertical transport into the stratosphere. The ratio of non-volatile particle number density to total particle number density was also measured by COPAS. The vertical profiles of this ratio have a maximum of 50% above 370 K over Australia and West Africa and a pronounced minimum directly below. Without detailed chemical composition measurements a reason for the increase of non-volatile particle fractions cannot yet be given. However, half of the particles from the tropical "reservoir" contain compounds other than sulphuric acid and water. Correlations of the measured aerosol mixing ratios with N2O and ozone exhibit compact relationships for the tropical data from SCOUT-AMMA, TROCCINOX, and SCOUT-O3. Correlations with CO are more scattered probably because of the connection to different pollution source regions. We provide additional data from the long distance transfer flights to the campaign sites in Brazil, Australia, and West-Africa. These were executed during a time window of 17 months within a period of relative volcanic quiescence. Thus the data represent a "snapshot picture" documenting the status of a significant part of the global UT/LS fine aerosol at low concentration levels 15 years after the last major (i.e., the 1991 Mount Pinatubo) eruption. The corresponding latitudinal distributions of the measured particle number densities are presented in this paper to provide data of the UT/LS background aerosol for modelling purposes.
Abrupt climate changes of the last deglaciation detected in a Western Mediterranean forest record
(2010)
Abrupt changes in Western Mediterranean climate during the last deglaciation (20 to 6 cal ka BP) are detected in marine core MD95-2043 (Alboran Sea) through the investigation of high-resolution pollen data and pollen-based climate reconstructions by the modern analogue technique (MAT) for annual precipitation (Pann) and mean temperatures of the coldest and warmest months (MTCO and MTWA). Changes in temperate Mediterranean forest development and composition and MAT reconstructions indicate major climatic shifts with parallel temperature and precipitation changes at the onsets of Heinrich stadial 1 (equivalent to the Oldest Dryas), the Bölling-Allerød (BA), and the Younger Dryas (YD). Multi-centennial-scale oscillations in forest development occurred throughout the BA, YD, and early Holocene. Shifts in vegetation composition and (Pann reconstructions indicate that forest declines occurred during dry, and generally cool, episodes centred at 14.0, 13.3, 12.9, 11.8, 10.7, 10.1, 9.2, 8.3 and 7.4 cal ka BP. The forest record also suggests multiple, low-amplitude Preboreal (PB) climate oscillations, and a marked increase in moisture availability for forest development at the end of the PB at 10.6 cal ka BP. Dry atmospheric conditions in the Western Mediterranean occurred in phase with Lateglacial events of high-latitude cooling including GI-1d (Older Dryas), GI-1b (Intra-Allerød Cold Period) and GS-1 (YD), and during Holocene events associated with high-latitude cooling, meltwater pulses and N. Atlantic ice-rafting. A possible climatic mechanism for the recurrence of dry intervals and an opposed regional precipitation pattern with respect to Western-central Europe relates to the dynamics of the westerlies and the prevalence of atmospheric blocking highs. Comparison of radiocarbon and ice-core ages for well-defined climatic transitions in the forest record suggests possible enhancement of marine reservoir ages in the Alboran Sea by 200 years (surface water age 600 years) during the Lateglacial.
Das Exil war sein Schicksal. Davon ist er zeit seines Lebens nicht losgekommen. Hans Sahl, aus Dresden gebürtig, gehörte zu jenen brillanten Intellektuellen, die bereits im geistigen Leben der Weimarer Republik eine Rolle spielten, vor den Nazis fliehen mußten und als ungeliebte Heimkehrer in der Bundesrepublik lange vergessen blieben. Erst in seinen letzten Lebensjahren, die der fast erblindete Autor in Tübingen verbrachte, wurde er mit Preisen überschüttet, wurden seine Gedichte und Romane neuaufgelegt. “Wir sind die Letzten“, hieß eine Gedichtsammlung, die 1941 erschien, in der sich dieser „Trödler des Unbegreiflichen“, wie er sich nannte, als Moralist und Wahrheitsfanatiker von hohen Graden zu erkennen gab.
“Es ist weder Schwäche noch Minderwertigkeit des Erotischen, wenn es seiner Art nach auf gespanntem Fuß mit der Treue steht, vielmehr bedeutet es an ihm das Abzeichen seines Aufstiegs zu noch weiteren Zusammenhängen. Und darum muß auch da, wo es in solche schon weiter einbezogen wird, ihm von dieser ungenügsamen Sensibilität vieles erhalten bleiben, gerade so, wie es seinerzeit sich nur begründet auf den ursprünglichsten Vorgängen des Organlebens.“ Lou Andreas-Salomé – sie taucht auf zum ersten Mal 1882 als Einundzwanzigjährige, von Nietzsche und seinem Freund Paul Rée gleichermaßen verehrt, geliebt, bewundert. Das Paar Lou/ Nietzsche hat die Phantasie späterer Generationen beflügelt, dieses Zuendedenken und –leben nicht erfüllter Wünsche und Sehnsüchte hat das Kolorit beider Erinnerung wesentlich überzeichnet.
Eines der markantesten Symbole der Advents- und Weihnachtszeit sind die in unterschiedlichsten Farben, Formen und sogar Düften angebotenen Kerzen. Ihr Licht gibt der Jahreszeit eine besondere Atmosphäre, sie unterstützen neben anderen Dekorationsartikeln die erwünschte besinnliche Stimmung. Kerzen stehen traditionell sinnbildlich für Licht, Wärme und Reinheit und symbolisieren damit im Christentum das Lebenslicht des Menschen und Christus als das Licht der Welt. Man könnte nun meinen, dass Kerzen auf den Seiten des Bochumer Botanischen Vereins nichts zu suchen haben, sondern eher dem Bereich Chemie (Stearin) oder Zoologie (Bienenwachs) zugeordnet werden sollten. Aber die Botanik hat auch hier schon immer eine wesentliche Rolle gespielt und steht auch heute noch im wörtlichen Sinne im Zentrum jeder Kerze, denn Wachs brennt ohne sie nicht: die Kerzendochte. Dabei ist die Erfindung des Dochtes weitaus älter als die der Kerzen. Bei den alten Griechen z. B. waren Kerzen noch weitestgehend unbekannt, man verwendete Öllampen, die einen (meist) pflanzlichen Docht enthielten.
Krokusse gehören zu den frühesten Boten des Frühlings. Wenn es im Spätherbst und Winter wärmer ist als gewöhnlich, sprießen schon sehr zeitig die charakteristischen grasartigen, aber fleischigen Blätter mit dem deutlich abgesetzten weißen Mittelstreifen (Unterschied zum Milchstern [Ornithogalum], bei dem das Weiß eher verschwommen und undeutlich abgesetzt ist). Die Blüten der ersten Arten öffnen sich bei uns ab dem zweiten Februardrittel, je nachdem wie die Witterung es zulässt. Diese Schwertliliengewächse (Iridaceae) besitzen wie die meisten Einkeimblättrigen eine einfache Blütenhülle, diese ist trichter- bis becherförmig ("Große Trichterblume"), mit gleich langen Abschnitten und einem röhrig erweiterten Schlund. Die Blüten öffnen sich nur bei Sonnenschein.
Diese Flechtenart gehört zu der umfangreichen Gattung Cladonia, den Becher-, Säulen- und Rentierflechten. Innerhalb dieser Gattung bilden die Rentierflechten eine eigene Gruppe nah verwandter Strauchflechten, die aufrechte, reich verzweigte Stämmchen aufweisen und an ein unbelaubtes Bäumchen oder ein übermäßig gegliedertes Geweih erinnern. Sie werden auch als eigene Gattung Cladina in einigen Bearbeitungen abgetrennt.