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Mit der vorliegenden Arbeit wurden zu ersten Mal die seit mehreren Jahren vorhergesagten dynamischen Aufbruchsmechanismen - der direkte, der sequentielle und der asynchrone Zerfall - in mehratomigen Molekülen kinematisch vollständig untersucht. Experimentell wurde hierfür ein Kohlenstoffdioxid-(CO2)-Molekül in langsamen Ion-Molekül Stößen dreifach ionisiert, indem die Elektronen des Targets von den langsamen, hochgeladenen Projektilionen (Ar8+-Ionen) eingefangen wurden. Die Untersuchung des Zerfalls des CO2-Ions in die einfach geladenen ionischen Fragmente C+ + O+ + O+ zeigte, dass bei diesem Zerfall das Projektilion vornehmlich einen positiven Ladungszustand von q = 6 und nicht den zunächst erwarteten Ladungszustand q = 5 aufweist. Dies ist darauf zurückzuführen, dass die eingefangenen Elektronen oftmals elektronisch hoch angeregte Zustände im Projektil populieren und demnach im weiteren Verlauf über Autoionisationsprozesse dieses auch wieder verlassen können. Ähnliche Autoionisationsprozesse können auch im Target ablaufen, treten dort jedoch mit einer geringeren Wahrscheinlichkeit auf, da der Wirkungsquerschnitt für Autoionisationsprozesse im Target um einen Faktor 1,3 kleiner ist als für Autoionisationen im Projektil. Zusätzlich zeigte die Untersuchung der Stoßdynamik, dass der dreifache Elektroneneinfang primär bei einer parallelen Orientierung der Molekülachse zur Projektilstrahlachse auftritt. Eine weitere Abhängigkeit der Stoßdynamik zum Beispiel vom Stoßparameter beziehungsweise vom Streuwinkel konnte nicht beobachtet werden. Durch die koinzidente Messung aller vier Reaktionsteilchen konnte der Kanal Ar8+ + CO2 --> Ar6+ + C+ + O+ + O+ eindeutig bestimmt werden und die Reaktionsdynamik des CO2-Ions nach dem Stoß analysiert werden. Dabei tritt deutlich der direkte Aufbruch hervor, bei welchem die drei einfach geladenen Ionen sich rein aufgrund ihrer Coulombkräfte voneinander abstoßen. Bei einer solchen Coulombexplosion bleibt dem Molekülion kaum Zeit, um eine molekulare Schwingung zu vollführen. Neben diesem schnellen Zerfall konnten aber auch jene Zerfälle beobachtet werden, bei denen das Molekülion zuerst molekular schwingt und dann zu einem späteren Zeitpunkt in die ionischen Fragmente zerfällt. Dieser letztere Zerfallsprozess gehört zu den sogenannten asynchronen Zerfallsmechanismen. Er stellt einen Zwischenprozess zwischen dem reinen 1-Stufen-Prozess wie dem direkten Aufbruch und dem reinen 2-Stufen-Prozess dar. Bei solchen sequentiellen 2-Stufen Prozessen fragmentiert das CO2-Molekül im ersten Schritt in ein O+- und ein CO2+-Ion. Im zweiten Schritt dissoziiert dann das CO2+-Fragment, nachdem es nahezu keine Wirkung der Coulombkräfte des ersten Sauerstoffions mehr spürt, in ein C+- und ein O+-Ion. Durch die Darstellung der Schwerpunktsimpulse der Fragmente in Dalitz- und Newton-Diagrammen ist es mit dieser Arbeit erstmals gelungen diesen sequentiellen Prozess experimentell eindeutig nachzuweisen. In der weiteren Analyse konnte gezeigt werden, dass über die im System deponierte Energie, welche über die kinetische Energie der Fragmente bestimmt wird, die verschiedenen Reaktionsmechanismen direkt kontrolliert werden können. Speziell bei Energien unterhalb von 20 eV wurde gezeigt, dass es keine Potentialflächen gibt, die über einen direkten bzw. simultanen Aufbruch zu dem Endzustand C+ + O+ + O+ führen. Bei mehratomigen Molekülen erweist sich das Treffen detaillierter Aussagen über mögliche Dissoziationskanäle ohne die genaue Kenntnis der Lage der Potentialflächen und den Übergängen zwischen diesen als äußerst schwierig. Selbst bei genauer Kenntnis der Lage und Form der Potentialflächen, ist es aufgrund der hohen Dichten innerhalb der Übergangsbereiche der Potentialflächen nahezu unmöglich, den Verlauf der Dissoziationskanäle zu verfolgen. Mit dieser Arbeit ist es gelungen, die verschiedenen Reaktionskanäle ohne die Existenz von Energiepotentialflächen eindeutig zu identifizieren. Außerdem konnte gezeigt werden, dass die Energie, die während des Stoßes im Molekül deponiert wird, eine Schlüsselgröße darstellt, mit welcher die Fragmentationskanäle direkt kontrolliert werden können.
In dieser Studie wurden die Veränderungen der Fibrinolyse während der Geburt bei insgesamt 84 Gebärenden untersucht. Gemessen wurden die Konzentrationen des Plasminogen-Aktivator-Inhibitors, alpha-2-Antiplasmins und Plasminogens mit Hilfe von photometrischen Tests mit chromogenem Substrat kurz vor Geburt, direkt nach Geburt des Kindes, 30 und 90 Minuten nach Lösung der Plazenta bei 41 Spontangebärenden und 43 Sectiopatientinnen. 30 Frauen erhielten kurz vor der Geburt eine Kurzinfusion von einer Millionen KIE Aprotinin (Trasylol®), darunter 15 Spontangebärende und 15 Sectiopatientinnen. Sowohl bei den Spontangebärenden als auch bei den Sectiopatientinnen ohne Gabe von Aprotinin war ein offensichtlicher Abfall der PAI-Konzentrationen nach Geburt zu beobachten, die Konzentrationen für alpha-2-Antiplasmin und Plasminogen blieben im gemessenen Zeitraum unverändert. Nach Gabe von Aprotinin dagegen stieg die PAI-Aktivität sowohl bei den Spontangebärenden als auch bei den Sectiopatientinnen nach Geburt leicht an und fiel dann - im Vergleich zu den Patientinnen ohne Verabreichung von Aprotinin - langsamer und schwächer ab. alpha-2-Antiplasmin stieg bei den mit Aprotinin behandelten Patientinnen nach Geburt an und fiel dann wieder bis auf den Ausgangswert ab, die Plasminogenkonzentrationen blieben im gemessenen Zeitraum weitgehend unverändert. Signifikante Unterschiede zwischen Spontangebärenden und Sectiopatientinnen gab es für alle drei Parameter nicht. Die Veränderungen der Faktoren sprechen für eine erhöhte fibrinolytische Aktivität nach Geburt, die als Reaktion auf die gesteigerte Gerinnung zum gleichen Zeitpunkt zu werten ist. Die Verminderung des Plasminogen-Aktivator-Inhibitors versteht sich als reaktiver Verbrauch durch die bei gesteigerter Gerinnung und folgender Fibrinolyse einsetzende "Anti-Fibrinolyse" durch die entsprechenden Hemmfaktoren. Die Veränderungen des PAI und des alpha-2-Antiplasmin unter Aprotinin sind am ehesten als geringere Beanspruchung des fibrinolytischen Systems zu interpretieren. Abschließend läßt sich aus den Beobachtungen ableiten, daß sich der durch die Plazentalösung ausgelöste Verbrauch von Gerinnungs- und Fibrinolysefaktoren durch die Gabe von Aprotinin reduzieren läßt, ein gerade bei intrapartalen Gerinnungsstörungen erwünschter Effekt.
Lattice simulation of a center symmetric three dimensional effective theory for SU(2) Yang-Mills
(2010)
We present lattice simulations of a center symmetric dimensionally reduced effective field theory for SU(2) Yang Mills which employ thermal Wilson lines and three-dimensional magnetic fields as fundamental degrees of freedom. The action is composed of a gauge invariant kinetic term, spatial gauge fields and a potential for the Wilson line which includes a "fuzzy" bag term to generate non-perturbative fluctuations between Z(2) degenerate ground states. The model is studied in the limit where the gauge fields are set to zero as well as the full model with gauge fields. We confirm that, at moderately weak coupling, the "fuzzy" bag term leads to eigenvalue repulsion in a finite region above the deconfining phase transition which shrinks in the extreme weak-coupling limit. A non-trivial Z(N) symmetric vacuum arises in the confined phase. The effective potential for the Polyakov loop in the theory with gauge fields is extracted from the simulations including all modes of the loop as well as for cooled configurations where the hard modes have been averaged out. The former is found to exhibit a non-analytic contribution while the latter can be described by a mean-field like ansatz with quadratic and quartic terms, plus a Vandermonde potential which depends upon the location within the phase diagram. Other results include the exact location of the phase boundary in the plane spanned by the coupling parameters, correlation lengths of several operators in the magnetic and electric sectors and the spatial string tension. We also present results from simulations of the full 4D Yang-Mills theory and attempt to make a qualitative comparison to the 3D effective theory.
The likely manifestations of climate change like flood hazards are prominent topics in public communication. This can be shown by media analysis and questionnaire data. However, in the case of flood risks an information gap remains resulting in misinformed citizens who probably will not perform the necessary protective actions when an emergency occurs. This paper examines more closely a newly developed approach to flood risk communication that takes the heterogeneity of citizens into account and aims to close this gap. The heterogeneity is analysed on the meso level regarding differences in residential situation as well as on the micro level with respect to risk perception and protective actions. Using the city of Bremen as a case study, empirical data from n=831 respondents were used to identify Action Types representing different states of readiness for protective actions in view of flood risks. These subpopulations can be provided with specific information to meet their heterogeneous needs for risk communication. A prototype of a computer-based information system is described that can produce and pass on such tailored information. However, such an approach to risk communication has to be complemented by meso level analysis which takes the social diversity of subpopulations into account. Social vulnerability is the crucial concept for understanding the distribution of resources and capacities among different social groups. We therefore recommend putting forums and organisations into place that can mediate between the state and its citizens.
Atmospheric new particle formation is a general phenomenon observed over coniferous forests. So far nucleation is described as a function of gaseous sulfuric acid concentration only, which is unable to explain the observed seasonality of nucleation events at different measurement sites. Here we introduce a new nucleation parameter including ozone and water vapor concentrations as well as UV-B radiation as a proxy for OH radical formation. Applying this new parameter to field studies conducted at Finnish and German measurement sites it is found capable to predict the occurrence of nucleation events and their seasonal and annual variation indicating a significant role of organics. Extrapolation to possible future conditions of ozone, water vapor and organic concentrations leads to a significant potential increase in nucleation event number.
Atmospheric new particle formation is a general phenomenon observed over coniferous forests. So far nucleation is either parameterised as a function of gaseous sulphuric acid concentration only, which is unable to explain the observed seasonality of nucleation events at different measurement sites, or as a function of sulphuric acid and organic molecules. Here we introduce different nucleation parameters based on the interaction of sulphuric acid and terpene oxidation products and elucidate the individual importance. They include basic trace gas and meteorological measurements such as ozone and water vapour concentrations, temperature (for terpene emission) and UV B radiation as a proxy for OH radical formation. We apply these new parameters to field studies conducted at conducted at Finnish and German measurement sites and compare these to nucleation observations on a daily and annual scale. General agreement was found, although the specific compounds responsible for the nucleation process remain speculative. This can be interpreted as follows: During cooler seasons the emission of biogenic terpenes and the OH availability limits the new particle formation while towards warmer seasons the ratio of ozone and water vapour concentration seems to dominate the general behaviour. Therefore, organics seem to support ambient nucleation besides sulphuric acid or an OH-related compound. Using these nucleation parameters to extrapolate the current conditions to prognosed future concentrations of ozone, water vapour and organic concentrations leads to a significant potential increase in the nucleation event number.
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.
Pollen-based climate reconstructions were performed on two high-resolution pollen marines cores from the Alboran and Aegean Seas in order to unravel the climatic variability in the coastal settings of the Mediterranean region between 15 000 and 4000 years BP (the Lateglacial, and early to mid-Holocene). The quantitative climate reconstructions for the Alboran and Aegean Sea records focus mainly on the reconstruction of the seasonality changes (temperatures and precipitation), a crucial parameter in the Mediterranean region. This study is based on a multi-method approach comprising 3 methods: the Modern Analogues Technique (MAT), the recent Non-Metric Multidimensional Scaling/Generalized Additive Model method (NMDS/GAM) and Partial Least Squares regression (PLS). The climate signal inferred from this comparative approach confirms that cold and dry conditions prevailed in the Mediterranean region during the Oldest and Younger Dryas periods, while temperate conditions prevailed during the Bølling/Allerød and the Holocene. Our records suggest a West/East gradient of decreasing precipitation across the Mediterranean region during the cooler Late-glacial and early Holocene periods, similar to present-day conditions. Winter precipitation was highest during warm intervals and lowest during cooling phases. Several short-lived cool intervals (i.e. Older Dryas, another oscillation after this one (GI-1c2), Gerzensee/Preboreal Oscillations, 8.2 ka event, Bond events) connected to the North Atlantic climate system are documented in the Alboran and Aegean Sea records indicating that the climate oscillations associated with the successive steps of the deglaciation in the North Atlantic area occurred in both the western and eastern Mediterranean regions. This observation confirms the presence of strong climatic linkages between the North Atlantic and Mediterranean regions.