Exploring physical processes related to past climate proxies: lake sediments and stable water isotopes

Proxy data are essential for the investigation of climate variability on time scales larger than the historical meteorological observation period. The potential value of a proxy depends on our ability to understand and quantify the physical processes that relate the corresponding climate parameter and the signal in the proxy archive. These processes can be explored under present-day conditions. In this thesis, both statistical and physical models are applied for their analysis, focusing on two specific types of proxies, lake sediment data and stable water isotopes.rnIn the first part of this work, the basis is established for statistically calibrating new proxies from lake sediments in western Germany. A comprehensive meteorological and hydrological data set is compiled and statistically analyzed. In this way, meteorological times series are identified that can be applied for the calibration of various climate proxies. A particular focus is laid on the investigation of extreme weather events, which have rarely been the objective of paleoclimate reconstructions so far. Subsequently, a concrete example of a proxy calibration is presented. Maxima in the quartz grain concentration from a lake sediment core are compared to recent windstorms. The latter are identified from the meteorological data with the help of a newly developed windstorm index, combining local measurements and reanalysis data. The statistical significance of the correlation between extreme windstorms and signals in the sediment is verified with the help of a Monte Carlo method. This correlation is fundamental for employing lake sediment data as a new proxy to reconstruct windstorm records of the geological past.rnThe second part of this thesis deals with the analysis and simulation of stable water isotopes in atmospheric vapor on daily time scales. In this way, a better understanding of the physical processes determining these isotope ratios can be obtained, which is an important prerequisite for the interpretation of isotope data from ice cores and the reconstruction of past temperature. In particular, the focus here is on the deuterium excess and its relation to the environmental conditions during evaporation of water from the ocean. As a basis for the diagnostic analysis and for evaluating the simulations, isotope measurements from Rehovot (Israel) are used, provided by the Weizmann Institute of Science. First, a Lagrangian moisture source diagnostic is employed in order to establish quantitative linkages between the measurements and the evaporation conditions of the vapor (and thus to calibrate the isotope signal). A strong negative correlation between relative humidity in the source regions and measured deuterium excess is found. On the contrary, sea surface temperature in the evaporation regions does not correlate well with deuterium excess. Although requiring confirmation by isotope data from different regions and longer time scales, this weak correlation might be of major importance for the reconstruction of moisture source temperatures from ice core data. Second, the Lagrangian source diagnostic is combined with a Craig-Gordon fractionation parameterization for the identified evaporation events in order to simulate the isotope ratios at Rehovot. In this way, the Craig-Gordon model can be directly evaluated with atmospheric isotope data, and better constraints for uncertain model parameters can be obtained. A comparison of the simulated deuterium excess with the measurements reveals that a much better agreement can be achieved using a wind speed independent formulation of the non-equilibrium fractionation factor instead of the classical parameterization introduced by Merlivat and Jouzel, which is widely applied in isotope GCMs. Finally, the first steps of the implementation of water isotope physics in the limited-area COSMO model are described, and an approach is outlined that allows to compare simulated isotope ratios to measurements in an event-based manner by using a water tagging technique. The good agreement between model results from several case studies and measurements at Rehovot demonstrates the applicability of the approach. Because the model can be run with high, potentially cloud-resolving spatial resolution, and because it contains sophisticated parameterizations of many atmospheric processes, a complete implementation of isotope physics will allow detailed, process-oriented studies of the complex variability of stable isotopes in atmospheric waters in future research.rn

AP-UV-MALDI mit flüssigen Matrizes: stabile Ionenausbeuten von mehrfach geladenen Peptid- und Proteinionen für die empfindliche Massenspektrometrie

In der biologischen Massenspektrometrie (MS) werden überwiegend zwei Ionisationstechniken für die Analyse von grçßeren Biomolekfürlen wie Polypeptiden eingesetzt. Dies sind die Nano-Elektrospray-Ionisation[1,2] (nanoESI) und die matrixunterstfürtzte Laserdesorption/-ionisation[3, 4] (MALDI). Beide Techniken werden als „sanft“ bezeichnet, weil sie die Desorption und Ionisation von intakten Analytmolekfürlen und damit ihre erfolgreiche massenspektrometrische Analyse erlauben. Einer der wichtigsten Unterschiede zwischen diesen beiden Ionisationstechniken liegt in ihrer F�higkeit, mehrfach geladene Ionen zu erzeugen. MALDI erzeugt typischerweise einfach geladene Peptidionen, w�hrend nano- ESI leicht mehrfach geladene Ionen produziert, sogar für Peptide mit einer Masse von weniger als 1000 Da. Die Erzeugung von hoch geladenen Ionen ist wünschenswert, da dies die Verwendung von Massenanalysatoren wie Ionenfallen (inkl. Orbitraps) und Hybrid-Quadrupolinstrumenten ermçglicht, die typischerweise nur einen begrenzten m/z- Bereich (<2000–4000) bieten. Hohe Ladungszust�nde ermçglichen auch die Aufnahme von informativeren Fragmentionenspektren, wenn Methoden wie die kollisionsinduzierte Dissoziation (CID), die Elektroneneinfang-Dissoziation (ECD) und die Elektronentransfer-Dissoziation (ETD) in Kombination mit der Tandem-MS (MS/MS) verwendet werden.

Tradurre per la scena: le didascalie dell'Edipo Re rivisitato e interpretato dal collettivo Teatro (In)stabile

L'elaborato consiste in una proposta di traduzione delle didascalie dell'opera teatrale La casa degli uomini zoppi o Edipo liberato, interpretata dal Laboratorio teatro (In)stabile. Il primo capitolo ripercorre la nascita, l'affermazione e i principali riconoscimenti ottenuti dal collettivo teatrale (In)stabile, soffermandosi in particolar modo sull'ideazione e sul percorso di realizzazione dello spettacolo La casa degli uomini zoppi o Edipo liberato. Seguirà poi un capitolo incentrato sulla comparsa delle didascalie, la loro evoluzione nel corso dei secoli e la loro funzione attuale, concentrandosi sulle varianti esistenti e il problema del doppio destinatario del testo teatrale. Il terzo capitolo presenta la proposta di traduzione delle didascalie dell'opera. Il capitolo che segue è dedicato, a completare il precedente, al commento della traduzione. Verranno messi in luce i problemi incontrati nella resa in lingua straniera e le strategie utilizzate per giungere alla soluzione più appropriata, con l'obiettivo di mantenere quanto più possibile inalterati il significato e lo stile del testo di partenza. Per concludere, saranno presentati i commenti e le riflessioni scaturiti dal lavoro di traduzione dell'opera.

Misure di rumore in corrente in un circuito per la generazione di un campo magnetico stabile

Questo lavoro di Tesi, svolto nell’ambito dell’esperimento BEC3 presso il LENS, costituisce il primo approccio al problema della stabilizzazione del campo magnetico di bias in una trappola per atomi ultra-freddi. Stabilizzare il campo magnetico generato da una coppia di bobine si traduce nello stabilizzare la corrente che le attraversa e il primo passo verso la soluzione di questo problema consiste nello stimare lo spettro di potenza del rumore in corrente del circuito. A questo scopo è stata misurata la PSD (Power Spectral Density) del segnale ai capi di diversi sensori per alcuni valori di corrente erogata da due diversi alimentatori. La PSD è stata misurata sia in maniera diretta, che indiretta, attraverso la trasformata di Fourier della Funzione di Autocorrelazione del segnale, misurata nelle stesse condizioni descritte. I dati raccolti costituiscono la base da cui partire per la progettazione e la realizzazione del circuito di stabilizzazione.

Hillel und Schamai, oder die conservative Reform und der stabile Conservatismus : eine Friedensstimme an die Gemeinden Israels und ihre Führer

verf. und hrsg. von L. Adler

Age models and stabile isotope ratios from SO35 cores

Stable isotope measurements on the planktonic foraminifer Globigerinoides ruber (white) have been carried out on a number of selected deep-seas sediment cores from the South Lau and Norlh Fiji Basins. The d18O-curves show good correlation with the inter-ocean oraphic correlation composite d18O-record of the standard reference section (Prell et al. 1986), which, in combination with the chronostratigraphic classifications of Herterich & Sarnthein (1984, modified) and Imbrie et al. 1984), allows a detailed dating of the sedimentary sequences. The deepest layers in core no. 119 (southern Lau Basin) could be assigned to Isotope Stage 24. Measurements made on bulk carbonate in two cores show a much higher glacial-interglacial amplitude, allowing the general identification of the conventional oxygen isotope stages. The d13C-values of the benthic foraminifer Cibicidoides wuellerstorfi show progressively lighter values northwards reflecting an increasing contribution of the isotopically lighter CO2 from the remineralisation of organic matter during the general northward movement of the deep water masses. Cyclicities in the sedimentation rates were observed in core nos. 117 and 119 (both southern Lau Basin) where the interglacials exhibit higher levels than the glacials. Calculated new or export paleoproductivity show that the glacials had higher productivity in the euphotic zone. From the oxygen isotope stratigraphy, the five ash layers in core nos. 117 and 119 could be dated as about 530 ka B.P. in Stage 14, 695 ka B.P. in Stage 18, 775 ka B.P. in Stage 21, 790 ka B.P. and 825 ka B.P. in Stage 22. Carbonate dissolution occurred during stages 5, 8 and 10 to 12.

(Table 1) Stabile isotopes at DSDP Leg 55 Holes

Deep sea drilling on four seamounts in the Emperor Seamount chain revealed that Paleogene shallow-water carbonate sediments of the "bryozoan-algal" facies crown the basalt edifices. According to the biofacies model of Schlanger and Konishi (1966, 1975), this bryozoan- algal assemblage suggests that the seamounts formed in cooler, more northerly waters than those presently occupied by the island of Hawaii; i.e., the paleolatitudes of formation were greater than 20 °N. Moving southward toward the youngest member of the seamount chain, a facies gradient indicative of warmer waters was observed. This gradient is interpreted as a reflection of a northward shift in isotherms during the time span in which the seamounts were progressively formed (Savin et al., 1975). On all seamounts, sedimentation at the drilling sites occurred in a high-energy environment with water depths of approximately 20 meters. Early-stage carbonate diagenesis began in the phreatic zone in the presence of meteoric water, but proceeded after subsidence of the seamounts into intermediate sea waters, where the bulk, stable isotopic composition was determined. The subsidence into intermediate waters was rapid, and permitted establishment of an isotopic equilibrium which, like the facies gradient, reflects the northward shift in isotherms during the Paleogene. Calcite and zeolite cements comprise the later-stage diagenesis, and originated from solutions arising from the hydrolysis of the underlying basalt. In conclusion, the results of this study of the shallow-water carbonate sediments are not inconsistent with a paleolatitude of formation for Suiko Seamount (Site 433) of 26.9 ±3.5 °N, as determined by paleomagnetic measurements (Kono, 1980).

Christus hospes stabile, beneficio Eucharistiae, apud selectissimas animas, ponens domicilium : dissertatio theologica de potissimo effectu Sacramenti Eucharistiae in qua ludus aestivalis a quodam R.P. Madalena adversus ... cardin. Cienfuegos sententiam institutus refellitur [et] dissipatur /

Mode of access: Internet.

Realizzazione di un dispositivo elettromeccanico per la simulazione e per la ricerca di una soluzione stabile del sistema dinamico del pendolo inverso

Obiettivo della tesi è la realizzazione di un dispositivo in grado di riprodurre il sistema del pendolo inverso e di trovare soluzioni vicine alla posizione di equilibrio stabile. Verranno ricavate le equazioni del moto che descrivono il sistema attraverso la meccanica Lagrangiana. Una volta integrate numericamente le equazioni, si procederà con la ricerca di una funzione di controllo per mantenere in equilibrio il sistema: l'efficacia della soluzione verrà valutata graficamente, senza approfondire l'approccio proveniente dalla teoria del controllo che ne è alla base. Infine il sistema verrà realizzato praticamente ed utilizzeremo le stesse funzioni studiate in precedenza.