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Knowing the rates and mechanisms of geomorphic process that shape the Earth’s surface is crucial to understand landscape evolution. Modern methods for estimating denudation rates enable us to quantitatively express and compare processes of landscape downwearing that can be traced through time and space—from the seemingly intact, though intensely shattered, phantom blocks of the catastrophically fragmented basal facies of giant rockslides up to denudational noise in orogen-wide data sets averaging over several millennia. This great variety of spatiotemporal scales of denudation rates is both boon and bane of geomorphic process rates. Indeed, processes of landscape downwearing can be traced far back in time, helping us to understand the Earth’s evolution. Yet, this benefit may turn into a drawback due to scaling issues if these rates are to be compared across different observation timescales.
This thesis investigates the mechanisms, patterns and rates of landscape downwearing across the Himalaya-Tibet orogen.
Accounting for the spatiotemporal variability of denudation processes, this thesis addresses landscape downwearing on three distinctly different spatial scales, starting off at the local scale of individual hillslopes where considerable amounts of debris are generated from rock instantaneously: Rocksliding in active mountains is a major impetus of landscape downwearing. Study I provides a systematic overview of the internal sedimentology of giant rockslide deposits and thus meets the challenge of distinguishing them from macroscopically and microscopically similar glacial deposits, tectonic fault-zone breccias, and impact breccias. This distinction is important to avoid erroneous or misleading deduction of paleoclimatic or tectonic implications. -> Grain size analysis shows that rockslide-derived micro-breccia closely resemble those from meteorite impact or tectonic faults. -> Frictionite may occur more frequently that previously assumed. -> Mössbauer-spectroscopy derived results indicate basal rock melting in the absence of water, involving short-term temperatures of >1500°C.
Zooming out, Study II tracks the fate of these sediments, using the example of the upper Indus River, NW India. There we use river sand samples from the Indus and its tributaries to estimate basin-averaged denudation rates along a ~320-km reach across the Tibetan Plateau margin, to answer the question whether incision into the western Tibetan Plateau margin is currently active or not. -> We find an about one-order-of-magnitude upstream decay—from 110 to 10 mm kyr^-1—of cosmogenic Be-10-derived basin-wide denudation rates across the morphological knickpoint that marks the transition from the Transhimalayan ranges to the Tibetan Plateau. This trend is corroborated by independent bulk petrographic and heavy mineral analysis of the same samples. -> From the observation that tributary-derived basin-wide denudation rates do not increase markedly until ~150–200 km downstream of the topographic plateau margin we conclude that incision into the Tibetan Plateau is inactive. -> Comparing our postglacial Be-10-derived denudation rates to long-term (>10^6 yr) estimates from low-temperature thermochronometry, ranging from 100 to 750 mm kyr^-1, points to an order- of-magnitude decay of rates of landscape downwearing towards present. We infer that denudation rates must have been higher in the Quaternary, probably promoted by the interplay of glacial and interglacial stages.
Our investigation of regional denudation patterns in the upper Indus finally is an integral part of Study III that synthesizes denudation of the Himalaya-Tibet orogen. In order to identify general and time-invariant predictors for Be-10-derived denudation rates we analyze tectonic, climatic and topographic metrics from an inventory of 297 drainage basins from various parts of the orogen. Aiming to get insight to the full response distributions of denudation rate to tectonic, climatic and topographic candidate predictors, we apply quantile regression instead of ordinary least squares regression, which has been standard analysis tool in previous studies that looked for denudation rate predictors. -> We use principal component analysis to reduce our set of 26 candidate predictors, ending up with just three out of these: Aridity Index, topographic steepness index, and precipitation of the coldest quarter of the year. -> Topographic steepness index proves to perform best during additive quantile regression. Our consequent prediction of denudation rates on the basin scale involves prediction errors that remain between 5 and 10 mm kyr^-1. -> We conclude that while topographic metrics such as river-channel steepness and slope gradient—being representative on timescales that our cosmogenic Be-10-derived denudation rates integrate over—generally appear to be more suited as predictors than climatic and tectonic metrics based on decadal records.
The characterization of exoplanets is a young and rapidly expanding field in astronomy.
It includes a method called transmission spectroscopy that searches for planetary spectral
fingerprints in the light received from the host star during the event of a transit. This
techniques allows for conclusions on the atmospheric composition at the terminator region,
the boundary between the day and night side of the planet. Observationally a big
challenge, first attempts in the community have been successful in the detection of several
absorption features in the optical wavelength range. These are for example a Rayleighscattering
slope and absorption by sodium and potassium. However, other objects show
a featureless spectrum indicative for a cloud or haze layer of condensates masking the
probable atmospheric layers.
In this work, we performed transmission spectroscopy by spectrophotometry of three
Hot Jupiter exoplanets. When we began the work on this thesis, optical transmission
spectra have been available for two exoplanets. Our main goal was to advance the current
sample of probed objects to learn by comparative exoplanetology whether certain
absorption features are common. We selected the targets HAT-P-12b, HAT-P-19b and
HAT-P-32b, for which the detection of atmospheric signatures is feasible with current
ground-based instrumentation. In addition, we monitored the host stars of all three objects
photometrically to correct for influences of stellar activity if necessary.
The obtained measurements of the three objects all favor featureless spectra. A variety
of atmospheric compositions can explain the lack of a wavelength dependent absorption.
But the broad trend of featureless spectra in planets of a wide range of temperatures,
found in this work and in similar studies recently published in the literature, favors an
explanation based on the presence of condensates even at very low concentrations in the
atmospheres of these close-in gas giants. This result points towards the general conclusion
that the capability of transmission spectroscopy to determine the atmospheric composition
is limited, at least for measurements at low spectral resolution.
In addition, we refined the transit parameters and ephemerides of HAT-P-12b and HATP-
19b. Our monitoring campaigns allowed for the detection of the stellar rotation period
of HAT-P-19 and a refined age estimate. For HAT-P-12 and HAT-P-32, we derived upper
limits on their potential variability. The calculated upper limits of systematic effects of
starspots on the derived transmission spectra were found to be negligible for all three
targets.
Finally, we discussed the observational challenges in the characterization of exoplanet
atmospheres, the importance of correlated noise in the measurements and formulated
suggestions on how to improve on the robustness of results in future work.
Polypeptoid block coloymers
(2014)
Obwohl in den unionalen Verträgen bis heute keine Vorschrift bezüglich einer Staatshaftung der Mitgliedstaaten für Entscheidungen ihrer Gerichte existiert, hat der Gerichtshof der Europäischen Union (EuGH) in einer Reihe von Entscheidungen eine solche Haftung entwickelt und präzisiert. Die vorliegende Arbeit analysiert eingehend diese Rechtsprechung mitsamt den sich daraus ergebenden facettenreichen Rechtsfragen. Im ersten Kapitel widmet sich die Arbeit der historischen Entwicklung der unionsrechtlichen Staatshaftung im Allgemeinen, ausgehend von dem bekannten Francovich-Urteil aus dem Jahr 1991. Sodann werden im zweiten Kapitel die zur Haftung für judikatives Unrecht grundlegenden Entscheidungen in den Rechtssachen Köbler und Traghetti vorgestellt. In dem sich anschließenden dritten Kapitel wird der Rechtscharakter der unionsrechtlichen Staatshaftung – einschließlich der Frage einer Subsidiarität des unionsrechtlichen Anspruchs gegenüber bestehenden nationalen Staatshaftungsansprüchen – untersucht. Das vierte Kapitel widmet sich der Frage, ob eine unionsrechtliche Staatshaftung für judikatives Unrecht prinzipiell anzuerkennen ist, wobei die wesentlichen für und gegen eine solche Haftung sprechenden Argumente ausführlich behandelt und bewertet werden. Im fünften Kapitel werden die im Zusammenhang mit den unionsrechtlichen Haftungsvoraussetzungen stehenden Probleme der Haftung für letztinstanzliche Gerichtsentscheidungen detailliert erörtert. Zugleich wird der Frage nachgegangen, ob eine Haftung für fehlerhafte unterinstanzliche Gerichtsentscheidungen zu befürworten ist. Das sechste Kapitel befasst sich mit der Ausgestaltung der unionsrechtlichen Staatshaftung für letztinstanzliche Gerichtsentscheidungen durch die Mitgliedstaaten, wobei u.a. zur Anwendbarkeit der deutschen Haftungsprivilegien bei judikativem Unrecht auf den unionsrechtlichen Staatshaftungsanspruch Stellung genommen wird. Im letzten Kapitel wird der Frage nachgegangen, ob der EuGH überhaupt über eine Kompetenz zur Schaffung der Staatshaftung für letztinstanzliche Gerichtsentscheidungen verfügte. Abschließend werden die wichtigsten Ergebnisse der Arbeit präsentiert und ein Ausblick auf weitere mögliche Auswirkungen und Entwicklungen der unionsrechtlichen Staatshaftung für judikatives Unrecht gegeben.
El lunfardo : Kontaktvarietät der Migrationskultur am Rio de la Plata und in der Welt des Tango
(2014)
Zwischen Liberalismus und Christentum : die sozialethischen Aspekte der sozialen Marktwirtschaft
(2014)
Enterprise-specific in-memory data managment : HYRISEc - an in-memory column store engine for OLXP
(2014)
Regeln virtueller Welten
(2014)
Sex-specific differences in the regulation of body weight dynamics and adipose tissue metabolism
(2014)