Global detection and analysis of coastline associated rainfall using an objective pattern recognition technique

Coastally associated rainfall is a common feature especially in tropical and subtropical regions. However, it has been difficult to quantify the contribution of coastal rainfall features to the overall local rainfall. We develop a novel technique to objectively identify precipitation associated with land-sea interaction and apply it to satellite based rainfall estimates. The Maritime Continent, the Bight of Panama, Madagascar and the Mediterranean are found to be regions where land-sea interactions plays a crucial role in the formation of precipitation. In these regions $\approx$ 40% to 60% of the total rainfall can be related to coastline effects. Due to its importance for the climate system, the Maritime Continent is a particular region of interest with high overall amounts of rainfall and large fractions resulting from land-sea interactions throughout the year. To demonstrate the utility of our identification method we investigate the influence of several modes of variability, such as the Madden-Julian-Oscillation and the El Ni\~no Southern Oscillation, on coastal rainfall behavior. The results suggest that during large scale suppressed convective conditions coastal effects tend modulate the rainfall over the Maritime Continent leading to enhanced rainfall over land regions compared to the surrounding oceans. We propose that the novel objective dataset of coastally influenced precipitation can be used in a variety of ways, such as to inform cumulus parametrization or as an additional tool for evaluating the simulation of coastal precipitation within weather and climate models

Quantification of specific bindings of biomolecules by magnetorelaxometry

The binding reaction of the biomolecules streptavidin and anti-biotin antibody, both labelled by magnetic nanoparticles (MNP), to biotin coated on agarose beads, was quantified by magnetorelaxometry (MRX). Highly sensitive SQUID-based MRX revealed the immobilization of the MNP caused by the biotin-streptavidin coupling. We found that about 85% of streptavidin-functionalised MNP bound specifically to biotin-agarose beads. On the other hand only 20% of antibiotin-antibody functionalised MNP were specifically bound. Variation of the suspension medium revealed in comparison to phosphate buffer with 0.1% bovine serum albumin a slight change of the binding behaviour in human serum, probably due to the presence of functioning (non heated) serum proteins. Furthermore, in human serum an additional non-specific binding occurs, being independent from the serum protein functionality

Coastal Tropical Convection in a Stochastic Modeling Framework

Recent research has suggested that the overall dependence of convection near coasts on large-scale atmospheric conditions is weaker than over the open ocean or inland areas. This is due to the fact that in coastal regions convection is often supported by meso-scale land-sea interactions and the topography of coastal areas. As these effects are not resolved and not included in standard cumulus parametrization schemes, coastal convection is among the most poorly simulated phenomena in global models. To outline a possible parametrization framework for coastal convection we develop an idealized modeling approach and test its ability to capture the main characteristics of coastal convection. The new approach first develops a decision algorithm, or trigger function, for the existence of coastal convection. The function is then applied in a stochastic cloud model to increase the occurrence probability of deep convection when land-sea interactions are diagnosed to be important. The results suggest that the combination of the trigger function with a stochastic model is able to capture the occurrence of deep convection in atmospheric conditions often found for coastal convection. When coastal effects are deemed to be present the spatial and temporal organization of clouds that has been documented form observations is well captured by the model. The presented modeling approach has therefore potential to improve the representation of clouds and convection in global numerical weather forecasting and climate models.Comment: Manuscript submitted for publication in Journal of Advances in Modeling Earth System

Magnetic nanoparticles interact and pass an in vitro co-culture blood-placenta barrier model

Magnetic nanoparticles are interesting tools for biomedicine. Before application, critical prerequisites have to be fulfilled. An important issue is the contact and interaction with biological barriers such as the blood-placenta barrier. In order to study these processes in detail, suitable in vitro models are needed. For that purpose a blood-placenta barrier model based on the trophoblast-like cell line BeWo and primary placenta-derived pericytes was established. This model was characterized by molecular permeability, transepithelial electrical resistance and cell-cell-contact markers. Superparamagnetic iron oxide nanoparticles (SPIONs) with cationic, anionic or neutral surface charge were applied. The localization of the nanoparticles within the cells was illustrated by histochemistry. The time-dependent passage of the nanoparticles through the BeWo/pericyte barrier was measured by magnetic particle spectroscopy and atomic absorption spectroscopy. Cationically coated SPIONs exhibited the most extensive interaction with the BeWo cells and remained primarily in the BeWo/pericyte cell layer. In contrast, SPIONs with neutral and anionic surface charge were able to pass the cell layer to a higher extent and could be detected beyond the barrier after 24 h. This study showed that the mode of SPION interaction with and passage through the in vitro blood-placenta barrier model depends on the surface charge and the duration of treatmen

Lithium in Europa

Aktuell ist die deutsche Industrie vollständig auf den Import von Metallen angewiesen, so auch für das leichteste Metall – Lithium. Die globale Produktion von Lithium ist in den letzten fünf Jahren um 263 % gestiegen, die Bergbauförderung liegt bei ca. 100 kt LCE1 (Stand 2021). Der Bedarf des Metalls für Batterien könnte 2030 laut der EU allein in Europa bei ca. 325 kt LCE liegen. Um diesen Bedarf des Marktes mit zu decken, werden in Europa derzeit verschiedene Lithiumprojekte entwickelt. Diese sehen eine Förderung von Lithium aus konventionellen, magmatischen oder sedimentären Gesteinen sowie unkonventionellen geothermalen Solen vor. Acht dieser Projekte befinden sich in einem fortgeschrittenen Entwicklungsstadium und könnten 2030 dazu beitragen, dass zwischen 40 % und 55 % des Bedarfs an Lithium aus europäischen Lagerstätten gewonnen werden könnten. Außerdem wird an Fördermethoden und Aufbereitungstechnologien geforscht, wie beispielsweise die Lithiumgewinnung aus Grubenwasser ehemaliger Bergwerke oder Produktionswässern aus Erdgas- oder Erdölförderungen. Die Entwickler der Lithiumprojekte in Europa erfahren neben technischen, wirtschaftlichen und genehmigungsrechtlichen Herausforderungen auch Ablehnung durch Bürgerinitiativen. Das Recycling von Lithium, speziell aus Lithiumionenbatterien wird in Deutschland durch verschiedene Förderprogramme des Bundes unterstützt und dadurch wissenschaftlich und technisch vorangetrieben. Dies soll dazu beitragen, dass die Quotenvorgaben für Rezyklate aus einem zukünftigen Rücklauf von Batterien erfüllt werden können. Ohne den nationalen und internationalen Bergbau unter der Beibehaltung und weiteren Etablierung von Umwelt- und Sozialstandards, die weitere Entwicklung von Bergbautechnologien sowie den Ausbau der Recyclingmöglichkeiten wird der Lithiumbedarf in Europa nicht zu decken sein

Crystallization age of alpine cleft monazite-(Ce) and correlation with tectonically driven hydrothermal dissolution/precipitation events

Hydrothermal monazite-(Ce) from open clefts/fissure veins in the Alps was utilized as a complimentary tool for dating brittle-ductile/brittle deformation. It may preserve evidence of several crystallization events, commonly over 4-7 Ma, up to ~20 Ma. Monazite-(Ce) crystallizes within ~350-200 °C during tectonic and/or fluid flux events disequilibrating the fluid-crystal/rock chemistry within a cleft. It resists alteration/diffusion under prevailing p-T conditions, but may experience new/re-crystallization or dissolution-reprecipitation. Ages from the northeastern Alps, Austria, of 90-70 Ma cover near peak metamorphism during Eo-Alpine collision over orogenic collapse to extension. In the eastern Tauern Window, ages date metamorphic dome exhumation during Alpine collision at ~19-15 Ma. In the Lepontine dome area ages of ~19-5 Ma date early exhumation, doming and a later change after 12 Ma from thrusting to strike-slip movements, linked to a progressive concentration of deformation towards the extended Rhone-Simplon/Penninic Front fault system in the Mont-Blanc/Aiguilles-Rouges, Aar and western Lepontine areas