Women in Sports Journalism : accepted or permitted?

Ein amerikanisches Phänomen erreicht Deutschland: Frauen im männerdominierten Sportfernsehen. Immer häufiger sieht man Frauen vor der Kamera, die männliche Fußballfunktionäre zu aktuellen Themen befragen. Sky ist dabei im deutschen TV, egal ob öffentlich-rechtlich, privat oder Pay-TV, Vorreiter. Insgesamt stehen acht Frauen bei Sky Sport News im Mittelpunkt und 9 weitere arbeiten in der Sport-Live-Produktion vor der Kamera bzw. hinter dem Mikrofon. Das sind erstaunliche Zahlen und so in Deutschland im Sportbereich einzigartig. Doch wie kam es zu diesem Frauen-Boom, wie fühlen sich die männlichen Kollegen, gibt es diese Entwicklung auch in den Sportredaktionen und was empfindet der normale Fernseh-Zuschauer beim Sportschauen

Towards a self-sufficient mobile broadband seismological recording system for year-round operation in Antarctica

Passive seismic measurements allow the study of the deeper Earth beneath the thick Antarctic ice sheet cover. Due to logistical and weather constraints, only a fraction of the area of the Antarctic ice sheet can be surveyed with long-term or temporary sensors. A fundamental limitation is the power supply and operation of the instruments during the polar winter. In addition, there is only a limited time window during the field seasons to deploy the stations over the year. Here we present a rapidly and simple deployable self-sufficient mobile seismic station concept. The station consists of different energy supply modules aligned according to the survey needs, measuring duration, and survey aim. Parts of the concept are integrated into an already existing pool of mobile stations and in the seismological network of the geophysical observatory at Neumayer III Station. Other concepts and features are still under development. The overall goal is to use these temporary mobile arrays in regions where little is known about local and regional tectonic earthquake activity

Understanding an ice stream in Greenland at the EastGRIP camp: An international-multidisciplinary effort and knowledge transfer among scientists

The East Greenland Ice-core Project (EastGRIP) aims to retrieve a 2650m long ice core by drilling through the Northeast Greenland Ice Stream (NEGIS). Scientists from a variety of physical sciences and engineers hope to gain new knowledge on ice stream dynamics and about the past climate. The project has many partners from all around the world, who contribute to the science, logistics and economics of the project. Most of the data is processed and analysed in the field. As there is limited capacity in the field camp, scientists and technical staff are encouraged to learn different working techniques to support their project partners. The community also invites scientists, who work on theoretical aspects on the ice stream to communicate the perspective on the procedures and challenges of data collection in the field. And so it happens that earth system modellers learn how to drill an ice core or non-scientific staff helps with the preparation of the ice core samples. Also, the project partners are motivated to bring together scientists at early stages in their careers to gain fieldwork experience. Once each season the field camp also welcomes high school students and teachers as a part of a joint science and education programme

Crystal fabric orientation of the NEGIS ice stream

IASC Workshop on the dynamics and mass budget of Arctic glacier

How ice anisotropy contributes to fold and ice stream in large-scale ice-sheet models

Satellite and airborne sensors have provided detailed data on ice surface flow velocities, englacial structures of ice sheets and bedrock elevations. These data give insight into the flow behaviour of ice sheets and glaciers. One significant phenomenon observed is large-scale folds (over 100 m in amplitude) in the englacial stratigraphy in the Greenland ice sheet. A large population of folds is located at ice streams, where the flow is distinctly faster than in the surroundings, such as the North-East Greenland Ice Stream (NEGIS). While there is no consensus regarding the formation of large-scale folds, unraveling the underlying mechanisms presents significant potential for enhancing our understanding of the formation and dynamics of ice streams. Ice in ice sheets is a ductile material, i.e., it can flow as a thick viscous fluid with a power-law rheology. Furthermore, ice is significantly anisotropic in its flow properties due to its crystallographic preferred orientation (CPO). Here, we use the Full-Stokes code Underworld2 (Mansour et al.,2022) for 3D modelling of the power-law and transversely isotropic ice flow, also in comparison with the isotropic ice models. Our simulated folds with anisotropic ice show complex patterns on a bumpy bedrock, and are classified into three types: large-scale folds (fold amplitudes >100 m), small-scale folds (fold amplitudes <<100 m, wavelength <<km) and recumbent basal-shear folds. Our results indicate that bedrock topography contributes to perturbations in ice layers, and that ice anisotropy due to the CPO amplifies these into large-scale folds in convergent flow by horizontal shortening. As for our ice stream model, we simulate convergent flow as initial condition, which subsequently initiates the development of shear margins due to the rotation of the ice crystal basal planes. As soon as the shear margins develop, the ice stream starts to propagate upstream in a short time and narrows in the upstream part. Our modeling shows that the anisotropic rheology of ice and CPO change play a significant role for large-scale folding and for the initiation of ice streams with distinct shear margins. Hence, we promote the implementation of ice anisotropy in large-scale ice-sheet evolution models as it holds the potential to introduce novel perspectives to the glaciological community on the dynamics of ice flow

The role of Antarctic overwintering teams and their significance for German polar research

Germany has been operating permanently crewed research stations in Antarctica for more than 45 years. The opening of the Georg Forster Station (1976) and Georg von Neumayer Station (1981) initiated a period of continuous environmental monitoring that allowed both the former East Germany and West Germany to become contracting parties in, and achieve consultative status with, the framework of the Antarctic Treaty. This marked a milestone in German polar research. Continuous research at the Neumayer Station III, its two predecessors, and the now-dismantled former German Democratic Republic (GDR) Georg Forster Station is undertaken by teams of so-called “overwinterers”, presently with nine members, who stay at the base for longer than an entire Antarctic winter. Their long-term stay in Antarctica is defined by isolation, separation from civilization, routine work to sustain long-term scientific observations, and unique personal experiences. This article is dedicated to them and outlines their part and role in the German Antarctic research landscape

Complex basal conditions influence flow at the onset of the Northeast Greenland Ice Stream

The onset and high upstream ice surface velocities of the North East Greenland Ice Stream (NEGIS) are not yet well reproducible in ice sheet models. A major uncertainty remains the understanding of basal sliding and a parameterization of basal conditions. In this study, we assess the slow-flowing part of the NEGIS in a systematic analysis of the basal conditions and investigate the increased ice flow. We analyze the spectral basal roughness in correlation with basal return power from an airborne radar survey with AWIs ultra-wideband radar system in 2018 and compare our results with current ice flow geometry and ice surface flow. We observe a roughness anisotropy where the ice stream widens, indicating a change from a smooth and soft bed to a harder bedrock as well as the evolution of elongated subglacial landforms. In addition, at the upstream part of the NEGIS we find a clear zoning of the bedrock return power, indicating an increased water content at the base of the ice stream. At the downstream part, we observe an increased bedrock return power throughout the entire width of the ice stream and outside its margins, indicating enhanced melting and the distribution of basal water beyond the shear zones

The role of Antarctic overwintering teams and their significance for German polar research

Germany has been operating permanently crewed research stations in Antarctica for more than 45 years. The opening of the Georg Forster Station (1976) and Georg von Neumayer Station (1981) initiated a period of continuous environmental monitoring that allowed both the former East Germany and West Germany to become contracting parties in, and achieve consultative status with, the framework of the Antarctic Treaty. This marked a milestone in German polar research. Continuous research at the Neumayer Station III, its two predecessors, and the now-dismantled former German Democratic Republic (GDR) Georg Forster Station is undertaken by teams of so-called "overwinterers", presently with nine members, who stay at the base for longer than an entire Antarctic winter. Their long-Term stay in Antarctica is defined by isolation, separation from civilization, routine work to sustain long-Term scientific observations, and unique personal experiences. This article is dedicated to them and outlines their part and role in the German Antarctic research landscape