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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Topp-Jørgensen, Elmer; Rasch, Morten; Elger, Kirsten; Vincent, Warwick; +2 Authors

    This book is about management of arctic and northern alpine research stations. It has been produced by a group of station managers participating in the EU 7th Framework Programme Infrastructure project called INTERACT. With this book we want to share the knowledge and experiences we have gained from managing very different research stations in very different environmental and climatic settings. The target audience for the book is mainly managers of research stations in arctic and alpine areas, but we hope that it will also be useful for others involved in science coordination and logistics, e.g. research institutions, chief scientists and expedition planners. The book has been produced mainly based on input from practising station managers being part of ‘INTERACT Station Managers’ Forum (SMF), a forum established to provide a platform for exchange of information between station managers and other participants within INTERACT, and to collect and disseminate knowledge embedded within the network. The scope of this book is to identify and describe best practices and key considerations of relevance to station management under arctic and alpine conditions. As research stations operate under very different legal regimes, financial conditions, environmental and climatic conditions, as well as remoteness, it is not possible to identify specific best practices that fit all stations. Instead, we have described key issues that should be considered and addressed by station management, and supplemented this with examples of good practices from stations operating under different conditions (e.g. different climate, remoteness or size).

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    Authors: Ziegler, M.; Heidbach, O.;

    These data are supplementary material to Ziegler & Heidbach (2020) and present the results of a 3D geomechanical-numerical model of the stress state with quantified uncertainties. The average modelled stress state is provided for each of the six components of the full stress tensor. In addition, the associated standard deviation for each component is provided. The modelling approach uses a published lithological model and the used data is described in the publication Ziegler & Heidbach (2020). The reduced stress tensor is derived using the Tecplot Addon GeoStress (Stromeyer & Heidbach, 2017).The model results are provided in a comma-separated ascii file. Each line in the file represents one of the approx. 3 million finite elements that comprise the model.

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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Bohsung, Lukas; Schanner, Maximilian; Korte, Monika; Holschneider, Matthias;

    The primary data sources for reconstructing the Earth's magnetic field of the past millennia are archeomagnetic and sedimentary paleomagnetic data. Sediment records, in particular, are crucial in extending the temporal and spatial coverage of global Earth's magnetic field models, especially when archeomagnetic data is sparse. However, the post-depositional remanent magnetization (pDRM) process is still poorly understood and can cause smoothing of the magnetic signal and offsets with respect to the sediment age. To make effective use of sedimentary data, it is essential to understand the lock-in process and its impact on the magnetic signal. In this study, we investigate the lock-in process theoretically and derive a parameterized lock-in function to approximate all possible lock-in behaviors. Additionally, we demonstrate that a lock-in function that is independent of absolute parameters can only be applied to the magnetic direction components, but not to the relative intensity. Integrating this lock-in function into the ArchKalMag14k modeling procedure (Schanner et al., 2022, https://doi.org/10.1029/2021JB023166) allows to include data from sediment records. The parameters of the lock-in function are estimated by maximum likelihood methods using archeomagnetic data as a reference. The effectiveness of the proposed method is evaluated through synthetic tests. Additionally, it is applied to real sediment records. Our results demonstrate that the proposed method is capable of effectively correcting the distortion caused by the lock-in process, making data from sedimentary records a more reliable and informative source for Earth's magnetic field reconstructions. The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

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    https://doi.org/10.57757/iugg2...
    Article . 2023
    License: CC BY
    Data sources: Datacite
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      https://doi.org/10.57757/iugg2...
      Article . 2023
      License: CC BY
      Data sources: Datacite
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Dostal, P.; Buerger, K.; Imbery, F.; Seidel, J.;
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    Authors: Marzocchi, W.; Iturrieta, P.; Falcone, G.;

    The main goal of WP3 is to advance the operational earthquake forecasting capabilities at different spatial scales. This deliverable contains the description of the repository where all promising codes of the OEF models that have been produced in the first 30 months of the project have been uploaded. Since all codes have to be tested in WP7 in the last year of the project, the structure of this deliverable has been agreed with colleagues working at WP7. The repository contains both the codes that will be used in the WP7 testing phase, and a detailed description of each model. In this document we will describe the main features of the repository and the link where codes and descriptions can be found. Then, we will briefly summarize the main features of the models that are contained in the repository. At the time of this deliverable, eight models have been submitted to the repository; however, at the end of the project we expect to have more; in fact, some additional models are almost finished, but not yet ready for the testing phase and so they have not been uploaded yet; very likely, they will be uploaded soon and tested in WP7 in the last year of the project. In this first phase the repository is kept private (available only after a specific request to the WP leader) to leave the time to the modelers to finalize the scientific papers relative to their models. The repository will be then made public through the platform Zenodo at the end of the project.

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    Authors: Stiller, M.; Krawczyk, C.; Lück, E.; BASIN Research Group;
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    Authors: Jousset, P.; Mortensen, A.; Wollin, C.; Diaz Meza, S.; +1 Authors

    The GFZ-Landsvirkjun Theistareykir Fibre array is located in the Theytareykir geothermal area, in North Iceland. It is collocated with arrays of broadband seismometers and gravity meters (see e.g., https://doi.org/10.1186/s40517-021-00208-w). The geometry of the fibre array is following the telecom network in the area, and was chosen to test the seismological capabilities of telecom cables in this geothermal environment. We connected an iDAS V2 interrogator from Silixa. The interrogator location is lat=65.898041, lon=-16.966274. The array starts N-S and after 1.5 km, turns towards the East, up to a local transmission antenna station for mobile phones. The length of the path is ~5 km. The length of the cable is actually more than 15 km, as other fibre instance is connected at the transmission antenna station.. Jumps were performed along the cable to geo-locate the channels. The exact location of the fibre can unfortunately not be disclosed. Original recordings at 1000 Hz were downsampled to 200 Hz using a software from INGV-OE (michele.prestifilippo@ingv.it) and are provided in an h5 format. We provide here the first fibre instance (5 km long). The data contain 1 h long recording intervals framing M>5 teleseismic earthquakes recorded in the frame of the global DAS month, an initiative to collaboratively record and share simultaneously recorded DAS data from all over the world (https://www.norsar.no/in-focus/global-das-monitoring-month-february-2023). DAS is an emerging technology increasingly used by seismologists to convert kilometer long optical fibers into seismic sensors.

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    Authors: Lott, F.; Al-Qaryouti, M.; Corsmeier, U.; Ritter, J.;

    A temporary seismic array was installed in combination with a meteorological station in the Dead Sea valley, Jordan. Within the scope of the HGF virtual institute DESERVE we operated 15 temporary seismic stations between February 2014 and February 2015 together with a nearby meteorological station close to the east coast of the Dead Sea. The main aim was to acquire data to study the influence of wind on seismic records and retrieve related meteorological parameters. The study area is scarcely populated and has ideal meteorological conditions to study periodically occurring winds.

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    Authors: Ingo Heinrich;
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    Authors: Pons, M.; Sobolev, S.; Liu, S.; Neuharth, D.;

    The Central Andes (~21°S) is a subduction-type orogeny formed in the last ~50 Ma from the subduction of the Nazca oceanic plate beneath the South American continental plate. However, the most important phases of deformation occur in the last 20 Ma. Pulses of shortening have led to the sudden growth of the by the Altiplano-Puna plateau. Previous studies have provided insights on the importance of various mechanisms on the overall shortening such as the weakening of the overriding plate from crustal eclogitization and delamination, or the importance of a relatively high friction at the subduction interface, and weak sediments in foreland. However none of them has addressed the mechanism behind these shortening pulses yet. Therefore, we built a series of high resolution 2D visco-plastic subduction models using the ASPECT geodynamic code, in which the oceanic plate is buoyancy-driven and the velocity of the continent is prescribed. We have also implemented a realistic geometry for the south American plate at ~30 Ma. We propose a new plausible mechanism (buckling and steepening of the slab) as the cause of these pulses. The buckling leads to the blockage of the trench. Consequently, the difference of velocity between the South American plate and the trench is accommodated by shortening. The data presented here includes the parameters files, for the reference model (S1) and the following alternative simulations: models with variation of the friction at the subduction interface (S2a-c), a model without eclogitization of the lower crust (S3) and a model with higher thermal conductivity of the upper crust (S4). Additionally, this publication includes the initial composition and thermal state of the lithosphere used for the models and a Readme file that gives all the instructions to run them.

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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Topp-Jørgensen, Elmer; Rasch, Morten; Elger, Kirsten; Vincent, Warwick; +2 Authors

    This book is about management of arctic and northern alpine research stations. It has been produced by a group of station managers participating in the EU 7th Framework Programme Infrastructure project called INTERACT. With this book we want to share the knowledge and experiences we have gained from managing very different research stations in very different environmental and climatic settings. The target audience for the book is mainly managers of research stations in arctic and alpine areas, but we hope that it will also be useful for others involved in science coordination and logistics, e.g. research institutions, chief scientists and expedition planners. The book has been produced mainly based on input from practising station managers being part of ‘INTERACT Station Managers’ Forum (SMF), a forum established to provide a platform for exchange of information between station managers and other participants within INTERACT, and to collect and disseminate knowledge embedded within the network. The scope of this book is to identify and describe best practices and key considerations of relevance to station management under arctic and alpine conditions. As research stations operate under very different legal regimes, financial conditions, environmental and climatic conditions, as well as remoteness, it is not possible to identify specific best practices that fit all stations. Instead, we have described key issues that should be considered and addressed by station management, and supplemented this with examples of good practices from stations operating under different conditions (e.g. different climate, remoteness or size).

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    Authors: Ziegler, M.; Heidbach, O.;

    These data are supplementary material to Ziegler & Heidbach (2020) and present the results of a 3D geomechanical-numerical model of the stress state with quantified uncertainties. The average modelled stress state is provided for each of the six components of the full stress tensor. In addition, the associated standard deviation for each component is provided. The modelling approach uses a published lithological model and the used data is described in the publication Ziegler & Heidbach (2020). The reduced stress tensor is derived using the Tecplot Addon GeoStress (Stromeyer & Heidbach, 2017).The model results are provided in a comma-separated ascii file. Each line in the file represents one of the approx. 3 million finite elements that comprise the model.

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    Authors: Bohsung, Lukas; Schanner, Maximilian; Korte, Monika; Holschneider, Matthias;

    The primary data sources for reconstructing the Earth's magnetic field of the past millennia are archeomagnetic and sedimentary paleomagnetic data. Sediment records, in particular, are crucial in extending the temporal and spatial coverage of global Earth's magnetic field models, especially when archeomagnetic data is sparse. However, the post-depositional remanent magnetization (pDRM) process is still poorly understood and can cause smoothing of the magnetic signal and offsets with respect to the sediment age. To make effective use of sedimentary data, it is essential to understand the lock-in process and its impact on the magnetic signal. In this study, we investigate the lock-in process theoretically and derive a parameterized lock-in function to approximate all possible lock-in behaviors. Additionally, we demonstrate that a lock-in function that is independent of absolute parameters can only be applied to the magnetic direction components, but not to the relative intensity. Integrating this lock-in function into the ArchKalMag14k modeling procedure (Schanner et al., 2022, https://doi.org/10.1029/2021JB023166) allows to include data from sediment records. The parameters of the lock-in function are estimated by maximum likelihood methods using archeomagnetic data as a reference. The effectiveness of the proposed method is evaluated through synthetic tests. Additionally, it is applied to real sediment records. Our results demonstrate that the proposed method is capable of effectively correcting the distortion caused by the lock-in process, making data from sedimentary records a more reliable and informative source for Earth's magnetic field reconstructions. The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

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    https://doi.org/10.57757/iugg2...
    Article . 2023
    License: CC BY
    Data sources: Datacite
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      https://doi.org/10.57757/iugg2...
      Article . 2023
      License: CC BY
      Data sources: Datacite
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    Authors: Dostal, P.; Buerger, K.; Imbery, F.; Seidel, J.;
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    Authors: Marzocchi, W.; Iturrieta, P.; Falcone, G.;

    The main goal of WP3 is to advance the operational earthquake forecasting capabilities at different spatial scales. This deliverable contains the description of the repository where all promising codes of the OEF models that have been produced in the first 30 months of the project have been uploaded. Since all codes have to be tested in WP7 in the last year of the project, the structure of this deliverable has been agreed with colleagues working at WP7. The repository contains both the codes that will be used in the WP7 testing phase, and a detailed description of each model. In this document we will describe the main features of the repository and the link where codes and descriptions can be found. Then, we will briefly summarize the main features of the models that are contained in the repository. At the time of this deliverable, eight models have been submitted to the repository; however, at the end of the project we expect to have more; in fact, some additional models are almost finished, but not yet ready for the testing phase and so they have not been uploaded yet; very likely, they will be uploaded soon and tested in WP7 in the last year of the project. In this first phase the repository is kept private (available only after a specific request to the WP leader) to leave the time to the modelers to finalize the scientific papers relative to their models. The repository will be then made public through the platform Zenodo at the end of the project.

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    Authors: Stiller, M.; Krawczyk, C.; Lück, E.; BASIN Research Group;
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    Authors: Jousset, P.; Mortensen, A.; Wollin, C.; Diaz Meza, S.; +1 Authors

    The GFZ-Landsvirkjun Theistareykir Fibre array is located in the Theytareykir geothermal area, in North Iceland. It is collocated with arrays of broadband seismometers and gravity meters (see e.g., https://doi.org/10.1186/s40517-021-00208-w). The geometry of the fibre array is following the telecom network in the area, and was chosen to test the seismological capabilities of telecom cables in this geothermal environment. We connected an iDAS V2 interrogator from Silixa. The interrogator location is lat=65.898041, lon=-16.966274. The array starts N-S and after 1.5 km, turns towards the East, up to a local transmission antenna station for mobile phones. The length of the path is ~5 km. The length of the cable is actually more than 15 km, as other fibre instance is connected at the transmission antenna station.. Jumps were performed along the cable to geo-locate the channels. The exact location of the fibre can unfortunately not be disclosed. Original recordings at 1000 Hz were downsampled to 200 Hz using a software from INGV-OE (michele.prestifilippo@ingv.it) and are provided in an h5 format. We provide here the first fibre instance (5 km long). The data contain 1 h long recording intervals framing M>5 teleseismic earthquakes recorded in the frame of the global DAS month, an initiative to collaboratively record and share simultaneously recorded DAS data from all over the world (https://www.norsar.no/in-focus/global-das-monitoring-month-february-2023). DAS is an emerging technology increasingly used by seismologists to convert kilometer long optical fibers into seismic sensors.

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    Authors: Lott, F.; Al-Qaryouti, M.; Corsmeier, U.; Ritter, J.;

    A temporary seismic array was installed in combination with a meteorological station in the Dead Sea valley, Jordan. Within the scope of the HGF virtual institute DESERVE we operated 15 temporary seismic stations between February 2014 and February 2015 together with a nearby meteorological station close to the east coast of the Dead Sea. The main aim was to acquire data to study the influence of wind on seismic records and retrieve related meteorological parameters. The study area is scarcely populated and has ideal meteorological conditions to study periodically occurring winds.

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