Prof. Dr. Jens Schröter

Prof. Schröter erforscht die Literaturgeschichte des frühen Christentums, insbesondere die Entstehung und Kanonisierung biblischer Texte sowie die Rezeption von Paulusbriefen in den ersten Jahrhunderten. Seine aktuellen Arbeiten konzentrieren sich auf die Textgenese der Bibel, Gleichnisse und Parabeln in frühchristlichen Schriften sowie auf die historischen Kontexte der frühen christlichen Gemeinschaften. Daneben beschäftigt er sich mit Mediengeschichte und Kulturwissenschaft, etwa mit der Geschichte digitaler Technologien und deren imaginativen Dimensionen. Für Kulturinstitutionen, Verlage und Museen bietet er fundierte Expertise zur Editionsphilologie und Literaturgeschichte; für Bildungseinrichtungen relevante Erkenntnisse zur Textinterpretation und Hermeneutik.

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• The Rise and Expansion of Christianity in the First Three Centuries C.E." (Veranstaltung: 26.-27.07.2010, Berlin)

  Quelle ↗

  Zeitraum: 07/2010 - 12/2010 Projektleitung: Prof. Dr. Jens Schröter

• Durchsicht der Lutherbibel

  Quelle ↗

  Zeitraum: 11/2010 - 12/2011 Projektleitung: Prof. Dr. Jens Schröter

• Endkorrektur eines Manuskripts "Texte und Materialien des Neuen Testaments"

  Quelle ↗

  Zeitraum: 08/2011 - 09/2011 Projektleitung: Prof. Dr. Jens Schröter

• The Finite Element Sea Ice-Ocean Model (FESOM) v.1.4: formulation of an ocean general circulation model

  2014

  Geoscientific model development · DOI

  Abstract. The Finite Element Sea Ice-Ocean Model (FESOM) is the first global ocean general circulation model based on unstructured-mesh methods that has been developed for the purpose of climate research. The advantage of unstructured-mesh models is their flexible multi-resolution modelling functionality. In this study, an overview of the main features of FESOM will be given; based on sensitivity experiments a number of specific parameter choices will be explained; and directions of future developments will be outlined. It is argued that FESOM is sufficiently mature to explore the benefits of multi-resolution climate modelling and that its applications will provide information useful for the advancement of climate modelling on unstructured meshes.

• Revisiting the contemporary sea-level budget on global and regional scales

  2016

  Proceedings of the National Academy of Sciences · DOI

  Dividing the sea-level budget into contributions from ice sheets and glaciers, the water cycle, steric expansion, and crustal movement is challenging, especially on regional scales. Here, Gravity Recovery And Climate Experiment (GRACE) gravity observations and sea-level anomalies from altimetry are used in a joint inversion, ensuring a consistent decomposition of the global and regional sea-level rise budget. Over the years 2002-2014, we find a global mean steric trend of 1.38 ± 0.16 mm/y, compared with a total trend of 2.74 ± 0.58 mm/y. This is significantly larger than steric trends derived from in situ temperature/salinity profiles and models which range from 0.66 ± 0.2 to 0.94 ± 0.1 mm/y. Mass contributions from ice sheets and glaciers (1.37 ± 0.09 mm/y, accelerating with 0.03 ± 0.02 mm/y(2)) are offset by a negative hydrological component (-0.29 ± 0.26 mm/y). The combined mass rate (1.08 ± 0.3 mm/y) is smaller than previous GRACE estimates (up to 2 mm/y), but it is consistent with the sum of individual contributions (ice sheets, glaciers, and hydrology) found in literature. The altimetric sea-level budget is closed by coestimating a remaining component of 0.22 ± 0.26 mm/y. Well above average sea-level rise is found regionally near the Philippines (14.7 ± 4.39 mm/y) and Indonesia (8.3 ± 4.7 mm/y) which is dominated by steric components (11.2 ± 3.58 mm/y and 6.4 ± 3.18 mm/y, respectively). In contrast, in the central and Eastern part of the Pacific, negative steric trends (down to -2.8 ± 1.53 mm/y) are detected. Significant regional components are found, up to 5.3 ± 2.6 mm/y in the northwest Atlantic, which are likely due to ocean bottom pressure variations.