Prof. Dr. Jens Schröter

Profil

Zusammenfassung

Prof. Dr. Jens Schröter erforscht die Literatur und Textüberlieferung des frühen Christentums, insbesondere die Rezeption des Apostels Paulus, apokryphe Schriften wie die Nag-Hammadi-Texte und narrative Formen wie Gleichnisse in frühchristlichen Quellen. Seine Expertise liegt in der historisch-kritischen Analyse antiker religiöser Texte und ihrer Bedeutung für die Entwicklung des frühen Christentums.

Skills

Name

Prof. Dr. Jens Schröter

Titel

Prof. Dr.

Fakultät

HU-Theologien

Institut

Theologische Fakultät

Arbeitsgruppe

Exegese und Theologie des Neuen Testaments sowie antike christliche Apokryphen

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HU-FIS-Profil

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Zuletzt gescrapt

27.6.2026, 01:14:18

• CL Topoi II / Ü: Ancient Judaism

  Quelle ↗

  Förderer: DFG Exzellenzinitiative Cluster Zeitraum: 11/2017 - 12/2018 Projektleitung: Prof. Dr. Gerd Graßhoff, Prof. Dr. Jens Schröter

• Die Nag-Hammadi-Schriften in der Literaturgeschichte des frühen Christentums

  Quelle ↗

  Förderer: Fritz Thyssen Stiftung Zeitraum: 02/2015 - 05/2016 Projektleitung: Prof. Dr. Jens Schröter

• Durchsicht der Lutherbibel

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

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

  2014

  Geoscientific model development · 303 Zitationen · 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 · 297 Zitationen · 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.

• Towards multi-resolution global climate modeling with ECHAM6–FESOM. Part I: model formulation and mean climate

  2014

  Climate Dynamics · 248 Zitationen · DOI

  A new climate model has been developed that employs a multi-resolution dynamical core for the sea ice-ocean component. In principle, the multi-resolution approach allows one to use enhanced horizontal resolution in dynamically active regions while keeping a coarse-resolution setup otherwise. The coupled model consists of the atmospheric model ECHAM6 and the finite element sea ice-ocean model (FESOM). In this study only moderate refinement of the unstructured ocean grid is applied and the resolution varies from about 25 km in the northern North Atlantic and in the tropics to about 150 km in parts of the open ocean; the results serve as a benchmark upon which future versions that exploit the potential of variable resolution can be built. Details of the formulation of the model are given and its performance in simulating observed aspects of the mean climate is described. Overall, it is found that ECHAM6–FESOM realistically simulates many aspects of the observed climate. More specifically it is found that ECHAM6–FESOM performs at least as well as some of the most sophisticated climate models participating in the fifth phase of the Coupled Model Intercomparison Project. ECHAM6–FESOM shares substantial shortcomings with other climate models when it comes to simulating the North Atlantic circulation.

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