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| {{CSDMS meeting abstract yes no 2025 | | {{CSDMS meeting abstract yes no 2025 |
| |CSDMS meeting abstract submit 2025=Yes | | |CSDMS meeting abstract submit 2025=No |
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| {{CSDMS meeting abstract poster Epub 2025
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| |CSDMS meeting poster Epub submit 2025=Poster
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| {{CSDMS meeting abstract title temp2025
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| |CSDMS meeting abstract title=How are Interactions of Seismic Cycle and Climate Reflected in Topography? Implications
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| for Understanding the Architecture of Long-Term Landscape Evolution
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| |Working_group_member_WG_FRG=Geodynamics Focus Research Group
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| {{CSDMS meeting authors template
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| |CSDMS meeting coauthor first name abstract=Adam
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| |CSDMS meeting coauthor last name abstract=Forte
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| |CSDMS meeting coauthor institute / Organization=LSU
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| |CSDMS meeting coauthor town-city=Baton Rouge
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| |CSDMS meeting coauthor country=United States
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| |State=Louisiana
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| |CSDMS meeting coauthor email address=aforte8@lsu.edu
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| {{CSDMS meeting abstract template 2025
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| |CSDMS meeting abstract=Landscape evolution is mainly governed by the head-to-head interactions of tectonic forcing and
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| climate in actively deforming regions. Morphological forms are sensitive recorders of such
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| imprints and a considerable number of previous studies have been dedicated to evaluating the
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| relationship between earthquakes and climatic effects like precipitation. However, distinguishing
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| the exact influence of the earthquake cycle or climate remains challenging and obscure in terms
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| of long-term landscape evolution. This study aims to evaluate and test various simplified
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| spatiotemporal earthquake cycles with respect to changing climatic conditions which will
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| provide insights into the records and marks of paleo-seismic cycles on tectonically active
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| landscapes. We will mainly employ numerical models to build the topography and simulate
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| deformation models associated with various earthquake cycles. The preliminary simulations
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| operate on the same topographic input under constant or cyclic climatic conditions with and
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| without a simulated seismic cycle that is subject to different recurrence intervals. The results of
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| these preliminary simulations demonstrate that the main components of fluvial channels such as
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| 𝜒-elevation and steepness (ksn) are approximately the same under consistent climate context with
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| or without simulated seismic cycles, whereas when cyclical climate oscillations are introduced in
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| the models with or without seismic cycles have meaningfully different final topography. These
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| initial results indicate that fluvial topography may record aspects of earthquake cycles,
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| specifically as a result of variable climate forcing. Further modelling work, along with field
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| validation, is required to clarify details, but these preliminary results highlight the potential for
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| these approaches to yield important data or proxies for the evolution stages of tectonically active
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| landscapes.
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| | {{CSDMS meeting abstract poster Epub 2025}} |
| | {{CSDMS meeting abstract title temp2025}} |
| | {{CSDMS meeting abstract template 2025}} |
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Mehran Basmenji (he/him) choose to not submit an abstract for this conference.
