MS
Member Since 2020
Maria Schmeer
Graduate Student, California Institute of Technology
AGU Research
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The role of initial ice morphology in controlling the thaw behavior of a permafrost soil column
SOIL WATER PHASE TRANSITIONS: MULTISCALE CHARACTERIZATION, HYDROLOGICAL MODELING, AND IMPLICATIONS FOR CRITICAL ZONE SCIENCE POSTER
hydrology | 12 december 2024
Maria Schmeer, Rio Kawate, Nathan Jones, Adrian Mo...
Coupling of mass balance, heat transfer and phase change in ice-bearing porous media is a complex modeling challenge but a key component in building p...
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Evaluating Threshold Channel Theory and Stress Partitioning in a Self-Formed Alluvial Channel with Bedforms
ALLUVIAL RIVERS: PROCESSES AND DYNAMICS ACROSS SCALES I ORAL
earth and planetary surface processes | 11 december 2024
Maria Schmeer, Kimberly Miller, Michael P. Lamb
To evaluate the magnitude of bank strength (e.g., the role of vegetation or cohesive sediment) in alluvial channels, it is typical to compare stress b...
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Modeling the Nonequilibrium Thermodynamic Response of a Permafrost Soil Column to Thermal Perturbations
OBSERVING AND MODELING OF EARTH SURFACE CRYOGENIC PROCESSES AND THE STATE OF PERMAFROST II POSTER
cryosphere | 15 december 2023
Maria Schmeer, Adrian Moure, Xiaojing Fu
Coupling of mass balance, heat transfer and phase change in ice-bearing porous media is a complex modeling challenge but a key component in building p...
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Towards Producing Single-Threaded Channels in the Laboratory
FLUID FLOW, SEDIMENT TRANSPORT, AND LANDSCAPE EVOLUTION IN FLUVIAL SYSTEMS ACROSS SCALES V POSTER
earth and planetary surface processes | 14 december 2023
Maria Schmeer, Kimberly Miller, Zhuo Liu, Michael ...
Despite being ubiquitous in nature, single-threaded channels are notoriously difficult to produce at reduced scale in laboratory experiments. Successf...
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Ablation‐Limited Erosion Rates of Permafrost Riverbanks
JOURNAL OF GEOPHYSICAL RESEARCH: EARTH SURFACE
29 july 2023
Madison Douglas, Kimberly Miller, Maria Schmeer, M...
Permafrost thaw is hypothesized to increase riverbank erosion rates, which threatens Arctic communities and infrastructure. However, existing erosi...
Searching for Topographic Signatures of Hillslope Diffusivity Across Landscapes
EARTH AND PLANETARY SURFACE PROCESSES GENERAL CONTRIBUTIONS IV POSTER
earth and planetary surface processes | 16 december 2022
Maria Schmeer, Claire C. Masteller
Diffusive erosion processes describe the transport of sediment across hillslopes and affect landscape-scale topographic change. The diffusivity consta...
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Permafrost Riverbank Erosion in Frozen Flume Experiments
PHYSICAL LANDSCAPE SIGNATURES OF CONTEMPORARY CLIMATE CHANGE I ORAL
earth and planetary surface processes | 17 december 2021
Madison Douglas, Kimberly L. Miller, Maria Schmeer...
Erosion of riverbanks within permafrost terrain threatens buildings and infrastructure in many Arctic communities, and has already forced some communi...
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Using Temperature Sensors to Track the Thaw and Erosion Fronts in an Experimental Permafrost Riverbank
PHYSICAL LANDSCAPE SIGNATURES OF CONTEMPORARY CLIMATE CHANGE II POSTER
earth and planetary surface processes | 17 december 2021
Maria Schmeer, Madison Douglas, Kimberly L. Miller...
As Artic rivers warm, more heat is available to thaw permafrost, which can destabilize riverbanks and affect Arctic riverside communities. The thermal...
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