C. E. Ozdemir
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View article: Rate of Sea‐Level Rise and Sediment Characteristics Modulate Deltaic River‐Tide Interactions
Rate of Sea‐Level Rise and Sediment Characteristics Modulate Deltaic River‐Tide Interactions Open
Due to sea‐level rise, small river‐dominated deltas (<100 km 2 ) are expected to become more exposed to tidal influences in the future. However, there remains a knowledge gap in the impending hydrodynamics of such deltas, particularly with…
View article: Phase space tableau simulation for quantum computation
Phase space tableau simulation for quantum computation Open
We introduce a novel tableau-based classical simulation method for quantum computation, formulated within the phase space framework of the extended stabilizer theory of closed non-contextual operators. This method enables the efficient cla…
View article: A conceptual Investigation of Turbidity Current Trigger from Alongshelf Current-supported Turbidity Currents
A conceptual Investigation of Turbidity Current Trigger from Alongshelf Current-supported Turbidity Currents Open
Wave- and current-supported turbidity currents (WCSTCs) are one of the sediment delivery mechanisms from the inner shelf to the shelf break. Therefore, they play a significant role in the global cycles of geo-chemically important particula…
View article: A Numerical Investigation of Wave‐Supported Gravity Flow During Cold Fronts Over the Atchafalaya Shelf
A Numerical Investigation of Wave‐Supported Gravity Flow During Cold Fronts Over the Atchafalaya Shelf Open
Wave‐supported fluid mud (WSFM) plays an important role in sediment downslope transport on the continental shelves. In this study, we incorporated WSFM processes in the wave boundary layer (WBL) into the Community Sediment Transport Modeli…
View article: SEDIMENT TRANSPORT DUE TO CURRENT-SUPPORTED TURBIDITY CURRENTS OVER AN ERODIBLE BED
SEDIMENT TRANSPORT DUE TO CURRENT-SUPPORTED TURBIDITY CURRENTS OVER AN ERODIBLE BED Open
Wave- and current-supported turbidity currents (WCSTCs), are one of the chief participants in shaping the marine geomorphology. What makes WCSTCs different from other turbidity currents is that boundary layer turbulence is required to susp…