David M Rubin
Scientist Emeritus, Pacific Coastal and Marine Science Center
Science and Products
Filter Total Items: 59
Sedimentology and stratigraphy of the Palisades, Lower Comanche, and Arroyo Grande areas of the Colorado River Corridor, Grand Canyon, Arizona
This report analyzes various depositional environments in three archaeologically significant areas of the Colorado River corridor in Grand Canyon.
Archaeological features are built on and buried by fluvial, aeolian, and locally derived sediment, representing a complex interaction between geologic and cultural history. These analyses provide a basis for determining the potential influence of Gl
Authors
Amy E. Draut, David M. Rubin, Jennifer L. Dierker, Helen C. Fairley, Ronald E. Griffiths, Joseph E. Hazel, Ralph E. Hunter, Keith Kohl, Lisa M. Leap, Fred L. Nials, David J. Topping, Michael Yeatts
Measurements of wind, aeolian sand transport, and precipitation in the Colorado River corridor, Grand Canyon, Arizona - November 2003 to December 2004
No abstract available.
Authors
Amy E. Draut, David M. Rubin
Estimating accumulation rates and physical properties of sediment behind a dam: Englebright Lake, Yuba River, northern California
Studies of reservoir sedimentation are vital to understanding scientific and management issues related to watershed sediment budgets, depositional processes, reservoir operations, and dam decommissioning. Here we quantify the mass, organic content, and grain-size distribution of a reservoir deposit in northern California by two methods of extrapolating measurements of sediment physical properties
Authors
Noah P. Snyder, David M. Rubin, Charles N. Alpers, Jonathan R. Childs, Jennifer A. Curtis, Lorraine E. Flint, Scott A. Wright
Bed-sediment grain-size and morphologic data from Suisun, Grizzly, and Honker Bays, CA, 1998-2002
The USGS Place Based Studies Program for San Francisco Bay investigates this sensitive estuarine system to aid in resource management. As part of the inter-disciplinary research program, the USGS collected side-scan sonar data and bed-sediment samples from north San Francisco Bay to characterize bed-sediment texture and investigate temporal trends in sedimentation. The study area is located in cen
Authors
Margaret A. Hampton, Noah P. Snyder, John L. Chin, Dan W. Allison, David M. Rubin
Under San Francisco Bay — A new view of the floor of west-central San Francisco Bay
No abstract available.
Authors
David A. Cacchione, Paul R. Carlson, Pat F. Chavez, John L. Chin, Peter Dartnell, James V. Gardner, Helen Gibbons, David M. Rubin, Miguel Velasco, Florence L. Wong
Tsunami
No abstract available.
Authors
L. Dengler, José C. Borrero, Guy Gelfenbaum, Bruce Jaffe, Emile A. Okal, Modesto Ortiz, Vasily V. Titov, Roberto Anima, Luis Bernales Anticona, Sebastián Araya, Brandon Gomer, J. Gómez, Shun-ichi Koshimura, Gustavo Laos, Leonidas Ocala, Daniel Olcese, Robert Peters, Percy Colque Riega, David M. Rubin, Matthew Swensson, Fernando Vegas
Recent sediment studies refute Glen Canyon Dam hypothesis
Recent studies of sedimentology hydrology, and geomorphology indicate that releases from Glen Canyon Dam are continuing to erode sandbars and beaches in the Colorado River in Grand Canyon National Park, despite attempts to restore these resources. The current strategy for dam operations is based on the hypothesis that sand supplied by tributaries of the Colorado River downstream from the dam will
Authors
David M. Rubin, David J. Topping, John C. Schmidt, Joe Hazel, Matt Kaplinski, Theodore S. Melis
Quantifying the relative importance of flow regulation and grain size regulation of suspended sediment transport α and tracking changes in grain size of bed sediment β
To predict changes in sediment transport, it is essential to know whether transport is regulated mainly by changes in flow or by changes in grain size of sediment on the bed. In flows where changes in suspended sediment transport are regulated purely by changes in flow (grain size of bed sediment is constant), increases in flow strength cause increases in both concentration and grain size of sedim
Authors
David M. Rubin, David J. Topping
Colorado River sediment transport: 1. Natural sediment supply limitation and the influence of Glen Canyon Dam
Analyses of flow, sediment‐transport, bed‐topographic, and sedimentologic data suggest that before the closure of Glen Canyon Dam in 1963, the Colorado River in Marble and Grand Canyons was annually supply‐limited with respect to fine sediment (i.e., sand and finer material). Furthermore, these analyses suggest that the predam river in Glen Canyon was not supply‐limited to the same degree and that
Authors
David J. Topping, David M. Rubin, L. E. Vierra
Colorado River sediment transport: 2. Systematic bed‐elevation and grain‐size effects of sand supply limitation
The Colorado River in Marble and Grand Canyons displays evidence of annual supply limitation with respect to sand both prior to [Topping et al, this issue] and after the closure of Glen Canyon Dam in 1963. Systematic changes in bed elevation and systematic coupled changes in suspended‐sand concentration and grain size result from this supply limitation. During floods, sand supply limitation either
Authors
David J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, Ingrid C. Corson
Regulated streamflow, fine-grained deposits, and effective discharge in canyons with abundant debris fans
No abstract available.
Authors
John C. Schmidt, David M. Rubin
How much velocity information is necessary to predict sediment suspension in the surf zone?
Instantaneous horizontal water velocity, or velocity to a power, does not contain enough information to predict suspension in the surf zone. Unlike steady uniform flow, more one than one velocity is necessary to parameterize pick-up and mixing of sediment into the water column. Using a velocity history improves predictions of suspension by more carefully specifying flow conditions (including accel
Authors
Bruce E. Jaffe, David M. Rubin, Asbury Sallenger
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Filter Total Items: 59
Sedimentology and stratigraphy of the Palisades, Lower Comanche, and Arroyo Grande areas of the Colorado River Corridor, Grand Canyon, Arizona
This report analyzes various depositional environments in three archaeologically significant areas of the Colorado River corridor in Grand Canyon. Archaeological features are built on and buried by fluvial, aeolian, and locally derived sediment, representing a complex interaction between geologic and cultural history. These analyses provide a basis for determining the potential influence of GlAuthorsAmy E. Draut, David M. Rubin, Jennifer L. Dierker, Helen C. Fairley, Ronald E. Griffiths, Joseph E. Hazel, Ralph E. Hunter, Keith Kohl, Lisa M. Leap, Fred L. Nials, David J. Topping, Michael YeattsMeasurements of wind, aeolian sand transport, and precipitation in the Colorado River corridor, Grand Canyon, Arizona - November 2003 to December 2004
No abstract available.AuthorsAmy E. Draut, David M. RubinEstimating accumulation rates and physical properties of sediment behind a dam: Englebright Lake, Yuba River, northern California
Studies of reservoir sedimentation are vital to understanding scientific and management issues related to watershed sediment budgets, depositional processes, reservoir operations, and dam decommissioning. Here we quantify the mass, organic content, and grain-size distribution of a reservoir deposit in northern California by two methods of extrapolating measurements of sediment physical propertiesAuthorsNoah P. Snyder, David M. Rubin, Charles N. Alpers, Jonathan R. Childs, Jennifer A. Curtis, Lorraine E. Flint, Scott A. WrightBed-sediment grain-size and morphologic data from Suisun, Grizzly, and Honker Bays, CA, 1998-2002
The USGS Place Based Studies Program for San Francisco Bay investigates this sensitive estuarine system to aid in resource management. As part of the inter-disciplinary research program, the USGS collected side-scan sonar data and bed-sediment samples from north San Francisco Bay to characterize bed-sediment texture and investigate temporal trends in sedimentation. The study area is located in cenAuthorsMargaret A. Hampton, Noah P. Snyder, John L. Chin, Dan W. Allison, David M. RubinUnder San Francisco Bay — A new view of the floor of west-central San Francisco Bay
No abstract available.AuthorsDavid A. Cacchione, Paul R. Carlson, Pat F. Chavez, John L. Chin, Peter Dartnell, James V. Gardner, Helen Gibbons, David M. Rubin, Miguel Velasco, Florence L. WongTsunami
No abstract available.AuthorsL. Dengler, José C. Borrero, Guy Gelfenbaum, Bruce Jaffe, Emile A. Okal, Modesto Ortiz, Vasily V. Titov, Roberto Anima, Luis Bernales Anticona, Sebastián Araya, Brandon Gomer, J. Gómez, Shun-ichi Koshimura, Gustavo Laos, Leonidas Ocala, Daniel Olcese, Robert Peters, Percy Colque Riega, David M. Rubin, Matthew Swensson, Fernando VegasRecent sediment studies refute Glen Canyon Dam hypothesis
Recent studies of sedimentology hydrology, and geomorphology indicate that releases from Glen Canyon Dam are continuing to erode sandbars and beaches in the Colorado River in Grand Canyon National Park, despite attempts to restore these resources. The current strategy for dam operations is based on the hypothesis that sand supplied by tributaries of the Colorado River downstream from the dam willAuthorsDavid M. Rubin, David J. Topping, John C. Schmidt, Joe Hazel, Matt Kaplinski, Theodore S. MelisQuantifying the relative importance of flow regulation and grain size regulation of suspended sediment transport α and tracking changes in grain size of bed sediment β
To predict changes in sediment transport, it is essential to know whether transport is regulated mainly by changes in flow or by changes in grain size of sediment on the bed. In flows where changes in suspended sediment transport are regulated purely by changes in flow (grain size of bed sediment is constant), increases in flow strength cause increases in both concentration and grain size of sedimAuthorsDavid M. Rubin, David J. ToppingColorado River sediment transport: 1. Natural sediment supply limitation and the influence of Glen Canyon Dam
Analyses of flow, sediment‐transport, bed‐topographic, and sedimentologic data suggest that before the closure of Glen Canyon Dam in 1963, the Colorado River in Marble and Grand Canyons was annually supply‐limited with respect to fine sediment (i.e., sand and finer material). Furthermore, these analyses suggest that the predam river in Glen Canyon was not supply‐limited to the same degree and thatAuthorsDavid J. Topping, David M. Rubin, L. E. VierraColorado River sediment transport: 2. Systematic bed‐elevation and grain‐size effects of sand supply limitation
The Colorado River in Marble and Grand Canyons displays evidence of annual supply limitation with respect to sand both prior to [Topping et al, this issue] and after the closure of Glen Canyon Dam in 1963. Systematic changes in bed elevation and systematic coupled changes in suspended‐sand concentration and grain size result from this supply limitation. During floods, sand supply limitation eitherAuthorsDavid J. Topping, David M. Rubin, Jonathan M. Nelson, Paul J. Kinzel, Ingrid C. CorsonRegulated streamflow, fine-grained deposits, and effective discharge in canyons with abundant debris fans
No abstract available.AuthorsJohn C. Schmidt, David M. RubinHow much velocity information is necessary to predict sediment suspension in the surf zone?
Instantaneous horizontal water velocity, or velocity to a power, does not contain enough information to predict suspension in the surf zone. Unlike steady uniform flow, more one than one velocity is necessary to parameterize pick-up and mixing of sediment into the water column. Using a velocity history improves predictions of suspension by more carefully specifying flow conditions (including accelAuthorsBruce E. Jaffe, David M. Rubin, Asbury Sallenger