Creation of residual flows in a partially stratified estuary
M.T. Stacey, J.R. Burau, Stephen G. Monismith
2001, Journal of Geophysical Research C: Oceans (106) 17013-17037
The creation of residual flows in estuaries is examined using acoustic Doppler current profiler data sets from northern San Francisco Bay. The data sets are analyzed using principal component analysis to examine the temporal variability of the flows which create the residual circulation. It is seen that in this periodically...
Ocean Drilling Program Leg 178 (Antarctic Peninsula): Sedimentology of glacially influenced continental margin topsets and foresets
N. Eyles, J. Daniels, L.E. Osterman, N. Januszczak
2001, Marine Geology (178) 135-156
Ocean Drilling Program Leg 178 (February-April 1998) drilled two sites (Sites 1097 and 1103) on the outer Antarctic Peninsula Pacific continental shelf. Recovered strata are no older than late Miocene or early Pliocene (<4.6 Ma). Recovery at shallow depths in loosely consolidated and iceberg-turbated bouldery sediment was poor but improved...
Trends in long-period seismicity related to magmatic fluid compositions
M.M. Morrissey, B. A. Chouet
2001, Journal of Volcanology and Geothermal Research (108) 265-281
Sound speeds and densities are calculated for three different types of fluids: gas-gas mixture; ash-gas mixture; and bubbly liquid. These fluid properties are used to calculate the impedance contrast (Z) and crack stiffness (C) in the fluid-driven crack model (Chouet: J. Geophys. Res., 91 (1986) 13,967; 101 (1988) 4375; A...
Spatial extent of a hydrothermal system at Kilauea Volcano, Hawaii, determined from array analyses of shallow long-period seismicity 2. Results
J. Almendros, B. Chouet, P. Dawson
2001, Journal of Geophysical Research B: Solid Earth (106) 13581-13597
Array data from a seismic experiment carried out at Kilauea Volcano, Hawaii, in February 1997, are analyzed by the frequency-slowness method. The slowness vectors are determined at each of three small-aperture seismic antennas for the first arrivals of 1129 long-period (LP) events and 147 samples of volcanic tremor. The source...
Evaluation of flash-flood discharge forecasts in complex terrain using precipitation
D. Yates, T.T. Warner, E.A. Brandes, G.H. Leavesley, Jielun Sun, C.K. Mueller
2001, Journal of Hydrologic Engineering (6) 265-274
Operational prediction of flash floods produced by thunderstorm (convective) precipitation in mountainous areas requires accurate estimates or predictions of the precipitation distribution in space and time. The details of the spatial distribution are especially critical in complex terrain because the watersheds are generally small in size, and small position errors...
Resolution analysis of finite fault source inversion using one- and three-dimensional Green's functions 2. Combining seismic and geodetic data
D.J. Wald, R.W. Graves
2001, Journal of Geophysical Research B: Solid Earth (106) 8767-8788
Using numerical tests for a prescribed heterogeneous earthquake slip distribution, we examine the importance of accurate Green's functions (GF) for finite fault source inversions which rely on coseismic GPS displacements and leveling line uplift alone and in combination with near-source strong ground motions. The static displacements, while sensitive to the...
Influence of reactive sulfide (AVS) and supplementary food on Ag, Cd and Zn bioaccumulation in the marine polychaete Neanthes arenaceodentata
J.-S. Lee, B.-G. Lee, H. Yoo, C.-H. Koh, S. N. Luoma
2001, Marine Ecology Progress Series (216) 129-140
A laboratory bioassay determined the relative contribution of various pathways of Ag, Cd and Zn bioaccumulation in the marine polychaete Neanthes arenaceodentata exposed to moderately contaminated sediments. Juvenile worms were exposed for 25 d to experimental sediments containing 5 different reactive sulfide (acid volatile sulfides, AVS) concentrations (1 to 30...
Fault zone amplified waves as a possible seismic hazard along the Calaveras fault in central California
P. Spudich, K.B. Olsen
2001, Geophysical Research Letters (28) 2533-2536
The Calaveras fault lies within a low velocity zone (LVZ) 1-2 km wide near Gilroy, California. Accelerographs G06, located in the LVZ 1.2 km from the Calaveras fault, and G07, 4 km from G06, recorded both the M 6.2 1984 Morgan Hill and the M 6.9 1989 Loma Prieta earthquakes....
A minimalist probabilistic description of root zone soil water
P. C. D. Milly
2001, Water Resources Research (37) 457-463
The probabilistic response of depth‐integrated soil water to given climatic forcing can be described readily using an existing supply‐demand‐storage model. An apparently complex interaction of numerous soil, climate, and plant controls can be reduced to a relatively simple expression for the equilibrium probability density function of soil water as a...
Historical effects of El Nino and La Nina events on the seasonal evolution of the montane snowpack in the Columbia and Colorado River Basins
Martyn P. Clark, Mark C. Serreze, Gregory J. McCabe
2001, Water Resources Research (37) 741-757
Snow‐water equivalent (SWE) data measured at several hundred montane sites in the western United States are used to examine the historic effects of El Nino and La Nina events on seasonal snowpack evolution in the major subbasins in the Columbia and Colorado River systems. Results are used to predict annual...
The failure of earthquake failure models
J. Gomberg
2001, Journal of Geophysical Research B: Solid Earth (106) 16253-16263
In this study I show that simple heuristic models and numerical calculations suggest that an entire class of commonly invoked models of earthquake failure processes cannot explain triggering of seismicity by transient or "dynamic" stress changes, such as stress changes associated with passing seismic waves. The models of this class...
Resolution analysis of finite fault source inversion using one- and three-dimensional Green's functions 1. Strong motions
R.W. Graves, D.J. Wald
2001, Journal of Geophysical Research B: Solid Earth (106) 8745-8766
We develop a methodology to perform finite fault source inversions from strong motion data using Green's functions (GFs) calculated for a three-dimensional (3-D) velocity structure. The 3-D GFs are calculated numerically by inserting body forces at each of the strong motion sites and then recording the resulting strains along the...
Empirical Green's function analysis of recent moderate events in California
S. E. Hough
2001, Bulletin of the Seismological Society of America (91) 456-467
I use seismic data from portable digital stations and the broadband Terrascope network in southern California to investigate radiated earthquake source spectra and discuss the results in light of previous studies on both static stress drop and apparent stress. Applying the empirical Green's function (EGF) method to two sets of...
The trade-off between food and temperature in the habitat choice of bluegill sunfish
M. L. Wildhaber
2001, Journal of Fish Biology (58) 1476-1478
A model is presented to describe the trade-off between food and temperature in bluegills Lepomis macrochirus, where temperature was the primary factor used in determining the patch in which to reside....
Thermal thickness and evolution of Precambrian lithosphere: A global study
I.M. Artemieva, Walter D. Mooney
2001, Journal of Geophysical Research B: Solid Earth (106) 16387-16414
The thermal thickness of Precambrian lithosphere is modeled and compared with estimates from seismic tomography and xenolith data. We use the steady state thermal conductivity equation with the same geothermal constraints for all of the Precambrian cratons (except Antarctica) to calculate the temperature distribution in the stable...
A look inside 'black box' hydrograph separation models: A study at the hydrohill catchment
C. Kendall, Jeffery J. McDonnell, W. Gu
2001, Hydrological Processes (15) 1877-1902
Runoff sources and dominant flowpaths are still poorly understood in most catchments; consequently, most hydrograph separations are essentially 'black box' models where only external information is used. The well-instrumented 490 m2 Hydrohill artificial grassland catchment located near Nanjing (China) was used to examine internal catchment processes. Since groundwater levels never...
Applying the scientific method to small catchment studies: Areview of the Panola Mountain experience
R. P. Hooper
2001, Hydrological Processes (15) 2039-2050
A hallmark of the scientific method is its iterative application to a problem to increase and refine the understanding of the underlying processes controlling it. A successful iterative application of the scientific method to catchment science (including the fields of hillslope hydrology and biogeochemistry) has been hindered by two factors....
Pollen-limited reproduction in blue oak: Implications for wind pollination in fragmented populations
E. E. Knapp, M.A. Goedde, K.J. Rice
2001, Oecologia (128) 48-55
Human activities are fragmenting forests and woodlands worldwide, but the impact of reduced tree population densities on pollen transfer in wind-pollinated trees is poorly understood. In a 4-year study, we evaluated relationships among stand density, pollen availability, and seed production in a thinned and fragmented population of blue oak (Quercus...
Aeromagnetic expression of faults that offset basin fill, Albuquerque basin, New Mexico
V. J. S. Grauch, M.R. Hudson, S.A. Minor
2001, Geophysics (66) 707-720
High-resolution aeromagnetic data acquired over the Albuquerque basin show widespread expression of faults that offset basin fill and demonstrate that the aeromagnetic method can be an important hydrogeologic and surficial mapping tool in sediment-filled basins. Aeromagnetic expression of faults is recognized by the common correspondence of linear anomalies to surficial...
Spatial extent of a hydrothermal system at Kilauea Volcano, Hawaii, determined from array analyses of shallow long-period seismicity 1. Method
J. Almendros, B. Chouet, P. Dawson
2001, Journal of Geophysical Research B: Solid Earth (106) 13565-13580
We present a probabilistic method to locate the source of seismic events using seismic antennas. The method is based on a comparison of the event azimuths and slownesses derived from frequency-slowness analyses of array data, with a slowness vector model. Several slowness vector models are considered including both homogeneous and...
Steady state deformation of the Coso Range, east central California, inferred from satellite radar interferometry
C.W. Wicks, W. Thatcher, Francis C. Monastero, M.A. Hasting
2001, Journal of Geophysical Research B: Solid Earth (106) 13769-13780
Observations of deformation from 1992 to 1997 in the southern Coso Range using satellite radar interferometry show deformation rates of up to 35 mm yr−1 in an area ∼10 km by 15 km. The deformation is most likely the result of subsidence in an area around the Coso geothermal field. The...
Identification of a new degradation product of the antifouling agent Irgarol 1051 in natural samples
I. Ferrer, D. Barcelo
2001, Conference Paper, Journal of Chromatography A
A main degradation product of Irgarol [2-(methylthio)-4-(tert-butylamino)-6-(cyclopropylamino)-s-triazine], one of the most widely used compounds in antifouling paints, was detected at trace levels in seawater and sediment samples collected from several marinas on the Mediterranean coast. This degradation product was identified as 2-methylthio-4-tert-butylamino-s-triazine. The unequivocal identification of this compound in seawater...
Rotund versus skinny orogens: Well-nourished or malnourished gold?
R.J. Goldfarb, D.I. Groves, S. Gardoll
2001, Geology (29) 539-542
Orogenic gold vein deposits require a particular conjunction of processes to form and be preserved, and their global distribution can be related to broad-scale, evolving tectonic processes throughout Earth history. A heterogeneous distribution of formation ages for these mineral deposits is marked by two major Precambrian peaks (2800-2555 Ma and...
Geophysical constraints on the location and geometry of the Las Vegas Shear Zone, Nevada
V.E. Langenheim, J. A. Grow, R.C. Jachens, G. L. Dixon, J. J. Miller
2001, Tectonics (20) 189-209
We model the basin configuration beneath Las Vegas Valley, Nevada, on the basis of gravity, drillhole, and seismic reflection data. We locate and characterize the various strands of the Las Vegas Valley Shear Zone (LVVSZ) by variations in basin thickness beneath the valley. The pre-Tertiary bedrock surface is complex, with...
Dynamics of diffuse pollution from US southern watersheds
J.D. Schreiber, R.A. Rebich, C.M. Cooper
2001, Water Research (35) 2534-2542
To understand the effects of diffuse pollution information on the source of pollutants, quantities in transport, mode of transport, transient nature of the pollution event, and most importantly, a consideration of remediation efforts need to be known. For example, water quality research in the Yazoo Basin uplands in Mississippi has...