Publications
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EAARL coastal topography - Assateague Island National Seashore, Maryland and Virginia, 2010 EAARL coastal topography - Assateague Island National Seashore, Maryland and Virginia, 2010
This DVD contains lidar-derived bare-earth (BE) and first-surface (FS) topography GIS datasets of a portion of the Assateague Island National Seashore in Maryland and Virginia. These datasets were acquired on March 19 and 24, 2010.
Authors
J.M. Bonisteel-Cormier, Amar Nayegandhi, C. W. Wright, J. C. Brock, D.B. Nagle, Saisudha Vivekanandan, E.S. Klipp, Xan Fredericks, Sara Stevens
Estimating earthquake-rupture rates on a fault or fault system Estimating earthquake-rupture rates on a fault or fault system
Previous approaches used to determine the rates of different earthquakes on a fault have made assumptions regarding segmentation, have been difficult to document and reproduce, and have lacked the ability to satisfy all available data constraints. We present a relatively objective and reproducible inverse methodology for determining the rate of different ruptures on a fault or fault...
Authors
E. H. Field, M.T. Page
High-frequency filtering of strong-motion records High-frequency filtering of strong-motion records
The influence of noise in strong-motion records is most problematic at low and high frequencies where the signal to noise ratio is commonly low compared to that in the mid-spectrum. The impact of low-frequency noise (5 Hz) on computed pseudo-absolute response spectral accelerations (PSAs). In contrast to the case of low-frequency noise our analysis shows that filtering to remove high...
Authors
J. Douglas, D.M. Boore
Spring-fall asymmetry of substorm strength, geomagnetic activity and solar wind: Implications for semiannual variation and solar hemispheric asymmetry Spring-fall asymmetry of substorm strength, geomagnetic activity and solar wind: Implications for semiannual variation and solar hemispheric asymmetry
We study the seasonal variation of substorms, geomagnetic activity and their solar wind drivers in 1993–2008. The number of substorms and substorm mean duration depict an annual variation with maxima in Winter and Summer, respectively, reflecting the annual change of the local ionosphere. In contradiction, substorm mean amplitude, substorm total efficiency and global geomagnetic activity...
Authors
K. Mursula, E. Tanskanen, J.J. Love
Economic resilience lessons from the ShakeOut earthquake scenario Economic resilience lessons from the ShakeOut earthquake scenario
Following a damaging earthquake, “business interruption” (BI)—reduced production of goods and services—begins and continues long after the ground shaking stops. Economic resilience reduces BI losses by making the best use of the resources available at a given point in time (static resilience) or by speeding recovery through repair and reconstruction (dynamic resilience), in contrast to...
Authors
A. Wein, A. Rose
Recovering from the ShakeOut earthquake Recovering from the ShakeOut earthquake
Recovery from an earthquake like the M7.8 ShakeOut Scenario will be a major endeavor taking many years to complete. Hundreds of Southern California municipalities will be affected; most lack recovery plans or previous disaster experience. To support recovery planning this paper 1) extends the regional ShakeOut Scenario analysis into the recovery period using a recovery model, 2)...
Authors
Anne Wein, Laurie Johnson, Richard Bernknopf
Deep rock damage in the san andreas fault revealed by P- and S-type fault-zone-guided waves Deep rock damage in the san andreas fault revealed by P- and S-type fault-zone-guided waves
Damage to fault-zone rocks during fault slip results in the formation of a channel of low seismic-wave velocities. Within such channels guided seismic waves, denoted by Fg, can propagate. Here we show with core samples, well logs and Fg-waves that such a channel is crossed by the SAFOD (San Andreas Fault Observatory at Depth) borehole at a depth of 2.7 km near Parkfield, California, USA...
Authors
William L. Ellsworth, Peter E. Malin
The 16 May 1909 northern Great Plains earthquake The 16 May 1909 northern Great Plains earthquake
The largest historical earthquake in the northern Great Plains occurred on 16 May 1909. Our analysis of intensity assignments places the earthquake location (48.81° N, 105.38° W) close to the Montana–Saskatchewan border with an intensity magnitude MI of 5.3–5.4. Observations from two seismic observatories in Europe give an average Ms value of 5.3. The 1909 earthquake is near an alignment...
Authors
W. H. Bakun, M. C. Stickney, Gary C. Rogers
Reply to "Comment on 'A model of earthquake triggering probabilities and application to dynamic deformations constrained by ground motion observations' by Ross Stein" Reply to "Comment on 'A model of earthquake triggering probabilities and application to dynamic deformations constrained by ground motion observations' by Ross Stein"
No abstract available.
Authors
J. Gomberg, K. Felzer
Estimating surface faulting impacts from the shakeout scenario earthquake Estimating surface faulting impacts from the shakeout scenario earthquake
An earthquake scenario, based on a kinematic rupture model, has been prepared for a Mw 7.8 earthquake on the southern San Andreas Fault. The rupture distribution, in the context of other historic large earthquakes, is judged reasonable for the purposes of this scenario. This model is used as the basis for generating a surface rupture map and for assessing potential direct impacts on...
Authors
J.A. Treiman, D.J. Pontib
Are secular correlations between sunspots, geomagnetic activity, and global temperature significant? Are secular correlations between sunspots, geomagnetic activity, and global temperature significant?
Recent studies have led to speculation that solar‐terrestrial interaction, measured by sunspot number and geomagnetic activity, has played an important role in global temperature change over the past century or so. We treat this possibility as an hypothesis for testing. We examine the statistical significance of cross‐correlations between sunspot number, geomagnetic activity, and global...
Authors
Jeffrey J. Love, K. Mursula, V.C. Tsai, D. M. Perkins
Rainfall intensity-duration thresholds for postfire debris-flow emergency-response planning Rainfall intensity-duration thresholds for postfire debris-flow emergency-response planning
Following wildfires, emergency-response and public-safety agencies can be faced with evacuation and resource-deployment decisions well in advance of coming winter storms and during storms themselves. Information critical to these decisions is provided for recently burned areas in the San Gabriel Mountains of southern California. A compilation of information on the hydrologic response to...
Authors
S.H. Cannon, E.M. Boldt, J.L. Laber, J. W. Kean, D.M. Staley