Publications
Filter Total Items: 2337
New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices New substorm index derived from high-resolution geomagnetic field data at low latitude and its comparison with AE and ASY indices
High-resolution geomagnetic field data (i.e., ≤5 seconds) have recently become more commonly used by space physicists. The data permit the identification of Pi2 pulsations, having periods of 40-150 seconds and irregular waveforms. Pulsations of this type appear clearly in time series from mid- and low-latitude ground stations on the nightside at substorm onset. Therefore, with data from...
Authors
M. Nose, T. Iyemori, M. Takeda, H. Toh, T. Ookawa, G. Cifuentes-Nava, J. Matzka, Jeffrey Love, H. McCreadie, M. Tuncer, J. Curto
Absolute Measurement Session XIII IAGA Workshop Boulder Magnetic Observatory Absolute Measurement Session XIII IAGA Workshop Boulder Magnetic Observatory
The absolute measurement session of the XIII IAGA Workshop was held at the Boulder Magnetic Observatory June 10-13, 2008. Approximately 85 people attended this session. The main focus of the session was for observers to make and compare measurements using DIFlux magnetometers. The session also included absolute measurement training, with lectures and practical training. Also included...
Authors
A. Berarducci, Andy Woods
Movement triggers and remediation in a fracture-dominated translational landslide at the Oregon coast Movement triggers and remediation in a fracture-dominated translational landslide at the Oregon coast
The Johnson Creek landslide is a translational slide in seaward dipping Miocene siltstone and sandstone (Astoria Formation) and an overlying Quaternary marine terrace deposit. The slide terminates in a sea cliff and has a hummocky to nearly horizontal ground surface. The basal slide plane, however, slopes subparallel to the dip of the Miocene rocks, except beneath the back-tilted toe...
Authors
George R. Priest, Jonathan Allan, Alan Niem, Wendy A. Niem, Stephen Dickenson
Missing data and the accuracy of magnetic-observatory hour means Missing data and the accuracy of magnetic-observatory hour means
Analysis is made of the accuracy of magnetic-observatory hourly means constructed from definitive minute data having missing values (gaps). Bootstrap sampling from different data-gap distributions is used to estimate average errors on hourly means as a function of the number of missing data. Absolute and relative error results are calculated for horizontal-intensity, declination, and...
Authors
Jeffrey Love
Total field sensor comparison Total field sensor comparison
During the XIIIth IAGA Workshop (hereafter referred to as “the workshop"), several total field comparison measurements were conducted at the Boulder Magnetic Observatory (BOU). The purpose of these tests was to look for errors within the total field instruments which are considered “absolutes” instruments. The total field measurement is a critical component of the absolute measurement...
Authors
Tim White
Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research Earth's magnetic field complex: U.S. National activities during the Decade of Geopotential Field Research
The US geomagnetism community is supported by NASA, NOAA, USGS, NSF, DOD, and US universities. During the Decade of Geopotential Field Research, inaugurated in 1999 with the launch of the Danish satellite Ørsted on a US rocket, the US community has been involved in satellite mission development and analysis, instrument development, model development, and in the discovery and...
Authors
Michael Purucker, T. Sabaka, W. Kuang, S. Maus, Jeffrey Love
Moderate rates of late Quaternary slip along the northwestern margin of the Basin and Range Province, Surprise Valley fault, northeastern California Moderate rates of late Quaternary slip along the northwestern margin of the Basin and Range Province, Surprise Valley fault, northeastern California
The 86-km-long Surprise Valley normal fault forms part of the active northwestern margin of the Basin and Range province in northeastern California. We use trench mapping and radiocarbon, luminescence, and tephra dating to estimate displacements and timing of the past five surface-rupturing earthquakes on the central part of the fault near Cedarville. A Bayesian OxCal analysis of timing
Authors
Stephen Personius, Anthony Crone, Michael N. Machette, Shannon Mahan, David Lidke
Probabilistic estimation of numbers and costs of future landslides in the San Francisco Bay region Probabilistic estimation of numbers and costs of future landslides in the San Francisco Bay region
We used historical records of damaging landslides triggered by rainstorms and a newly developed Probabilistic Landslide Assessment Cost Estimation System (PLACES) to estimate the numbers and direct costs of future landslides in the 10-county San Francisco Bay region. Historical records of damaging landslides in the region are incomplete. Therefore, our estimates of numbers and costs of...
Authors
R. A. Crovelli, J. Coe
Size distributions and failure initiation of submarine and subaerial landslides Size distributions and failure initiation of submarine and subaerial landslides
Landslides are often viewed together with other natural hazards, such as earthquakes and fires, as phenomena whose size distribution obeys an inverse power law. Inverse power law distributions are the result of additive avalanche processes, in which the final size cannot be predicted at the onset of the disturbance. Volume and area distributions of submarine landslides along the U.S...
Authors
Uri S. ten Brink, R. Barkan, B.D. Andrews, J.D. Chaytor
Relations between hydrology and velocity of a continuously moving landslide-evidence of pore-pressure feedback regulating landslide motion? Relations between hydrology and velocity of a continuously moving landslide-evidence of pore-pressure feedback regulating landslide motion?
We measured displacement, pore-water pressure, and climatic conditions for 3 years at the continuously moving Slumgullion landslide in Colorado, USA. The landslide accelerated when pore-water pressure increased within the landslide body, but this occurred as pore-water pressure decreased along the landslide margin. The decrease probably occurred in response to shear-induced soil dilation...
Authors
W.H. Schulz, J.P. McKenna, J.D. Kibler, G. Biavati
On the reported magnetic precursor of the 1993 guam earthquake On the reported magnetic precursor of the 1993 guam earthquake
Using 1-second magnetometer data recorded 67 km from the epicenter of the 1993 Mw 7.7 Guam earthquake, Hayakawa et al. (1996) and Miyahara et al. (1999) identify anomalous precursory changes in ultra-low frequency magnetic polarization (the ratio of vertical to horizontal field components). In a check of their results, we compare their data (GAM) with 1-second data from the Kakioka...
Authors
J.N. Thomas, J.J. Love, M.J.S. Johnston, K. Yumoto
Landsliding in partially saturated materials Landsliding in partially saturated materials
Rainfall‐induced landslides are pervasive in hillslope environments around the world and among the most costly and deadly natural hazards. However, capturing their occurrence with scientific instrumentation in a natural setting is extremely rare. The prevailing thinking on landslide initiation, particularly for those landslides that occur under intense precipitation, is that the failure...
Authors
J. W. Godt, R.L. Baum, N. Lu