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broad-band noise

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Journal Article
Published: 01 March 1971
Canadian Journal of Earth Sciences (1971) 8 (3): 347–360.
... recording on sea ice was plagued by unusually high background noise levels which could be attributed to low frequency (below 1 Hz) oscillations of the ice pans and to the broad-band noise generated by frequent ice cracking. It was discovered, and is shown theoretically, that seismic wave propagating through...
Image
The Brownian noise of the Seismic Experiment for Interior Structure–Very Broad Band (SEIS‐VBB) has been calculated assuming constant internal friction and considering viscous damping from the chamber pressure at Mars launch. The Brownian noise estimate is below that of the SEIS‐VBB noise model for Mars deployment (Lognonné et al., 2020), but is higher than the International Lunar Network (ILN) requirement (ILN, 2009). The Streckeisen Seismometer (STS‐1) noise is included for reference (Ringler and Hutt, 2010). A Brownian noise projection of the SEIS‐VBB for lunar operation is higher than the ILN requirement. The color version of this figure is available only in the electronic edition.
Published: 02 November 2021
Figure 4. The Brownian noise of the Seismic Experiment for Interior Structure–Very Broad Band (SEIS‐VBB) has been calculated assuming constant internal friction and considering viscous damping from the chamber pressure at Mars launch. The Brownian noise estimate is below that of the SEIS‐VBB
Journal Article
Published: 21 March 2017
Bulletin of the Seismological Society of America (2017) 107 (3): 1402–1412.
... ) or low‐frequency ( < 0.05 Hz ) bands. In this study, we use modern high‐quality broadband (BB) and very broadband (VBB) seismometers installed at depths ranging from 1.5 to 188 m at the Albuquerque Seismological Laboratory to evaluate noise attenuation as a function of depth over a broad range...
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Journal Article
Published: 01 February 1989
Bulletin of the Seismological Society of America (1989) 79 (1): 172–179.
...Michael A. H. Hedlin; John A. Orcutt Abstract A study of seafloor and island stations shows that for the frequency band 0.1 to 10 Hz the seismic noise levels on islands are comparable to the levels on the seafloor. The microseism peak at the seafloor appears to be comparable to the highest levels...
Image
Comparison of horizontal-to-vertical-spectral monitoring (HVSR) of ambient noise with the spectral ratio of an eastern Canadian earthquake at a broad-band seismic recording station within the City of Ottawa, Ontario. The site is situated on 95 m of soft Holocene Leda clay overlying firm lower Paleozoic shale; the boundary presents a significant shear-wave impedance ratio. Both the earthquake event and the HVSR noise monitor indicate a large-amplitude resonant effect at the relatively low frequency of 0.77 Hz.
Published: 01 August 2010
Figure 11. Comparison of horizontal-to-vertical-spectral monitoring (HVSR) of ambient noise with the spectral ratio of an eastern Canadian earthquake at a broad-band seismic recording station within the City of Ottawa, Ontario. The site is situated on 95 m of soft Holocene Leda clay overlying
Journal Article
Journal: Geophysics
Published: 01 December 1996
Geophysics (1996) 61 (6): 1789–1803.
... for shallow-reflection surveys where high resolution and cost-effectiveness are critical. A low-power impact source transmits a few to several hundred high-frequency broad-band seismic pulses during several seconds of recording time according to a deterministic coding scheme. The coding scheme consists...
Journal Article
Journal: Geophysics
Published: 26 February 2024
Geophysics (2024) 89 (3): V209–V217.
... spectrum, noise suppression is achieved. Extensive testing with theoretical models, synthetic shot gathers, and field data indicate a notable improvement in the signal-to-noise ratio (S/N) compared with the traditional band-pass filtering method. This method proves particularly effective for enhancing...
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Journal Article
Published: 02 November 2021
Bulletin of the Seismological Society of America (2021) 111 (6): 3065–3075.
...Figure 4. The Brownian noise of the Seismic Experiment for Interior Structure–Very Broad Band (SEIS‐VBB) has been calculated assuming constant internal friction and considering viscous damping from the chamber pressure at Mars launch. The Brownian noise estimate is below that of the SEIS‐VBB...
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Journal Article
Published: 28 November 2017
Bulletin of the Seismological Society of America (2018) 108 (1): 248–259.
... correlation with the significant wave height computed from WAVEWATCH III. The ambient noise is down to − 140 dB for the band from 0.1 to 1 s, which provides the best signal‐to‐noise ratio level for local earthquakes. For very short periods ( < 0.1 s ), the ambient noise level increases to − 120 dB...
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Image
The electromagnetic spectrum (EMS) is shown in wavelength (mm) on the X-axis from visible through the shortwave infrared (SWIR) and relative reflectance on the Y-axis. The naked eye sees from about 0.4 to 0.7 mm. Typical reflectance spectra for vegetation and dry soil are shown. Also shown are the bars representing the different sensors, vertically offset for comparison and implying no variation in the amount of energy detected. Notice the broad spectrum covered by panchromatic film. Similarly, single panchromatic digital bands are broad within the visible to near IR for increased signal-to-noise.
Published: 01 July 2004
shown are the bars representing the different sensors, vertically offset for comparison and implying no variation in the amount of energy detected. Notice the broad spectrum covered by panchromatic film. Similarly, single panchromatic digital bands are broad within the visible to near IR for increased
Journal Article
Published: 26 October 2021
Bulletin of the Seismological Society of America (2021) 111 (6): 2924–2950.
.... * Corresponding author: [email protected] 25 February 2021 © Seismological Society of America Seismic events with energy above 2 Hz commonly excite a broad resonance at 2.4 Hz, which appears to be decoupled from local noise disturbances. Seismic events do not excite any other...
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Journal Article
Published: 01 July 1963
Bulletin of the Seismological Society of America (1963) 53 (4): 765–781.
... and seas over a broad area were weakly reflected as small changes in the amplitude of the ocean bottom noise. Similar small amplitude variations were recorded at Bermuda, 150 nautical miles to the northeast, but the absolute Bermuda amplitudes were an order of magnitude less than those at the noisiest...
Image
High-pressure spectra in the OH stretching mode region, with increasing pressure from bottom to top. Notice the increase of bandwidth at the maximum pressure due to the onset of solidification of the pressure medium. Dotted lines underline the nearly parallel behavior of two OH bands assigned to the in-phase stretching mode of the outer OH and stretching mode of inner OH at 3672 and 3698 cm−1, respectively, while the thick arrow illustrates the strong pressure dependence of a third broad band masked at low pressure under the two former ones. Sharp spikes are noise with random occurrence at high counting times.
Published: 01 February 2006
assigned to the in-phase stretching mode of the outer OH and stretching mode of inner OH at 3672 and 3698 cm −1 , respectively, while the thick arrow illustrates the strong pressure dependence of a third broad band masked at low pressure under the two former ones. Sharp spikes are noise with random
Journal Article
Journal: Geophysics
Published: 04 April 2016
Geophysics (2016) 81 (3): R57–R74.
... impedance demonstrated the efficacy of the method, even when a significant amount of noise was added to the data. The emergence of consistent estimates of impedance, approximating the original impedance, from synthetic data generated for several frequency bands has inspired our confidence in the method...
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Journal Article
Journal: The Leading Edge
Published: 01 March 2021
The Leading Edge (2021) 40 (3): 194–201.
... and poroelastic response of rocks in a broad frequency range from subhertz to megahertz, potentially closing the frequency gap between traditional ultrasonic characterization and properties of interest in the seismic frequency band. In exploration settings, electric current dipole/bipole sources, or novel...
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Journal Article
Journal: Geophysics
Published: 01 June 1966
Geophysics (1966) 31 (3): 576–605.
... in other applications, e.g., mapping broad fault zones, the repeatability is notoriously poor. In an endeavor to elucidate the factors controlling repeatability of AFMAG dip angle readings, we have conducted a continuing program of research in the State of California since 1961. Among the items we have...
Journal Article
Published: 01 December 1976
Bulletin of the Seismological Society of America (1976) 66 (6): 2049–2068.
... developed broad-band borehole seismometer and a software-controlled recording system. The seismometers are being installed at a depth of 100 meters to avoid wind-generated noise in the long-period band. A seismometer output that is flat in acceleration between periods of 1 and 50 sec is used to produce both...
Series: EMU Notes in Mineralogy series
Published: 01 January 2019
DOI: 10.1180/EMU-notes.20.12
EISBN: 9780903056625
... and the underlying stratum, both dominated by a very strong and broad carbonyl stretching absorption and by alkyl stretches. The broad band corresponding to the distribution of C=O stretching vibrations is centred at 1.709 cm −1 , a value intermediate between that of aged drying oils at higher wavenumbers...
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Journal Article
Published: 13 September 2016
Bulletin of the Seismological Society of America (2016) 106 (5): 1926–1938.
... deployments. We make coda envelope‐amplitude measurements for 2247 events recorded by 68 stations over 13 narrow frequency bands ranging between 0.03 and 8 Hz. The absolute scaling of these spectra was calculated based on independent waveform modeling solutions of the moment magnitudes for a subset...
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Journal Article
Published: 01 May 2009
Earthquake Spectra (2009) 25 (2): 257–276.
..., is produced by a dislocation strip sweeping the fault area. In its high-frequency part, it is defined by random local slip history, represented by a segment of pulsed noise. Subsource signals are convolved with broad-band Green functions for a layered half-space, and stacked, resulting in the ground motion...