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  • 1
    In: Journal of Allergy and Clinical Immunology, Elsevier BV, Vol. 138, No. 2 ( 2016-08), p. 367-374.e2
    Type of Medium: Online Resource
    ISSN: 0091-6749
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2016
    detail.hit.zdb_id: 2006613-2
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  • 2
    Online Resource
    Online Resource
    Acoustical Society of America (ASA) ; 1996
    In:  The Journal of the Acoustical Society of America Vol. 100, No. 4_Supplement ( 1996-10-01), p. 2613-2613
    In: The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 100, No. 4_Supplement ( 1996-10-01), p. 2613-2613
    Abstract: Simultaneous observations of internal wave activity and acoustic wave propagation in 70 m water in the Yellow Sea were made in the late summer of 1996. The objective of the experiment was to validate the predicated modal coupling and resulting fluctuations and alterations in propagation loss induced by shallow-water internal waves. Propagation over distances up to 50 km (using narrow- and broadband sources over the frequency range of 50 Hz to 6 kHz) was measured with moored and suspended arrays which spanned the water column. Internal wave activity was monitored using several thermistor chains. Details of the experiment and preliminary data will be presented. [Work supported by ONR and the Chinese Academy of Sciences.]
    Type of Medium: Online Resource
    ISSN: 0001-4966 , 1520-8524
    RVK:
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 1996
    detail.hit.zdb_id: 1461063-2
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  • 3
    Online Resource
    Online Resource
    Acoustical Society of America (ASA) ; 1997
    In:  The Journal of the Acoustical Society of America Vol. 101, No. 5_Supplement ( 1997-05-01), p. 3015-3015
    In: The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 101, No. 5_Supplement ( 1997-05-01), p. 3015-3015
    Abstract: Simultaneous observations of internal wave activity and acoustic wave propagation in 70-m water in the Yellow Sea were made in the late summer of 1996. The primary objective of this experiment was to validate the predicated modal coupling and fluctuations induced by shallow-water internal waves. The Yellow Sea provides an ideal environment for such research because it has a very flat and homogeneous bottom and a very strong, sharp thermocline. The environment lends itself to relatively simple models for both the acoustic field and the internal wave field. Propagation was measured over distances up to 55 km in the frequency range of 50 Hz–5 kHz. The receivers were three moored and two suspended hydrophone arrays. Internal wave activity was monitored using thermistor chains, SAR satellite imagery, and high-frequency sonar. Propagation data were taken as a function of range, as a function of time at a fixed range, and as a function of azimuth in the presence of differing levels of internal wave activity. Supporting environmental data obtained during the experiment include ADCP, bottom profile and surface wave-height spectra, and bottom coring. Preliminary data on internal wave field, sound propagation, reverberation, and bottom acoustic parameters will be presented. [Work supported by ONR and the Chinese Academy of Sciences.]
    Type of Medium: Online Resource
    ISSN: 0001-4966 , 1520-8524
    RVK:
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 1997
    detail.hit.zdb_id: 1461063-2
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  • 4
    In: Proceedings of the National Academy of Sciences, Proceedings of the National Academy of Sciences, Vol. 108, No. 29 ( 2011-07-19), p. 11983-11988
    Abstract: High-throughput sequencing technology enables population-level surveys of human genomic variation. Here, we examine the joint allele frequency distributions across continental human populations and present an approach for combining complementary aspects of whole-genome, low-coverage data and targeted high-coverage data. We apply this approach to data generated by the pilot phase of the Thousand Genomes Project, including whole-genome 2–4× coverage data for 179 samples from HapMap European, Asian, and African panels as well as high-coverage target sequencing of the exons of 800 genes from 697 individuals in seven populations. We use the site frequency spectra obtained from these data to infer demographic parameters for an Out-of-Africa model for populations of African, European, and Asian descent and to predict, by a jackknife-based approach, the amount of genetic diversity that will be discovered as sample sizes are increased. We predict that the number of discovered nonsynonymous coding variants will reach 100,000 in each population after ∼1,000 sequenced chromosomes per population, whereas ∼2,500 chromosomes will be needed for the same number of synonymous variants. Beyond this point, the number of segregating sites in the European and Asian panel populations is expected to overcome that of the African panel because of faster recent population growth. Overall, we find that the majority of human genomic variable sites are rare and exhibit little sharing among diverged populations. Our results emphasize that replication of disease association for specific rare genetic variants across diverged populations must overcome both reduced statistical power because of rarity and higher population divergence.
    Type of Medium: Online Resource
    ISSN: 0027-8424 , 1091-6490
    RVK:
    RVK:
    Language: English
    Publisher: Proceedings of the National Academy of Sciences
    Publication Date: 2011
    detail.hit.zdb_id: 209104-5
    detail.hit.zdb_id: 1461794-8
    SSG: 11
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    Acoustical Society of America (ASA) ; 2002
    In:  The Journal of the Acoustical Society of America Vol. 112, No. 5_Supplement ( 2002-11-01), p. 2361-2361
    In: The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 112, No. 5_Supplement ( 2002-11-01), p. 2361-2361
    Abstract: Time series data collected on the APL–UW/URI VLA in the East China Sea as part of the Asian Sea International Acoustics Experiment are analyzed for the information they contain on the characteristics of the seabed. Sound generated by explosive sources deployed by the IOA propagates in a shallow water wave guide under downward refracting conditions, making the received field at the VLA sensitive to the structure of the seabed. A broadband normal mode approach is used to model the measured time series in the 10–500 Hz band. The complex multipath arrival pattern as a function of source–receiver range and source depth allows one to infer certain characteristics of the seabed without the aid of an inversion approach. A finer specification of the seabed, including the determination of the statistics of the geoacoustic parameters is achieved by a simulated annealing inversion methodology. The sensitivity of the acoustic propagation to the elastic properties of the seabed is also investigated along with the nature of the attenuation. The estimated properties of the seabed are compared with independent geophysical measurements and those that can be obtained from reverberation data. [Work supported by ONR.]
    Type of Medium: Online Resource
    ISSN: 0001-4966 , 1520-8524
    RVK:
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 2002
    detail.hit.zdb_id: 1461063-2
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  • 6
    Online Resource
    Online Resource
    Acoustical Society of America (ASA) ; 2007
    In:  Acoustics Today Vol. 3, No. 1 ( 2007), p. 23-
    In: Acoustics Today, Acoustical Society of America (ASA), Vol. 3, No. 1 ( 2007), p. 23-
    Type of Medium: Online Resource
    ISSN: 1557-0215
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 2007
    detail.hit.zdb_id: 2466509-5
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  • 7
    In: Geological Survey of Denmark and Greenland Bulletin, Geological Survey of Denmark and Greenland, Vol. 43 ( 2019-07-01)
    Abstract: The landslide of 17 June 2017 at Karrat Fjord, central West Greenland, triggered a tsunami that caused four fatalities. The catastrophe highlighted the need for a better understanding of landslides in Greenland and initiated a recent nation-wide landslide screening project led by the Geological Survey of Denmark and Greenland (GEUS; see also Svennevig (2019) this volume). This paper describes an approach for compiling freely available data to improve GEUS’ capability to monitor active landslides in remote areas of the Arctic in near real time. Data include seismological records, space borne Synthetic Aperture Radar (SAR) data and multispectral optical satellite imagery. The workflow was developed in 2018 as part of a collaboration between GEUS and scientists from the Technical University of Denmark (DTU). This methodology provides a model through which GEUS will be able to monitor active landslides and provide relevant knowledge to the public and authorities in the event of future landslides that pose a risk to human life and infrastructure in Greenland. We use a minor event on 26 March 2018, near the site of the Karrat 2017 landslide, as a case study to demonstrate 1) the value of multidisciplinary approaches and 2) that the area around the landslide has continued to be periodically active since the main landslide in 2017.
    Type of Medium: Online Resource
    ISSN: 1604-8156 , 1904-4666
    URL: Issue
    Language: Unknown
    Publisher: Geological Survey of Denmark and Greenland
    Publication Date: 2019
    detail.hit.zdb_id: 2133781-0
    detail.hit.zdb_id: 2390893-2
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  • 8
    Online Resource
    Online Resource
    Geological Survey of Denmark and Greenland ; 2014
    In:  Geological Survey of Denmark and Greenland Bulletin Vol. 31 ( 2014-06-25), p. 75-78
    In: Geological Survey of Denmark and Greenland Bulletin, Geological Survey of Denmark and Greenland, Vol. 31 ( 2014-06-25), p. 75-78
    Abstract: Two earthquake swarms have been detected in Greenland. One occurred on the island of Disko in August 2010, the other one was active from January 2008 to June 2009 near the South-East Greenland coast c. 200 km south of Tasiilaq. An earthquake swarm is defined as a series of earthquakes of similar magnitude located within a small area. The magnitude of the largest earthquakes in a swarm is typically less than 4 (Ma & Eaton 2009). Swarm activity is distinctly different from the more common mainshock–aftershock activity, which is characterised by one large earthquake (mainshock) followed by a series of smaller aftershocks. Earthquake swarms mainly occur in areas with tectonic and/or volcanic activity (Stykes 1970), but intraplate swarms are also found in otherwise stable environments (Gregersen 1979; Atakan et al. 1994; Uski et al. 2006; Ma & Eaton 2009). Geological boundaries and old fault zones appear to be a common setting for intraplate earthquake swarms. Earthquake swarms have previously been detected in North and North-East Greenland (Gregersen 1979) at a time when the seismograph coverage was very sparse. It was concluded that the earthquake swarms were caused by tectonic stresses in and around old sedimentary basins near the continental margin.
    Type of Medium: Online Resource
    ISSN: 1604-8156 , 1904-4666
    Language: Unknown
    Publisher: Geological Survey of Denmark and Greenland
    Publication Date: 2014
    detail.hit.zdb_id: 2133781-0
    detail.hit.zdb_id: 2390893-2
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  • 9
    In: Earth Surface Dynamics, Copernicus GmbH, Vol. 8, No. 4 ( 2020-12-08), p. 1021-1038
    Abstract: Abstract. The 17 June 2017 rock avalanche in the Karrat Fjord, West Greenland, caused a tsunami that flooded the nearby village of Nuugaatsiaq and killed four people. The disaster was entirely unexpected since no previous records of large rock slope failures were known in the region, and it highlighted the need for better knowledge of potentially hazardous rock slopes in remote Arctic regions. The aim of the paper is to explore our ability to detect and locate unstable rock slopes in remote Arctic regions with difficult access. We test this by examining the case of the 17 June 2017 Karrat rock avalanche. The workflow we apply is based on a multidisciplinary analysis of freely available data comprising seismological records, Sentinel-1 spaceborne synthetic-aperture radar (SAR) data, and Landsat and Sentinel-2 optical satellite imagery, ground-truthed with limited fieldwork. Using this workflow enables us to reconstruct a timeline of rock slope failures on the coastal slope here collectively termed the Karrat Landslide Complex. Our analyses show that at least three recent rock avalanches occurred in the Karrat Landslide Complex: Karrat 2009, Karrat 2016, and Karrat 2017. The latter is the source of the abovementioned tsunami, whereas the first two are described here in detail for the first time. All three are interpreted as having initiated as dip-slope failures. In addition to the recent rock avalanches, older rock avalanche deposits are observed, demonstrating older (Holocene) periods of activity. Furthermore, three larger unstable rock slopes that may pose a future hazard are described. A number of non-tectonic seismic events confined to the area are interpreted as recording rock slope failures. The structural setting of the Karrat Landslide Complex, namely dip slope, is probably the main conditioning factor for the past and present activity, and, based on the temporal distribution of events in the area, we speculate that the possible trigger for rock slope failures is permafrost degradation caused by climate warming. The results of the present work highlight the benefits of a multidisciplinary approach, based on freely available data, to studying unstable rock slopes in remote Arctic areas under difficult logistical field conditions and demonstrate the importance of identifying minor precursor events to identify areas of future hazard.
    Type of Medium: Online Resource
    ISSN: 2196-632X
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2020
    detail.hit.zdb_id: 2736054-4
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  • 10
    Online Resource
    Online Resource
    Acoustical Society of America (ASA) ; 1988
    In:  The Journal of the Acoustical Society of America Vol. 83, No. 6 ( 1988-06-01), p. 2175-2179
    In: The Journal of the Acoustical Society of America, Acoustical Society of America (ASA), Vol. 83, No. 6 ( 1988-06-01), p. 2175-2179
    Abstract: The frequency dispersion of hour-long acoustic tonal signals, stepped in frequency between 25 and 200 Hz, is measured via the covariance method. This method is computationally efficient and relatively unexploited for this purpose. The signals are from MIZEX 84 and have propagated through a partially ice-covered 100-km path. Source/receive drift-induced Doppler shift compares favorably with available navigational data. The dispersion is expressed in terms of the parameter ν, which is a function of a host of possible oceanic processes dynamically perturbing the sound field.
    Type of Medium: Online Resource
    ISSN: 0001-4966 , 1520-8524
    RVK:
    Language: English
    Publisher: Acoustical Society of America (ASA)
    Publication Date: 1988
    detail.hit.zdb_id: 1461063-2
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