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  • 1
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Solid Earth Vol. 95, No. B10 ( 1990-09-10), p. 15303-15318
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 95, No. B10 ( 1990-09-10), p. 15303-15318
    Kurzfassung: To study the resolving power of teleseismic P waveforms for receiver structure, we model synthetic waveforms using a time domain waveform inversion scheme beginning with a range of initial models to estimate the range of acceptable velocity structures. To speed up the waveform inversions, we implement Randall's (1989) efficient algorithms for calculating differential seismograms and include a smoothness constraint on all the resulting velocity models utilizing the “jumping” inversion technique of Shaw and Orcutt (1985). We present the results of more than 235 waveform inversions for one‐dimensional velocity structures that indicate that the primary sensitivity of a receiver function is to high wavenumber velocity changes, and a depth‐velocity product, not simply velocity. The range of slownesses in a typical receiver function study does not appear to be broad enough to remove the depth‐velocity ambiguity; the inclusion of a priori information is necessary. We also present inversion results for station RSCP, located in the Cumberland Plateau, Tennessee. Our results are similar to those from a previous study by Owens et al. (1984) and demonstrate the uncertainties in the resulting velocity estimate more clearly.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1990
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    In: The Astrophysical Journal Supplement Series, American Astronomical Society, Vol. 265, No. 1 ( 2023-03-01), p. 1-
    Kurzfassung: NASA’s Transiting Exoplanet Survey Satellite (TESS) mission promises to improve our understanding of hot Jupiters by providing an all-sky, magnitude-limited sample of transiting hot Jupiters suitable for population studies. Assembling such a sample requires confirming hundreds of planet candidates with additional follow-up observations. Here we present 20 hot Jupiters that were detected using TESS data and confirmed to be planets through photometric, spectroscopic, and imaging observations coordinated by the TESS Follow-up Observing Program. These 20 planets have orbital periods shorter than 7 days and orbit relatively bright FGK stars (10.9 〈 G 〈 13.0). Most of the planets are comparable in mass to Jupiter, although there are four planets with masses less than that of Saturn. TOI-3976b, the longest-period planet in our sample ( P = 6.6 days), may be on a moderately eccentric orbit ( e = 0.18 ± 0.06), while observations of the other targets are consistent with them being on circular orbits. We measured the projected stellar obliquity of TOI-1937A b, a hot Jupiter on a 22.4 hr orbit with the Rossiter–McLaughlin effect, finding the planet’s orbit to be well aligned with the stellar spin axis (∣ λ ∣ = 4.°0 ± 3.°5). We also investigated the possibility that TOI-1937 is a member of the NGC 2516 open cluster but ultimately found the evidence for cluster membership to be ambiguous. These objects are part of a larger effort to build a complete sample of hot Jupiters to be used for future demographic and detailed characterization work.
    Materialart: Online-Ressource
    ISSN: 0067-0049 , 1538-4365
    RVK:
    Sprache: Unbekannt
    Verlag: American Astronomical Society
    Publikationsdatum: 2023
    ZDB Id: 2006860-8
    ZDB Id: 2207650-5
    SSG: 16,12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    In: The Astronomical Journal, American Astronomical Society, Vol. 163, No. 3 ( 2022-03-01), p. 120-
    Kurzfassung: Giant planets on short-period orbits are predicted to be inflated and eventually engulfed by their host stars. However, the detailed timescales and stages of these processes are not well known. Here, we present the discovery of three hot Jupiters ( P 〈 10 days) orbiting evolved, intermediate-mass stars ( M ⋆ ≈ 1.5 M ⊙ , 2 R ⊙ 〈 R ⋆ 〈 5 R ⊙ ). By combining TESS photometry with ground-based photometry and radial velocity measurements, we report masses and radii for these three planets of between 0.4 and 1.8 M J and 0.8 and 1.8 R J . TOI-2337b has the shortest period ( P = 2.99432 ± 0.00008 days) of any planet discovered around a red giant star to date. Both TOI-4329b and TOI-2669b appear to be inflated, but TOI-2337b does not show any sign of inflation. The large radii and relatively low masses of TOI-4329b and TOI-2669b place them among the lowest density hot Jupiters currently known, while TOI-2337b is conversely one of the highest. All three planets have orbital eccentricities of below 0.2. The large spread in radii for these systems implies that planet inflation has a complex dependence on planet mass, radius, incident flux, and orbital properties. We predict that TOI-2337b has the shortest orbital decay timescale of any planet currently known, but do not detect any orbital decay in this system. Transmission spectroscopy of TOI-4329b would provide a favorable opportunity for the detection of water, carbon dioxide, and carbon monoxide features in the atmosphere of a planet orbiting an evolved star, and could yield new information about planet formation and atmospheric evolution.
    Materialart: Online-Ressource
    ISSN: 0004-6256 , 1538-3881
    RVK:
    Sprache: Unbekannt
    Verlag: American Astronomical Society
    Publikationsdatum: 2022
    ZDB Id: 2207625-6
    ZDB Id: 2003104-X
    SSG: 16,12
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    In: Earth and Planetary Science Letters, Elsevier BV, Vol. 289, No. 1-2 ( 2010-1), p. 145-155
    Materialart: Online-Ressource
    ISSN: 0012-821X
    RVK:
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2010
    ZDB Id: 300203-2
    ZDB Id: 1466659-5
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 125, No. 5 ( 2020-05)
    Kurzfassung: High‐resolution teleseismic P wave tomography reveals the detailed structure of the subducted Nazca slab to lower mantle depths A new, comprehensive Nazca slab model is produced from the trench to 1,100 km depth Lower mantle slab penetration occurs along the entire South American margin, inconsistent with variable upper plate shortening
    Materialart: Online-Ressource
    ISSN: 2169-9313 , 2169-9356
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2020
    ZDB Id: 2016813-5
    ZDB Id: 161666-3
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1985
    In:  Geophysical Research Letters Vol. 12, No. 9 ( 1985-09), p. 565-568
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 12, No. 9 ( 1985-09), p. 565-568
    Materialart: Online-Ressource
    ISSN: 0094-8276
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1985
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1988
    In:  Geophysical Research Letters Vol. 15, No. 6 ( 1988-06), p. 613-616
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 15, No. 6 ( 1988-06), p. 613-616
    Kurzfassung: Broadband receiver functions determined from teleseismic P‐waveforms recorded at two seismic stations in eastern Kazakh, U.S.S.R., are inverted for the vertical velocity structure beneath the stations. The detailed broadband receiver functions are obtained by stacking source‐equalized radial components of teleseismic P‐waveforms. A time‐domain inversion of the radial receiver function is used to determine the structure assuming a crustal model parameterized by flat‐lying, homogeneous layers. The general features of the inversion results are: a complex shallow crust, velocities less than 6 km/s in the upper crust, a high velocity (6.9‐7.5 km/s) lower crust, and a Moho that varies between 47 and 57 km depth. These results compare favorably with a composite velocity model from Deep Seismic Sounding data, but show lower velocities in the upper crust, and higher velocities in the lower crust. The results indicate that the crust in this region is relatively uniform, however the nature and depth of the Moho changes significantly across the region. The receiver function inversion structure for the Kazakh sites is similar to a published receiver function structure for a site on the Canadian Shield.
    Materialart: Online-Ressource
    ISSN: 0094-8276 , 1944-8007
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1988
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
    Online-Ressource
    Online-Ressource
    Geological Society of America ; 1994
    In:  Geology Vol. 22, No. 11 ( 1994), p. 1003-
    In: Geology, Geological Society of America, Vol. 22, No. 11 ( 1994), p. 1003-
    Materialart: Online-Ressource
    ISSN: 0091-7613
    Sprache: Englisch
    Verlag: Geological Society of America
    Publikationsdatum: 1994
    ZDB Id: 184929-3
    ZDB Id: 2041152-2
    SSG: 13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 2004
    In:  Journal of Geophysical Research: Solid Earth Vol. 109, No. B2 ( 2004-02)
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 109, No. B2 ( 2004-02)
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2004
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Online-Ressource
    Online-Ressource
    American Geophysical Union (AGU) ; 1986
    In:  Journal of Geophysical Research: Solid Earth Vol. 91, No. B7 ( 1986-06-10), p. 7309-7325
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 91, No. B7 ( 1986-06-10), p. 7309-7325
    Kurzfassung: Differential attenuation (δ t *) measurements of teleseismic P and S waves are made in the frequency range 0.05–5.0 Hz across North America using broadband seismic data from the Department of Energy's Regional Seismic Test Network and Lawrence Livermore National Laboratory's Basin and Range network. Data from four events have been analyzed by first assuming frequency independent Q . The observed regional variations for (δ t *) are consistent with previous studies and show greater attenuation for stations in the Basin and Range relative to those in shield regions of North America. A significant component of apparent P attenuation appears at frequencies above about 0.5 Hz in both the Basin and Range and shield which reduces the t s */ t p * ratio to values possibly as low as 2. The second part of the analysis involved an extension to an absorption band attenuation model for both P and S waves. A linearized inversion for δ t *( f ) is then performed on the averaged spectral ratios for the Basin and Range and shield. Both S and P attenuation decrease with increasing frequency in both provinces, but the frequency dependence of Q s −1 is more pronounced. Attenuation is greater for the Basin and Range, and the data suggest enhanced S attenuation between about 0.2 and 1.4 Hz relative to the shield. The ratio of Q s −1 / Q p −1 ( Q p / Q s ) decreases from ∼2.0 at 0.05 Hz to less than 1.0 at frequencies greater than 1 Hz with similar effects in both provinces. Comparisons of our observations with different types of geophysical data lead us to conclude that dissipative mechanisms involving partial melt may be acting beneath the Basin and Range. The decrease in Q s −1 / Q p −1 at high frequencies is difficult to explain on both the Basin and Range and shield using intrinsic absorption mechanisms. The broadband data set used in this study appears to span the frequency band where intrinsic attenuation mechanisms evident at low frequencies are dominated by effects due to scattering at higher frequencies. If P and S waves interact with the same heterogeneities, the frequency where the attenuation due to scattering will be strongest is proportional to the inverse of the wavelength (i.e., where ka ∼ 1, where k is the wave number and a is the scale length of heterogeneity). Thus, in the presence of scattering, a decrease in the apparent S to P attenuation should be observed at higher frequencies, which is consistent with our observations.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1986
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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