派博傳思國際中心

標(biāo)題: Titlebook: Ocean Seismo-Acoustics; Low-Frequency Underw Tuncay Akal,Jonathan M. Berkson Book 1986 Springer Science+Business Media New York 1986 Arctic [打印本頁]

作者: Intimidate    時間: 2025-3-21 16:07
書目名稱Ocean Seismo-Acoustics影響因子(影響力)




書目名稱Ocean Seismo-Acoustics影響因子(影響力)學(xué)科排名




書目名稱Ocean Seismo-Acoustics網(wǎng)絡(luò)公開度




書目名稱Ocean Seismo-Acoustics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Ocean Seismo-Acoustics被引頻次




書目名稱Ocean Seismo-Acoustics被引頻次學(xué)科排名




書目名稱Ocean Seismo-Acoustics年度引用




書目名稱Ocean Seismo-Acoustics年度引用學(xué)科排名




書目名稱Ocean Seismo-Acoustics讀者反饋




書目名稱Ocean Seismo-Acoustics讀者反饋學(xué)科排名





作者: accessory    時間: 2025-3-21 23:01

作者: Ophthalmologist    時間: 2025-3-22 02:18
A Green’s Function Method for One-Way Wave Propagation in a Range-Dependent Ocean Environmentronment. However, there has been no exact theory for applying the Green’s function approach to one-way wave propagation in a range-dependent environment. This paper derives a generalized Green’s function method for exactly solving the one-way wave equation in an environment that varies discretely in
作者: peptic-ulcer    時間: 2025-3-22 06:03

作者: THROB    時間: 2025-3-22 08:42
An Acoustic Reflectivity Method for Laterally Varying Layered Medial layers. The equations of motion are Fourier transformed with respect to time and Fourier-Bessel transformed with respect to the horizontal coordinates. Then one computes the exact response of the layer stack using Haskell. matrices, or Kennett. iteration, or the global matrix method of Schmidt. an
作者: 慌張    時間: 2025-3-22 13:48
A Vector Parabolic Equation Model for Elastic Propagation published model, based on a Born approximation for scattering from an inhomogeneous layer, enables parabolic equation (PE) computations in elastic media with different longitudinal and shear speeds. This method of derivation is shown to reduce to the normal PE for the scalar case. The elastic PE mo
作者: Condyle    時間: 2025-3-22 17:07

作者: intricacy    時間: 2025-3-22 23:00

作者: Hemiplegia    時間: 2025-3-23 04:51
Development of a Parabolic Approximation for the Computation of Propagation Loss in a Range-Dependenolution for a quadratic development of the propagation operator which allows us to take into account a larger angular aperture of the source. The numerical solution is given by an algorithm of finite differences using the Crank-Nicholson method. The problem of rectilinear, horizontal and oblique int
作者: 配置    時間: 2025-3-23 06:11
Linear and Nonlinear Ocean Acoustic Propagation Modelsfluid dynamics a nonlinear time domain wave equation is then derived. A unidirectional approximation leads to a nonlinear time domain version of the parabolic equation, a nonlinear progressive wave equation (NPE), which can treat propagation of finite amplitude signals in a refracting medium in a wa
作者: 跳脫衣舞的人    時間: 2025-3-23 12:08

作者: 鋸齒狀    時間: 2025-3-23 13:52

作者: 排他    時間: 2025-3-23 20:39

作者: 清洗    時間: 2025-3-23 23:53

作者: Phagocytes    時間: 2025-3-24 02:51

作者: BOON    時間: 2025-3-24 07:10

作者: inventory    時間: 2025-3-24 13:49
Predicted Partitioning of VLF Acoustic Energy in a Range-Dependent Environmentpport of the Cape Fear VLF Exercise to be conducted during June 1985. Because the first several hundred meters of subbottom in this area consist of sediments that can only weakly support shear, the effect of shear in the subbottom will be primarily to increase transmission loss. This increased trans
作者: Irrepressible    時間: 2025-3-24 18:17

作者: 持久    時間: 2025-3-24 20:38

作者: 背心    時間: 2025-3-25 00:14

作者: 跑過    時間: 2025-3-25 07:20

作者: JIBE    時間: 2025-3-25 07:46

作者: 嚙齒動物    時間: 2025-3-25 13:38
Homer P. Bucker,Michael B. Porterlle ist dort begrenzt, wo es notwendig ist, diese Stoffe rein zu erschmelzen. Auch Graphit als Tiegelmaterial ist dann nicht zu verwenden, wenn eine Kohlenstoffaufnahme des zu schmelzenden Materials unerwünscht ist. Wenn es gelingt, entweder ohne Tiegel oder in gekühlten Tiegeln und Kokillen zu schm
作者: jettison    時間: 2025-3-25 19:34

作者: Organization    時間: 2025-3-25 22:20

作者: Mercantile    時間: 2025-3-26 03:39

作者: 填滿    時間: 2025-3-26 07:42

作者: Kaleidoscope    時間: 2025-3-26 08:28
nders, giving us the first capability of producing both global and local maps of the seafloor. Subsequently, better instrumentation and techniques led to a clearer, more quantitative picture of the seabed itself, which stimulated new hypotheses such as seafloor spreading through the availability of
作者: Costume    時間: 2025-3-26 13:57
Book 1986ing us the first capability of producing both global and local maps of the seafloor. Subsequently, better instrumentation and techniques led to a clearer, more quantitative picture of the seabed itself, which stimulated new hypotheses such as seafloor spreading through the availability of more relia
作者: invulnerable    時間: 2025-3-26 19:20

作者: GLUE    時間: 2025-3-26 22:00
Predicted Partitioning of VLF Acoustic Energy in a Range-Dependent Environment the effective subbottom parameters are discussed. The numerical results presented include the transmission loss as a function of depth and range and the relative fraction of acoustic energy that is bottom-interacting.
作者: OGLE    時間: 2025-3-27 02:39
A Green’s Function Method for One-Way Wave Propagation in a Range-Dependent Ocean Environment term. On a given range step, the source distribution is the acoustic field at the end of the previous step. It is shown numerically that the method gives an accurate solution for one-way propagation.
作者: Fierce    時間: 2025-3-27 05:57

作者: Arboreal    時間: 2025-3-27 09:41

作者: Largess    時間: 2025-3-27 13:48
Shear Wave Effects on Propagation to a Receiver in the Substrateical and horizontal displacements are found to increase significantly when shear wave processes are included. An analysis of the range dependence of displacement suggests that shear wave propagation is the major acoustical mechanism producing this increase.
作者: jeopardize    時間: 2025-3-27 21:03

作者: llibretto    時間: 2025-3-27 22:50
D. R. DelBalzo,J. E. Matthews,J. V. Soileau,C. Feuillade
作者: 可觸知    時間: 2025-3-28 04:35
teigt also die Wahrscheinlichkeit für einen st?rungsfreien Betrieb und eine hohe Lebenserwartung verzinkter Installationsrohre. Einschr?nkend ist hier jedoch auf die stark ungleichm??ige Anfangskorrosion bei pH-Werten um 7,9 hinzuweisen, da nicht auszuschlie?en ist, da? sich diese Effekte bei noch h
作者: GILD    時間: 2025-3-28 07:30
L. Neil Frazer,John J. McCoyErgebnisse befriedigend zu erkl?ren. Insbesondere bedeutet die nicht vorhandene oder nur sehr geringe Abh?ngigkeit der Korrosionsgeschwindigkeit vom Sauerstoffgehalt, da? der Transportwiderstand der Deckschicht proportional den Sauerstoffkonzentrationen sein mü?te. Keine der an den Deck- schichten v
作者: Thrombolysis    時間: 2025-3-28 14:29

作者: 變異    時間: 2025-3-28 18:21
J. Miller,A. Nagl,H. überallelbarer Erw?rmung wird die W?rmeenergie von au?en an das Schmelzgut herangebracht und geht durch W?rmeleitung, Konvektion, W?rmestrahlung oder elektromagnetische Strahlung auf das Gut über. Die unmittelbare Erw?rmung dagegen l??t die W?rme im Gut selbst entstehen. Auch Grenzf?lle zwischen unmittelba
作者: Accede    時間: 2025-3-28 19:05

作者: chronicle    時間: 2025-3-29 00:20
Homer P. Bucker,Michael B. Porterelbarer Erw?rmung wird die W?rmeenergie von au?en an das Schmelzgut herangebracht und geht durch W?rmeleitung, Konvektion, W?rmestrahlung oder elektromagnetische Strahlung auf das Gut über. Die unmittelbare Erw?rmung dagegen l??t die W?rme im Gut selbst entstehen. Auch Grenzf?lle zwischen unmittelba
作者: Criteria    時間: 2025-3-29 04:00

作者: MIR    時間: 2025-3-29 07:48
Bottom Interaction Effects on Normal Modes: an Algebraic Approach
作者: 鉆孔    時間: 2025-3-29 12:17

作者: 有花    時間: 2025-3-29 15:59
Intrinsic Modes in a Wedge-Shaped Ocean with Stratified Elastic Bottomlanted interface. The model is now generalized to allow for stratification of the slanted bottom along planes parallel to the water-bottom interface, and for elastic properties in these layers. Examined in detail is the special case where the bottom is an elastic half space. Upslope propagation in t
作者: LEVER    時間: 2025-3-29 22:35
An Acoustic Reflectivity Method for Laterally Varying Layered Mediabed as a stack of plane parallel layers; however, within each layer the velocity, density, and quality factor, Q, are now functions of horizontal position x. These functions are all independent from layer to layer so any earth or sea-bed model can be parameterized in this way. The two foundations of
作者: Lumbar-Spine    時間: 2025-3-30 00:36

作者: 最高峰    時間: 2025-3-30 06:32
Gaussian Beams and 3-D Bottom Interacting Acoustic Systemsy differential equation along the central ray. This latter method has recently received a lot of attention in the seismological community. Both methods are free of the difficulties at caustics and in shadow zones which afflict standard ray tracing algorithms. Comparisons are presented between the st
作者: Offbeat    時間: 2025-3-30 08:40
A Study of Propagation Loss Dependence on Sediment Layer Thickness Using the Fast Field Programhe intermediate layer is lossy produces an increasing loss with increasing layer thickness by straightforward absorption. This paper uses the Fast Field Program (FFP) to investigate these effects parametrically in a three layer simulation. It is shown that dependence of loss on layer thickness may t
作者: Infirm    時間: 2025-3-30 15:37

作者: 刪除    時間: 2025-3-30 18:28
Experimental Confirmation of Horizontal Refraction of Sound Propagation in a Wedge-Like Oceanls which showed significant bearing shifts due to repeated reflections from the ocean surface and bottom. The obliqueness of the azimuthal launch angle with respect to the shore line prevented the local grazing angle from becoming large enough to produce much bottom loss which is in accord with pred
作者: Innovative    時間: 2025-3-30 22:40
Acoustic Propagation over Large-Scale Linear Ocean Slopes generic class (passive margin) was chosen for detailed acoustic propagation calculations. The passive-margin slope is common in the North Atlantic, has a vertical angle of 2.8°, and is covered by 500 m of silt. Using a summer Sargasso Sea sound speed profile, numerous calculations of transmission l
作者: 擦掉    時間: 2025-3-31 03:01

作者: Relinquish    時間: 2025-3-31 08:08
re of the seafloor is still far from complete. Underwater acoustics concerns itself today with the phenomena of propagation and noise at frequencies and ranges that require an understanding of acoustic interaction at both of its boundaries, the sea surface and seafloor, over depths ranging from tens to thousa978-1-4612-9293-7978-1-4613-2201-6
作者: 神刊    時間: 2025-3-31 11:24
9樓
作者: 意見一致    時間: 2025-3-31 15:04
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作者: 必死    時間: 2025-3-31 17:50
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作者: 不整齊    時間: 2025-4-1 00:10
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作者: 議程    時間: 2025-4-1 01:50
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作者: 印第安人    時間: 2025-4-1 06:52
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