ライフサイエンスコーパス: surface wave

1 itting and conversion of propagation wave to surface wave.

2 so by generating longitudinal or transverse surface waves.

3 ation pattern created by the interference of surface waves.

4 interface where they waste energy generating surface waves.

5 ion ratios achievable within the distributed surface waves.

6 osity in the volcanic areas traversed by the surface waves.

7 d testing an ultrathin MetaSurface cloak for surface waves.

8 magnetopause, has long been known to support surface waves.

9 istics to conventional grating coupled Bloch surface waves.

10 red near the surface with an interference of surface waves.

11 cal ground displacements during the Rayleigh surface waves.

12 , which is estimated from 300- to 500-second surface waves.

13 water strider relies on momentum transfer by surface waves.

14 struction naturally arises in gravity (water surface) waves.

15 which small excitations such as sound(2) or surface waves(3,4) behave as fields propagating on a cur

16 ne-hertz GPS receivers also detected seismic surface waves 750 to 3800 kilometers from the epicenter,

17 cattering-immune propagation of a nontrivial surface wave across a three-dimension physical step.

18 sensitive measurements of the near-field of surface waves across the metasurface show the contrastin

19 The dispersion of Rayleigh surface waves across the ultrawide band allowed us to pr

20 of short-term seismicity within teleseismic surface waves also increased with peak dynamic strain.

21 Also surface wave amplitudes are used, to produce autospectru

22 ace can be efficiently manipulated using the surface-wave analogue of optical lattices.

23 and fidelity of crustal images obtained from surface-wave analyses.

24 we show direct observations of a plasmapause surface wave and its impacts during a geomagnetic storm

25 We illustrate the robust character of this surface wave and show its potential for control of sound

26 nt on both the momentum mismatch between the surface wave and the freely propagating modes as well as

27 Only surface waves and evanescence are observed outside this

28 rovides a versatile platform for controlling surface waves and exploring topological matter in higher

29 because of the combination of unusually long surface waves and seismic stations near the local earthq

30 This technique mitigates the surface waves and the substrate losses, thereby improvin

31 Here we jointly invert surface-wave and receiver function data to constrain cru

32 ft-handed inductors L(L), which suppress the surface-waves and reduce the substrates losses that lead

33 ries of experiments, emphasizing film flows, surface waves, and thermal convection.

34 In our model, these surface waves are driven by the travelling wave of elect

35 are encoded on the sample boundary), and the surface waves are Rayleigh waves.

36 In the second step, these backward surface waves are recycled and directed forward with the

37 the first millimeters to meters above ocean surface waves are shown.

38 mensional photonic crystals sustaining Bloch surface waves are tailored with a monoclonal antibody fo

39 Like waves on water, magnetopause surface waves are thought to travel in the direction of

40 ilometers), during times that high-amplitude surface waves arrive from the mainshock (less than 200 s

41 The generation of Bloch surface waves as a function of azimuthal angle has simil

42 The long-term changes of ocean surface waves associated with tropical cyclones (TCs) ar

43 be coupled into propagating electromagnetic surface waves at a metal-dielectric interface known as s

44 on characteristics of the two Dyakonov-Voigt surface waves at the planar interface are quite differen

45 teering, ultrasound lens design and acoustic surface wave-based applications.

46 retrieve empirical Green's function (EGF) of surface waves between stations.

47 nomenon, the onset and subsequent process of surface wave breaking are not fully understood.

48 ltilayer, it supports a guided mode, a Bloch surface wave (BSW) confined in one dimension.

49 (PSi) grating-coupled Bloch surface and sub-surface wave (BSW/BSSW) biosensor is demonstrated to siz

50 The top segment supports Bloch surface waves (BSWs) at the excitation wavelength and th

51 interact with both internal modes and Bloch surface waves (BSWs) of the 1DPC.

52 mbient noise was dominated by shoaling ocean surface waves but also contained observations of in situ

53 ping, by taking advantage of a stop-band for surface waves, but also selective mode conversion of sur

54 We demonstrate this phenomenon with elastic surface waves by strategically patterning an elastic sur

55 echnique for partitioning the propagation of surface waves by utilizing a T-shaped structure and path

56 the fluorophores thought to be lost by lossy surface waves can be recovered as emission by adjustment

57 Surface waves can lead to intriguing transport phenomena

58 revealed that as many as two Dyakonov-Voigt surface waves can propagate in each quadrant of the inte

59 demonstrate for the first time a dielectric surface wave cloak from engineered gradient index materi

60 The surface wave cloak is fabricated from a metallic backed

61 od agreement and performance as an effective surface wave cloak.

62 tion among multiple devices within a unified surface wave communication network.

63 We show that the surface wave component can mutually cancel the direct tr

64 ear the ocean surface, a tiny patch of arced surface waves confined to oppositely placed 70 degrees s

65 itats, its association with storms and ocean surface waves could in effect make it a useful cue for a

66 The conditions for Bloch surface wave coupling can be achieved by rotating both p

67 ition from Gaussian to anomalous behavior as surface waves cross an abrupt depth change (ADC).

68 tical models used previously in the study of surface wave damping by sea ice do not capture correctly

69 In addition, predictions from surface-wave-derived models are largely incompatible wit

70 The surface wave direction is switchable with the polarizati

71 cutaneous tissue stiffness through real-time surface wave dispersion analysis.

72 he proposed approach's efficacy in achieving surface wave division while minimizing interference.

73 We also show that the surface-wave-driven sawtooth auroras occurred in more th

74 been applied to fully control both space and surface waves due to their exceptional abilities to dyna

75 ciently transforms incident waves into spoof surface waves, effectively blocking sound while allowing

76 approach can be generalised to all kinds of surface waves, either for the coupling and discriminatio

77 Background Lung US surface wave elastography (SWE) can noninvasively quanti

78 Conclusion Lung US surface wave elastography may be adjunct to high-resolut

79 ent a novel optical structure design, termed surface-wave-enabled darkfield aperture (SWEDA), which c

80 z is interpreted as an Airy phase related to surface wave energy trapped in this local low-velocity c

81 xcitation, where energy is mostly carried by surface waves, energy reflection and redirection might l

82 The physics of capillary surface wave excitation is discussed and simulation is p

83 m to the phase matching conditions for Bloch surface wave excitation.

84 In the latter the surface wave fields are more confined within the structu

85 f an M = 6.9 quake remotely triggered by the surface waves from an M = 6.6 quake 4,800 kilometres awa

86 As surface waves from the 26 December 2004 earthquake in Su

87 We detected surface waves from two meteorite impacts on Mars.

88 The distortion of the shape of the surface wave fronts due to the curvature is corrected wi

89 guration explicitly designed to exploit this surface-wave geometry.

90 n California yields hundreds of short-period surface-wave group-speed measurements on interstation pa

91 Electromagnetic surface waves guided by the planar interface of an ortho

92 However, azimuthally generated Bloch surface waves have enhanced angular sensitivity compared

93 Structural variations revealed by surface waves hold implications for models of the format

94 n in forward scattering, but into near-field surface waves in reverse scattering.

95 Surface waves in topological states of quantum matter ex

96 re-emerged on the possibility to manipulate surface waves, in particular, towards the THz and optica

97 The reflection coefficient of a microwave surface wave incident at the termination of a metasurfac

98 To mitigate the surface-wave interactions and the substrate losses in th

99 f crystal momentum; we mode-convert Rayleigh surface waves into bulk waves that form tunable beams.

100 c material for which only one Dyakonov-Voigt surface wave is possible.

101 gths of MHA layer are unaffected whereas the surface wave is significantly increased, thereby paving

102 The polarity of the phase profile of the surface waves is found to be strongly correlated to the

103 The coexistence of two Dyakonov-Voigt surface waves marks a fundamental departure from the cor

104 interferometry and multichannel analysis of surface waves (MASW).

105 This paper analytically investigates the surface wave mode propagating along a planar Goubau line

106 displacements as arising from the driving of surface wave modes in which potential energy is stored i

107 Here we combine long-period surface-wave observations with simultaneous Global Posit

108 e of the SIW H-plane horn generates backward surface waves on both broad walls which increases the ba

109 We propagated surface waves on the lung through gentle mechanical exci

110 w water, downwelling light is refracted from surface waves onto the substrate creating bands of light

111 The surface-wave patch is a section of the sphere of radiati

112 ion at microwave frequencies of an analogous surface wave phenomenon whereby a metasurface supports a

113 Here, the ultrastrong coupling of a Bloch surface wave photon and molecular excitons in a disorder

114 spaced cylindrical cavities within a porous surface wave platform.

115 Surface waves play an important role in the exchange of

116 or charge transfer are satisfied using Bloch surface wave polaritons, which exhibit favourable disper

117 Surface waves process the turbulent disturbances which d

118 The interaction of ocean surface waves produces pressure fluctuations at the seaf

119 in long-periodic NCAI-SNSPDs grating-coupled surface waves promote EM-field transportation to the NbN

120 The two Dyakonov-Voigt surface waves propagate in different directions in each

121 be significantly enhanced through the use of surface waves propagating parallel to the metasurface ar

122 ssibility of using nanocomposites to control surface wave propagation through advanced additive manuf

123 direction perpendicular to the direction of surface wave propagation.

124 ffness or fibrosis by evaluating the rate of surface wave propagation.

125 The proposed technique suppresses the surface-wave propagation and reduces substrate loss ther

126 tiveness of using SIW technology to suppress surface wave propagations and near field mutual coupling

127 Our results show clear body and surface waves recorded at expected time and locations, a

128 Comparison of the measured surface-wave reflection spectra is made with that obtain

129 eoretical studies suggested that plasmapause surface waves related to the sharp inhomogeneity exist a

130 Interestingly, large transverse surface waves require a smaller additional noncollapse s

131 lies on detecting changes in the position of surface wave resonance during capillary condensation in

132 the wavepaths, but also introduce multiples, surface waves, scattering noise, and interference among

133 a realistic system for the amplification of surface-wave signals in future wireless communications.

134 Ghost polaritons are an atypical non-uniform surface wave solution of Maxwell's equations, arising at

135 ssical dynamic fracture theories predict the surface wave speed to be the limiting speed for propagat

136 he external chest wall and measured the lung surface wave speed with a US probe.

137 ely couple free-space beams into any type of surface wave, such as focused surface plasmon polaritons

138 The dispersion of an acoustic surface wave supported by a line of regularly spaced, op

139 e to E-field enhancement via grating-coupled surface waves synchronized with the NbN stripes in S-ori

140 In contrast, when surface wave systems are the focus, it has been shown th

141 This allows one to create a slower acoustic surface wave than can be achieved with the same uncovere

142 he crystal bulk, in contrast to conventional surface waves that are purely evanescent away from the i

143 his is compatible with shoreward-propagating surface waves that break in shallow water.

144 In addition to conventional Dyakonov surface waves, the analysis revealed that as many as two

145 displacements in Alaska and large-amplitude surface waves throughout western North America.

146 terize hybrid modes, which can be tuned from surface waves to bulk waveguide modes, traversing an exc

147 he immune nature of the topologically pumped surface waves to disorder and defects.

148 he function of this array may be to generate surface waves to power gliding.

149 was developed to assess the contribution of surface waves to the observed nighttime E. coli replenis

150 quifer is well isolated relative to previous surface wave tomography studies.

151 Here, using surface wave tomography, we establish the lateral extent

152 esults which monitor the transient change of surface wave travel time associated with high power lase

153 he ocean originates from the growth of ocean surface waves under the action of wind.

154 nset of illumination and further decrease in surface wave velocity associated with melting.

155 t with both showing a rapid reduction in the surface wave velocity at the onset of illumination and f

156 It is demonstrated that changes in the surface wave velocity can be used to track local heating

157 This dataset was processed to extract surface wave velocity information using ambient noise in

158 Here we report temporal changes of surface wave velocity over a large area associated with

159 Surface wave velocity, a nondestructive measure of tissu

160 rasound transducer for excitation of elastic surface waves was used to estimate phase speed and shear

161 steeper fault derived from seismic body and surface waves, we approximated free oscillation amplitud

162 iderations suggest that the so called "lossy surface waves" which quench fluorescence are due to indu

163 ng center using phase-delay times of seismic surface waves, which show anomalous polarization anisotr

164 rface plasmon polaritons are electromagnetic surface waves, which, due to their nanoscale nature, are

165 Anomalous launch of a surface wave with different handedness phase control is

166 face are quite different: the Dyakonov-Voigt surface wave with the higher relative phase speed is muc

167 sitive mode index, and another that supports surface waves with negative mode index.

168 arrow band of frequencies: one that supports surface waves with positive mode index, and another that

169 t-frequency impulsively-excited magnetopause surface waves, with standing structure along the terrest