and a bounded field excited at x=0 decays as e−γnx. It is an evanescent wave, rather than a freely propagating mode carrying net time-averaged energy flux down an indefinitely long uniform strip. A finite section can still transmit through coupling of evanescent fields.
State atime convention before using complex response: take fields proportional to ei(kz−ωt), with k=kr+iκ and κ≥0 for a passive wave entering the material. In a homogeneous Ohmic medium, Maxwell equations with J=σE give
A crest can move faster than c without carrying a new signal faster than light. Below cutoff the idealwave is evanescent, with penetration lengthc/ωp2−ω2; it does not propagate as an ordinary real-k bulk wave. Evanescence in the lossless limit is not Jouledissipation. Nonzero collision rate gives a dissipative conductivity and smooths this ideal cutoff picture.
For agood conductor with approximately real σ≫ωϵ, the spatial branch becomes
Below the waveguide cutoff frequencyωc=vk⊥, that mode is evanescent rather than freely propagating. TM modes require both indices positive; TE modes may have one zero but not both. For a>b, the lowest cutoff is the TE10 mode, with fc=v/(2a). A hollow single-conductor guide has no TEM mode, whereas a two-conductor transmission line can support one without this geometrical cutoff.[ref]
For a propagating TE or TM mode, vp=v/1−ωc2/ω2 and vg=v1−ωc2/ω2. The phase velocity can exceed v without superluminal information transfer. Frequency-dependent group delay can broaden pulses; excitation of several modes adds intermodal dispersion.
The requested power limit 0.01%=10−4 implies ∣Δb∣/b<0.02ln(b/a). Since ln(b/a)=2πnZ/Zvac=1.918 for the stated line, the adjacent cables' outer radii must match within approximately 3.84%. If a tolerance is quoted separately asa symmetric manufacturing range ±δb and arbitrary worst-case pairs can differ by 2δb, the corresponding individual tolerance is approximately ±1.92%. The leading calculation is for small mismatches; the exact logarithmic expression gives slightly asymmetric positive and negative limits. The vacuum wave impedance used here is approximately 376.73Ω.[ref]
Here vp is the propagation phase velocity in the cable, c/n for the stated nondispersive nonmagnetic filling. Squaring the amplitude gives the requested expression
For real r<0, write q=t2. The denominator of the powercoefficient is 1+q2−2qcosϕ. It has constructive peaks at ϕ=2πj and minima at ϕ=(2j+1)π, repeating with frequency spacing Δν=vp/(2L). Within this approximation,
Weak individual shunts thus give narrow interference peaks, with phase width of order ∣r∣.
The requested sum excludes paths that reflect repeatedly between different needles. It should not be read as an exact multiple-scattering result, particularly at the coherent peaks. For example the exact semi-infiniteamplitude satisfies
At ϕ=2πj this equation reduces to (R+1)2=0: the exact ideal infinite array has unit power reflection there, rather than the first-return approximation's value near 1/4. This does not change the requested geometric-series derivation, but identifies its physical limitation.
The corrected circulation of H is independent of that surfacechoice. Free conduction current stops at a plate; displacement current supplies the gap contribution.
The transmitted field is evanescent rather than a traveling bulk wave. A sufficiently thick collisionless plasma reflects such radiation without Ohmic absorption. Collisions make the response complex and permit absorption. This accounts for a plasma cutoff and, qualitatively, the reflection of some radio frequencies by ionized atmospheric layers. The simple model describes transverse waves; plasmas also support longitudinal collective modes.
The current J=σ0E is therefore concentrated within a few skin depths of the surface: this is the skin effect. Asfrequency increases within this regime, δ∝ω−1/2. In awire whose radius greatly exceeds δ, only a thin outer region carries appreciable alternating current, increasing the effective resistance. In a conducting shield, the same penetration suppresses the field transmitted through a sufficiently thick wall.
The wave impedance is Z=μω/k. For incidence from vacuum at normal incidence, the electric reflection amplitude is r=(Z−Z0)/(Z+Z0), where Z0=μ0/ϵ0. Agood conductor has small ∣Z∣ and therefore strong reflection, while the part of the incident power entering it is dissipated over the skin depth.
The edge condition gives cos(kya/2)=0, hence ky=(2j+1)π/a, j=0,1,…, for this even-in-y family. Opposite relative phase gives the sine family; together they yield all Dirichlet transverse modes ky=nπ/a, n≥1. For the equal-phase family,
It approaches c for λ→0 and diverges as λ→2a−; there is no real travelling-mode kz beyond the cutoff. This is an axial phase velocity, not the group velocity: vg=c1−(λ/2a)2<c. Here c denotes the membrane wave speed, not the speed of light.
For the evanescent membrane response below cutoff, below fc=c/(2a), put kz=−iκ for decay along positive z, with κ=(π/a)2−(ω/c)2. A localized central drive creates an evanescent, sinusoidally oscillating deformation decaying away in both axial directions. Far enough from the drive the leading profile is proportional to cos(πy/a)e−κ∣z−z0∣cos(ωt+ϕ0). Higher evanescent modes contribute near the point source. The pattern has no steadily advancing axial phase front or far-field propagating wave; decreasing frequency increases its spatial localization.
Here ρ has units kg/m, not the volume-density units used for a bulk fluid. The phase moves along the string at c, while a material point moves transversely with ψt=Aωsin(kx−ωt). Its maximum speed is Aω, which is not the phase velocity. Small slope Ak≪1 makes Aω≪c in this model.
The second expression follows from extra length1+ψx2dx−dx≃ψx2dx/2 against the pre-existing constant tension. Time averagingaharmonic wave gives ⟨EK⟩=ρA2ω2/4 and ⟨EU⟩=TA2k2/4=ρA2ω2/4. Therefore
The secondcurve is the first shifted right by π/(2k)=λ/4. More generally a point of fixed wave phase satisfies ωt−kx=constant, so it moves along x=(ω/k)t+constant. Hence the wavetravels in the positive x direction with
For the force derivation take a short segment between x and x+Δx. Let the tangentangles to the positive x axis be θL and θR. The left tension pulls along the negative tangent and the right tension along the positive tangent. With small slopes and approximately constant tension magnitude T, the horizontal components cancel to leading order and
For the pulse, define g(x)=Ae−ax2/2 with a>0. The given initial velocity is −cg′(x), exactly the velocity associated with a right-moving displacement g(x−ct). Therefore
Let θ1,θ2 be the incident and refracted ray angles from the interface normal. They also equal the corresponding acute angles between the wavefronts and the interface. The two right triangles have common hypotenuse AC, giving
This is Snell's law. In particular, entering a medium of larger refractive index reduces the ray'sangle to the normal. The construction assumes a stationary interface and homogeneous isotropic media with a propagating refracted wave.
Work with the explicitly corrected reduced-pressure system in b. Write d=1/(2H) and use the complex wave amplitude, taking real parts at the end. The vertical factor satisfies (∂z2−H−1∂z)w=−(m2+d2)w, so the wave equation gives
In particular u,w,b,Φ have amplitude proportional to ez/(2H), whereas pressurep′ has amplitude proportional to e−z/(2H). Directly substituting these expressions into vertical momentum gives Φz=−iω(m2+d2)w/k2=i(ω−N2/ω)w, verifying both the sign and the dispersion relation.
Meridional momentum is βyu+Φy=0. Since Φ=cu, it integrates to a Gaussianexp[−βy2/(2c)]. Thus
For short vertical wavelengths, m2≫k2+d2, so ω2≃N2k2/m2, c≃N/∣m∣ and LD2≃N/(β∣m∣). The wave is a slowly oscillating, hydrostatic internal gravity wave with strong vertical variation and relatively narrow trapping. Here u≃−(m/k)w and p′/ρ0≃−(ωm/k2)w; the buoyancy expression above remains valid.
For long vertical wavelengths, ∣m∣≪k2+d2, the exact limiting speed is c=N/k2+d2. To obtain the stated height-controlled limit also requires long horizontal wavelength, ∣k∣H≪1. With both ∣m∣H≪1 and ∣k∣H≪1,
Apply the intended, corrected dispersion relation in c. A uniform mean zonal wind gives ωground=ω+kU. Stationarity with U=−20ms−1 therefore requires eastward intrinsic phase speedω/k=−U=20ms−1. With k=1/a,
Astorm within roughly 12∘ of the equator has substantial projection on the Gaussian mode. There is no sharp latitude cutoff: ∣y∣=LD gives amplitude e−1/2 and the 1/eamplitude latitude is about 16.4∘. Forcing outside that core has progressively weaker overlap.
The intrinsic wave is eastward even though its observed ground pattern is stationary; westward advection cancels its phase propagation. Its intrinsic period is about 12.4Earthdays. The inferred ∣m∣≫1/(2H) puts it in the short-vertical-wavelength branch, well below the long-wavespeed 2NH=200ms−1. For upward energyradiation, ∂ω/∂m must be positive, which selects m<0 for positive k,ω: vertical phase propagation is then downward. Dust absorption supplies thermal forcing with a zonally asymmetric component; the response does not imply that dust itself moves eastward at the intrinsic phase speed.