01Low liquid layer
INTERACTIVE CLOUD RF LAB
Change the atmosphere.
Watch the channel respond.
Build up to four liquid-cloud layers and inspect how height, thickness, water content, temperature, motion, geometry, and carrier frequency change the selected satellite-to-ground path.LINK GEOMETRY
Experiment inputs
MULTILAYER COLUMN
Cloud slabs
02Mid mixed layer
03Upper mixed layer
MODELED OBSERVABLE
Pair response
EXCESS PATH0.000 mm
SLANT MODELED LIQUID WATER1.392 kg/m²
GAS / RAIN-- / 1.142 dB
WAVELENGTH14.99 mm
SEPARATED FORWARD TERMS
Contribution by modeled layer
- Slant path
- 2.199 km
- Attenuation
- 0.2256 dB
- Excess path
- 0.0000 mm
- Phase
- OFF
- Wind projection
- +9.00 m/s
- Residual Doppler
- OFF
- Slant path
- 2.795 km
- Attenuation
- 0.1762 dB
- Excess path
- 0.0000 mm
- Phase
- OFF
- Wind projection
- +17.22 m/s
- Residual Doppler
- OFF
- Slant path
- 1.994 km
- Attenuation
- 0.0684 dB
- Excess path
- 0.0000 mm
- Phase
- OFF
- Wind projection
- +25.39 m/s
- Residual Doppler
- OFF
ACTIVE FORWARD EQUATIONS
γcloud,k = Kl(f,Tk) · MkAcloud = Σk γcloud,k · LkΔφk = −2π ΔLk / λfD,k = −(f/c) · d(ΔLk)/dtLayer terms are separable because their states are supplied to the forward model. A measured total does not uniquely recover them unless the multi-ray/multi-frequency Jacobian has sufficient rank.