NEPHELESENSING SYSTEMS
Open twin

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.
Open cloud equations

LINK GEOMETRY

Experiment inputs

MULTILAYER COLUMN

Cloud slabs

01Low liquid layer
02Mid mixed layer
03Upper mixed layer

MODELED OBSERVABLE

Pair response

FAST PATH · 20.0 GHz
MODELED LIQUID LOSS0.470dB · ice contribution unavailable
EXPERIMENTAL PHASEOFFdefault governance
CLOUD DOPPLEROFFdepends on phase model
RECEIVED POWER--withheld · incomplete path budget
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

Low liquid layer0.902.00 km
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
Mid mixed layer3.204.60 km
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
Upper mixed layer5.806.80 km
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 EQUATIONSγcloud,k = Kl(f,Tk) · MkAcloud = Σk γcloud,k · LkΔφk = −2π ΔLk / λfD,k = −(f/c) · d(ΔLk)/dt

Layer 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.