Titan U glossary

Radar Attenuation

Radar attenuation is the weakening of a radar signal as some of its energy is absorbed or scattered on the way out to a target and back, so returned echoes are dimmer than a clean, hazard-free path would produce.

Radar attenuation is the weakening of a radar signal as some of its energy is absorbed or scattered on the way out to a target and back, so returned echoes are dimmer than a clean, hazard-free path would produce. It is a fractional reduction in power per unit path length, usually described in decibels per kilometer.

How energy is lost

Two physical processes drive attenuation. Absorption removes energy as it interacts with water molecules and other atmospheric constituents. Scattering redirects energy in other directions, so some of the outgoing pulse never reaches the target of interest, and some of the returning echo never makes it home.

The amount of loss grows with the density and size of the hydrometeors in the beam path. A distant storm hidden behind a nearer heavy core is being sampled through a lot of extra water, and every meter of that path takes another small bite out of the signal.

Why wavelength changes the story

Attenuation is strongly wavelength-dependent. Shorter-wavelength radars, like C-band systems commonly used on some television and research platforms, attenuate more heavily in rain than longer-wavelength radars. The S-band WSR-88D near 10 centimeters attenuates much less, which is one of the reasons it was chosen for the national operational network.

Even S-band can be attenuated by intense rain and by melting hail, and dual-polarization variables such as specific differential phase are used to estimate and correct for that loss in modern processing.

How forecasters compensate

The classic tell is a storm that looks weaker on the far side of a heavy rain core than physics would suggest, sometimes ending in a 'V' notch of quiet behind the core. Forecasters cross-check with a neighboring radar that sees the same downstream storm through a cleaner path, and lean on satellite and lightning trends to keep intensity honest.

Dual-pol products help too. When correlation coefficient stays high through a suspect volume, the softer reflectivity is more likely to reflect a real environmental change; when it dips and specific differential phase surges upstream, attenuation is a good candidate for the dimmer picture downstream.

Keep going

How Radar Attenuation connects

Builds on 1

  • Radar Beam

    Attenuation is the radar beam losing energy to absorption and scattering on its trip out and back, so the beam itself is the starting point.

Part of 1

  • Radar Artifact

    Attenuation belongs with radar artifacts because it is a propagation effect that dims echoes, not a real change in the storm being sampled.

Contrasts with 2

  • Beam Broadening

    Both can make a distant storm look weaker, but attenuation is energy lost through heavy rain on the way, while beam broadening is averaging inside a bigger sample volume.

  • Reflectivity Gradient

    Attenuation behind a heavy core can create or exaggerate an edge that looks like a real reflectivity gradient but is not.

Measured by 1

  • Specific Differential Phase

    Specific differential phase is one of the dual-polarization variables modern processing uses to estimate and correct for attenuation, even on S-band radar.

More related terms