Viewing angle correction for slanted radar

Knowledge graph centered on Viewing angle correction for slanted radar with 42 nodes and 131 connections. Top connected: Gothic, Water Runoff, Multiscale Model to Model Cloud Compare method, Snow Water Equivalent (SWE), forecast skill.

Method synopsis

Statistical correction method to account for snow particle orientation effects when comparing slanted and vertical radar observations, derived from empirical offset analysis.

Synthesized from method descriptions across 1 paper using this protocol.

Procedure as described in the canonical source

Steps below were extracted from the paper that introduces this protocol — Riming-dependent snowfall rate and ice water content retrievals for W-band cloud radar (2025), Atmospheric Measurement Techniques. Implementations in other papers (listed below) may differ.

1. Apply viewing angle correction to radar data
   A viewing angle correction of 2.29 ± 0.39 dB was applied to correct slanted 40° radar observations to equivalent 90° vertical observations. This correction accounts for snow particle orientation effects, where falling ice and snow particles typically orient themselves horizontally in the atmosphere, resulting in lower radar reflectivity for slanted observations compared to vertical observations.
   Quantities: 2.29 dB offset correction, ±0.39 dB standard deviationDuration: Applied to all 40° observationsConditions: For comparison with vertical radar data from other sites
   Equipment: Statistical analysis of Ze distributions

Typical Equipment

• Statistical analysis of Ze distributions

Output Measurements

• corrected radar reflectivity

Papers Using This Protocol (1)

Places Where Used