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Doppler weather radar observing a structured storm while a satellite and subtle model contours appear above
WEATHER FIELD GUIDE · EVIDENCE TYPES

Radar, Satellite and Forecast Models Are Not the Same

Learn what each weather layer actually represents, why their timestamps differ and how forecasters combine observations with numerical guidance.

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What the data really means

Use these four anchors before interpreting the related live visualization.

Radar
Remote observation near the instrument
Satellite
Remote observation from orbit
Model
Numerical estimate of atmospheric evolution
Official warning
Authority-issued decision product
EVIDENCE FLOW

From evidence to the PlanetVexa view

Each stage changes what can be claimed. PlanetVexa keeps the source record, derived interpretation and visual presentation visibly distinct.

  1. 01Radar

    Remote observation near the instrument

  2. 02Satellite

    Remote observation from orbit

  3. 03Model

    Numerical estimate of atmospheric evolution

  4. 04Official warning

    Authority-issued decision product

01

Radar samples energy returned to the instrument

Weather radar sends pulses and measures energy scattered back by precipitation and other targets. Reflectivity can indicate where hydrometeors are present and how strong the returned signal is; Doppler velocity estimates motion toward or away from the radar. Neither field is a direct photograph of rainfall at the ground. Beam height, distance, blockage, attenuation and non-weather echoes all matter.

A radar timestamp is the observation time of a scan or composite. Animation shows successive observations; it is not automatically a forecast.

02

Satellites observe radiation from above

Weather satellites measure reflected sunlight and emitted infrared or microwave radiation. Visible imagery reveals cloud texture during daylight. Infrared channels estimate radiative temperature and work day and night, while water-vapor and microwave products expose different atmospheric layers or properties. A bright or cold cloud top is not by itself a measured surface rain total.

Satellites provide broad coverage over oceans and remote regions where surface instruments and radars are sparse. Products may be direct radiance measurements or algorithms derived from several channels, so the product label matters.

03

Models calculate a possible future atmosphere

Numerical weather prediction starts from an analyzed atmospheric state built from many observations. Equations describing fluid motion, thermodynamics and physical processes are solved on a three-dimensional grid. Output has a model initialization time and one or more valid times. Those are different from the observation time shown on radar or satellite imagery.

Models have finite resolution and approximate processes smaller than their grid. Comparing multiple runs and ensembles helps reveal uncertainty; agreement does not turn guidance into an observation.

04

Warnings add expert and institutional judgment

An official watch, warning or advisory is not another sensor layer. It is an authority-issued product based on evidence, forecasts, thresholds and local responsibility. PlanetVexa keeps those products labeled as official-only rather than inferring warnings from colorful imagery or model values.

FREQUENTLY ASKED QUESTIONS

Questions people ask

Is radar a rainfall forecast?

No. A radar scan is an observation; extrapolation or model guidance is needed to estimate future conditions.

Does satellite imagery show rain reaching the ground?

Not necessarily. Satellite channels observe radiation and cloud properties, and derived precipitation products retain algorithmic uncertainty.

Why do model runs disagree?

They can start from different analyses, resolutions and physics, and small initial differences can grow over time.

PRIMARY REFERENCES

Read the official material

PlanetVexa summarizes these sources in original language and links to the responsible institutions for definitions and operational context.

  1. NOAA/NWS: Computer model data
  2. National Weather Service education
  3. NOAA/NWS upper-air observations