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Module 4 of 6 · 7 min

How forecasting works

Three instruments, in order of warning time: coronagraphs that see the launch days out, a physics model that turns launch speed into an arrival, and the L1 monitor that turns the last hour from a forecast into a measurement.

One CMEThe main Gannon CME, mid-transit. Selected wedge, arrival drawn at Earth.
The bright wedge is the selected CME. Its arrival estimate moves when you change the wind below.
1

The idea

A fast CME plows into the slower solar wind ahead of it and decelerates, like a boat pushing through water. Feed the model a launch speed, a direction and the wind it must push through, and physics gives an arrival time. The catch is that the wind changes daily and a head-on CME's speed is hard to measure. That is where the error bars come from.

2

Turn the dial

Same CME, same launch. Change only the wind it must push through and watch the arrival move.

Estimated arrival
Transit time
Speed at Earth
Shift vs typical wind

Check yourself · Module 4

1. The L1 monitoring spacecraft give roughly how much certain warning?
L1 sits about 1.5 million km upstream. When a shock sweeps past it, arrival at Earth is measured, not modeled: half an hour to an hour out.
2. Why is a storm's strength so much harder to predict than its arrival time?
Arrival is physics on speed and distance. Strength hinges on whether the CME's field points south, invisible until the last hour.
3. Our published arrival accuracy is honestly about…
Twelve hours at the median, about fifteen on average, validated against hundreds of real arrivals. Imperfect inputs, honest physics.
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