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Native SVG diagrams

The book's science graphics, remade — native and interactive.

The book's science graphics, rebuilt as native SVG instead of raster images — and extended with new interactive ones: sharp on every screen, theme-aware, and not a single copyrighted image carried over.

01Kp index & auroral oval
Kp8_G4_Forecast.jpg
80°70°60°50°40°TromsøReykjavíkOsloEdinburghİstanbulNORTH POLE
Kp index & auroral oval
See how far the aurora
descends from the north.
3
Kp 0 – 9
Active
calmstorm
At this Kp level the aurora can be seen from:
Tromsø · Norway · 69.6°N● visible
Reykjavík · Iceland · 64.1°N● visible
Oslo · Norway · 59.9°N○ —
Edinburgh · Scotland · 55.95°N○ —
İstanbul · Türkiye · 41°N○ —

Drag the slider — the oval descends from north to south, and cities light up as it reaches them.

02Earth's magnetic shield
NASA_Magnetic_Field.jpg
Earth's magnetic shield
The solar wind leaks in through the poles.
SOLAR WIND →BOW SHOCKMAGNETOPAUSEMAGNETO·TAILPOLAR CUSPEarth

The atmosphere is an immense shield. Most of the charged particles from the Sun are deflected at the bow shock and flow around the magnetopause; only those that leak through the polar cusps reach the atmosphere and create the northern lights.

Solar-wind particles are animated; most are deflected, and those that leak through the polar cusp create the aurora.

03Aurora colours and altitude
NASA_Ionosphere_Infographic.jpg
0100200300400ALTITUDE · KMRed300400 kmGreen110300 kmPink90110 kmGROUND
Why different colours?
Colour is the work of
gas and altitude.
Green110300 km · Oxygen

The most commonly seen colour. It forms when charged particles collide with oxygen at low altitude (≈100–300 km).

Blue and violet — the human eye often struggles to make out these colours, produced by hydrogen and helium gases.
Hover over a colour band.

Hover over a colour band — which gas, which altitude.

04Watching points — by country
survey_data_3.png
81%10%10%21LOCATIONS
Watch points since 2013
Norway17 locations%81
Iceland2 locations%10
Sweden2 locations%10

Generated from the book's location data — not a static image, but live data.

05The 11-year solar cycle
NOAA_SWPC_solar_cycle.png
Does the Sun sleep?
Eleven years, minimum to maximum.
2008201220162020202420282031minmaxmaxnow
year
202688%
Solar maximum

The Sun's activity rises and falls on an ~11-year rhythm. Near maximum, sunspots and solar storms are frequent and the aurora reaches far south; near minimum, quiet nights can pass with nothing at all.

Drag the year — activity swings from quiet minimum to stormy maximum over ~11 years. We're near a maximum now.

06The night viewing window
twilight_diagram.png
The ideal time
Darkness is the other half.
DaylightCivilNauticalAstronomical dark16:0018:0020:0022:0000:0002:0004:0006:0008:00SunsetSolar midnightSunrise
Moon illumination · 0%
Dark window
18:4505:15
10.5 h

A clear, dark sky is half the battle. True (astronomical) darkness is the best window — but a bright moon lifts the sky's glow and eats into it. A new moon, or shooting before the moon rises, gives the deepest dark.

Drag the moon's brightness — a full moon washes out the sky and shrinks the truly-dark window.

07Anatomy of a substorm
aurora_substorm_phases.png
0~2–3 h
Anatomy of a substorm
Quiet, breakup, and recovery.

The arc suddenly brightens and erupts — rays shoot up, the curtain surges poleward and folds into swirls. The fast, dramatic part most people picture as 'the aurora.'

The aurora doesn't burn steadily — it pulses through a substorm cycle. Patience pays: a quiet arc can erupt into a breakup in seconds.

Step through the phases — a quiet arc loads, erupts at breakup, then fades through recovery.

Make it moveDrive the curtain with Kp and Bz.Open the simulator →Now test yourselfTen questions on the northern lights.Take the quiz →