📘 How snowflakes get their shapes
Learn how ice lattices, temperature, humidity, branching, riming, and aggregation shape snow.
What you’ll learn
- Crystal seed
- Hexagonal lattice
- Temperature
- Humidity
- Branches
- Plates and columns
- Riming
- Aggregation
- Melting
- Symmetry and variation
Questions this course answers
Why do ordinary snow crystals have six-fold symmetry?
The molecular arrangement of common atmospheric ice is hexagonal.
What generally supplies material for crystal growth?
Supersaturated vapor deposits onto the ice crystal.
What is riming?
Riming coats an ice particle when supercooled liquid droplets freeze on contact.
How do separate crystals become a snowflake?
Aggregation joins crystals through collisions aided by sticky or rimed surfaces.
What determines whether falling snow becomes rain?
Warm and cold layers control melting and refreezing during descent.
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