Cloudiness distributions of Viking sailing routes.
Cloudiness distributions during simulated voyages using calcite sunstones at summer solstice with navigation periodicity Δ t = 1 hour for cloudiness dominances m dominance = -1, 0 or 1 (meaning dominantly weakly, medium or strongly cloudy skies) and for cloudiness changeabilities σ changeability = 1...
Main Authors: | , , , |
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Format: | Still Image |
Language: | unknown |
Published: |
2022
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Subjects: | |
Online Access: | https://doi.org/10.1371/journal.pone.0262762.g008 |
Summary: | Cloudiness distributions during simulated voyages using calcite sunstones at summer solstice with navigation periodicity Δ t = 1 hour for cloudiness dominances m dominance = -1, 0 or 1 (meaning dominantly weakly, medium or strongly cloudy skies) and for cloudiness changeabilities σ changeability = 1, 2 or 4 (meaning weakly/slowly, medium or strongly/rapidly changing cloudiness). |
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