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...

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Bibliographic Details
Main Authors: Péter Takács (563290), Dénes Száz (3943997), Ádám Pereszlényi (4575124), Gábor Horváth (3944000)
Format: Still Image
Language:unknown
Published: 2022
Subjects:
Online Access:https://doi.org/10.1371/journal.pone.0262762.g008
Description
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).