list last updated Friday, 28 April 2006
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camouflage patterns |
created |
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[ ‘Bushland’ δ-series, Deep Taiga 4.1, bright ] |
2006-04-15 |
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[ ‘Bushland’ δ-series, Deep Taiga 4.1, dark ] |
2006-04-14 |
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[ ‘Bushland’ δ-series, Deep Taiga 4.1, subdued ] |
2006-04-15 |
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[ ‘Kurdaitcha’ β-series, Deep Taiga 4.1, bright ] |
2006-04-16 |
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[ ‘Kurdaitcha’ β-series, Deep Taiga 4.1, dark ] |
2006-04-16 |
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[ ‘Kurdaitcha’ β-series, Deep Taiga 4.1, subdued ] |
2006-04-16 |
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[ ‘Storm Front’ α-series, Taiga 6.1 ] |
2006-04-28 |
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[ ‘Taiga’ α-series, Taiga 4.1 ] |
2006-01-28 |
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[ ‘Taiga’ α-series, Taiga 4.2 ] |
2006-04-03 |
click images for more information
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Eleven per cent of the world's terrestrial surface can be classified as
taiga. This type of forest occurs in the Northern hemisphere, in a circumpolar band that runs though Canada, China, northern Japan, the Korean Peninsula, Mongolia, Russia and Scandinavia. To the north, taiga fades into
[ tundra ]. To the south, it gives way to grasslands, in the drier continental interiors, or to
[ taiga forest ], in maritime climates.
The climate of the taiga is characterised by long winters and short summers. Due to the high latitude, the daylight period is short in winter and average temperatures can be as low as −30°C (−22°F). The daylight period is correspondingly long in summer; however, average summer temperatures range from 6–14°C (43–57°F). Only about 50–100 days are free of frost. The taiga experiences low annual precipitation, which typically ranges between 350–500mm (14–20in.); much of this is in the form or snow. Strong winds cause high rates of evaporation and the wind chill factor is high.
Repeated freeze–thaw cycles often give rise to ground characterised by cracks, polygons, hummocks, knolls, frost boils and earth stripes, which result from the differential movement of soil, stones and rocks. The soil mantle in taiga regions is usually thin, deficient in nutrients, and acidic. It is also poorly-drained; as a result, the topsoil may become saturated with standing water during the summer thaw. Bogs and fens are common features.
Cold-tolerant evergreen conifers, such as fir, pine and spruce, dominate taiga forests. The leaves of these trees exhibit water-conserving characteristics, such reduced surface area and a thick, reflective cuticle. They are also dark in colour, so that they can absorb heat from sunlight and begin to photosynthesise when temperatures rise above 6°C (43°F).
Another adaptation, which helps trees in taiga regions to exploit fully the short growing season, is a high, dense canopy. As a result, very little sunlight penetrates to the ground and there is little understorey vegetation.
Almost all Roggenwolf digital camouflage patterns can be adapted for deployment in taiga forests. The most successful are those in which the macropattern is omnidirectional with a bias toward vertically-aligned elements, which further disrupt the geometry of the human shape at longer ranges by blending with the dominant pattern of shadows in wooded terrain. Strong contrasts may also be used, to simulate the perception of different layers in space.
Still, a well-devised macropattern can do only so much; the choice and arrangement of colours is also important. If the colours displayed in a camouflage pattern differ too much from the colours present in the immediate surroundings, the target shape can still be discerned and successful recognition shall occur.
Appropriate colours help a camouflage pattern to blend with its surroundings. In some cases, the colours displayed in Roggenwolf taiga forest digital camouflage patterns have been derived from computer-aided analyses of colour satellite photographs; the Deep Taiga 4.1 palette is illustrated on this page. Alternatively, more localised palettes may be created, to match specific tactical settings, through computer-aided analyses of ground-level photographs.
notice: All materials, including photos, camouflage patterns, simulations and text embodied within the pages of this Web site are the property of their respective copyright holders and may not be used elsewhere without explicit written permission from the copyright holder.
All original camouflage patterns and simulations shown on this Web site are copyright © 2005–2006
[ Brad Turner ]. All rights reserved.