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Finger rafting

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Finger rafting

Aerial photograph showing two thin ice sheets (made of nilas) that are moving toward each other. Along the length of the contact between the two sheets, segments where one sheet climbs onto the other alternate with others where it is the other way around. The lighter areas are where the ice thickness has doubled due to the overlapping process. This pattern is known as finger rafting. In many cases, it is highly systematic.
Three-dimensional representation of finger rafting, as it is often observed in the field. It occurs when two thin ice sheets converge toward each other.
Finger rafting derives its name from its resemblance to the interlocking of fingers.

Finger rafting develops in an ice cover as a result of a compression regime established within the plane of the ice. As two expanses of sea ice converge toward another, one of them slides smoothly on top of the other (it is overthrusted) along a given distance, resulting in a local increase in ice thickness. The term finger rafting refers to the systematic alternation of interlocking overthrusts and underthrusts involved in this process.[1][2][3] Such a pattern derives its name from its resemblance to the interlocking of fingers.[note 1]

The process

Rafting, also called telescoped ice,[3] is most noticeable when it involves new and young ice, but also occurs in ice of all thicknesses.[4] The process of finger rafting as such is commonly observed inside a lead, once a thin layer of ice (at the nilas stage) has formed. Although this ice is typically very weak (it is unable to support its own weight outside the water), it contains a lot of brine and is also relatively warm, since being that thin, its temperature is near that of the water. Rafting is accompanied with rapid draining of the brine inside the overlying ice sheet. This brine acts as a lubricant, significantly reducing the friction between the two sheets during overthrusting. Such a mechanism, and the fact that the upper surface of nilas is already slippery, account for overthrust distances in excess of 100 metres (330 ft) (a length-to-thickness ratio of 1000 to one).[4][note 2]

Rafting versus ridging

Rafting and ridging are two possible responses expected from the interaction between two converging ice sheets or floes.[4][5] The term ‘ridging’ refers to the process of ridge formation, involving the breaking up of the ice sheet into distinct blocks (which does not happen during rafting).[1][2][3] The reason why breaking happens is that, as the ice thickness increases, the bending moment exerted on the upper surface of the ice exceed its tensile strength.[5] In other words, the ice is no longer flexible enough to withstand the overthrust event without breaking.

Maximum thickness for rafting

A theoretical formula has been used to estimate the maximum thickness an ice sheet can have in order to be able to raft.[5] This thickness (h_{rf}) is

h_{rf}=\frac{14.2(1-\nu^2)}{\rho_wg}\frac{\sigma_t^2}{Y}

where \nu is Poisson's ratio, \sigma_t is the tensile strength of the ice, \rho_w is water density, Y is the Young's modulus of sea ice and g is the gravitational acceleration. What this equation shows is that, assuming a representative tensile strength of 0.65 MPa, the maximum thickness is in the range of 0.2 metres (7.9 in).[5]

See also

Notes

  1. ^ Whereby the first finger in one hand overlies the same finger in the other hand, the second finger in one hand underlies the second finger in the other hand, the third fingers do as the first fingers, etc.
  2. ^ According to this source, finger rafting is also possible in lakes and rivers even though this ice is non saline, but only if it is very thin, i.e. less than 2 centimetres (0.79 in).

References

  1. ^ a b Wmo Sea-Ice Nomenclature • Terminology
  2. ^ a b Environment Canada - Weather and Meteorology - Ice Glossary
  3. ^ a b c All About Sea Ice, Introduction :: National Snow and Ice Data Center
  4. ^ a b c Weeks, W. F. (2010) On sea ice (Chap. 12). University of Alaska Press, Fairbanks, 664 p.
  5. ^ a b c d Leppäranta, M. (2005). The Drift of Sea Ice. Springer-Verlag, New York, 266 p.
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