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Record #209562:

Antarctic sea ice drift shown to cause sea ice cover increase / Anon.

Title: Antarctic sea ice drift shown to cause sea ice cover increase / Anon.
Date: 2012.
In: Sea Technology. (2012.), Vol. 53(12) (2012)
Abstract: Brief report of first direct evidence that changes to Antarctic sea ice drift caused by changing winds are responsible for increases in sea ice cover in past two decades, which helps to explain why Antarctic sea ice cover has increased under effects of climate change.
Notes:

Sea Technology. Vol. 53(12) :74 (2012).

Keywords: 551.326 -- Floating ice.
551.326.1 -- Floating ice, distribution and movement.
551.326.13 -- Floating ice, distribution, secular change.
551.55 -- Wind and air turbulence.
551.588 -- Climate, effect of man and environment.
551.588.5 -- Climate, relationship with ice.
E6 -- Glaciology: floating ice.
(*7) -- Antarctic regions.
(*80) -- Southern Ocean.
SPRI record no.: 209562

MARCXML

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245 10 ‡aAntarctic sea ice drift shown to cause sea ice cover increase /‡cAnon.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2012.
300 ## ‡ap. 74.
500 ## ‡aSea Technology. Vol. 53(12) :74 (2012).
520 3# ‡aBrief report of first direct evidence that changes to Antarctic sea ice drift caused by changing winds are responsible for increases in sea ice cover in past two decades, which helps to explain why Antarctic sea ice cover has increased under effects of climate change.
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.1 -- Floating ice, distribution and movement.‡2udc
650 07 ‡a551.326.13 -- Floating ice, distribution, secular change.‡2udc
650 07 ‡a551.55 -- Wind and air turbulence.‡2udc
650 07 ‡a551.588 -- Climate, effect of man and environment.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
773 0# ‡7nnas ‡tSea Technology. ‡gVol. 53(12) (2012) ‡wSPRI-109554
916 ## ‡a2014/06/20 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220930 ‡bHS