By (International Geophysical Year)
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Published via the yankee Geophysical Union as a part of the Geophysical Monograph Series.
As plans for our nationwide participation within the co-ordinated geophysical exploration of Antarctica via 11 international locations constructed, it turned more and more obvious that we must always assemble to be had medical wisdom of the Continent for heritage reasons in reading the most important medical difficulties watching for us.
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Extra info for Antarctica in the International Geophysical Year: Based on a Symposium on the Antarctic
O •'-. • -85 -75 -65 -55 -45 -35 .... -;•5 -15 -5 ,c Fi•. 1- Meanandindividual wintertime temperature soundings, illustratingthe phenomenon of a 'disappearing' tropopause Copyright American Geophysical Union Antarctica in the International Geophysical Year Geophysical Monograph Series 38 WEXLEK Km Vol. 1 AND RUBIN onecanconceive of one,orperhaps tworelatively permanent deep,coldstratospheric lowsoverthose regionsof Antarcticaduring the winter season. 5øS 1o• • January 1941 ,o _ • o• M:Maudheim-71'S x ol -- January 1951,1952 • o• AB: ArcticBQy-73'N.
Confirmationof this predictionwould accumulationand wastageat as many pointsas bean excitingand valuable discovery. possibleto provide a better estimateof Antarctic Fabric studies should also contribute to an underglacier regime. Principal interest focuseson the standingof the constitutionand origin of the Ross inlandice,of course,but studieson smalloutlying Ice Shelf by providing one of the best means of bodiescanbe significantasthey aremoresensitive, identifyingthe varioustypesof ice composingthe easierhandled,and may be responding alreadyto body.
From submarine topography and glaciomarine Seismic explorations by Poulter  have sediments [Ross,1937,pp. 577-578]. already definedmany of the geometricrelationsof The objectiveshouldbe to establisha sequence the RossIce Shelf, and further seismic,gravity, of eventsin relative order, and then, more im- andgeodeticmeasurements duringIGY will extend portantly,to date them in an absolutechronology. Data will be obtainedonthickness, Carbon •4offersthe best hopefor this, and efforts areaswhere the shelfis aground,depth of undershouldbe made to find, collect,and establishthe lying water, and possiblythe thicknessof unconpropergeologicalrelation of organicmaterialsof solidateddepositson the seabottom.
Antarctica in the International Geophysical Year: Based on a Symposium on the Antarctic by (International Geophysical Year)