Century. Although It Was Recognized As a Probable Continent More Than

978978GEOPHYSICS: P. A. SIPLE PROP. N. A. S. Forces such as radiation pressure or simple convection appear to be incapable of ejecting the material. The only one I have discovered capable of performing the required action is the magnetohydrodynamic force associated with a current loop. One can show that such forces are entirely adequate to account for the elevation of prominence material against the force of gravity. At the same time these cur- rents can produce and maintain the observed filamentation of spots. Further, it appears that the energy stored in the current system is of the order of that released during a solar flare. Thus, even though we still cannot define an M region un- ambiguously, we have achieved some understanding of the force fields that may occur in the solar atmosphere and which may have some effect on the ionosphere. * The research reported on was made possible in part through support and sponsorship ex- tended by the Geophysics Research Division of the Air Force Cambridge Research Center, under Contract AF 19(604)-146 with Harvard University. It is published for technical information only and does not necessarily represent recommendations or conclusions of the sponsoring agency. 1 G. P. Kuiper (ed.), The Sun (Chicago: University of Chicago Press, 1953); G. Abetti, II Sole; D. H. Menzel, Our Sun (Cambridge, Mass.: Harvard University Press, 1949). 2 Helen W. Dodson in Kuiper, op. cit. 3Ibid.; J. L. Pawsey and S. F. Smerd, in Kuiper, op. cit. 4D. H. Menzel, Elementary Manual of Radio Propagation. 5 J. A. Simpson, in Kuiper, op. cit. 6 S. Chapman and J. Bartels, Geomagnetism (2 vols.; Oxford, 1940); D. H. Menzel, Our Sun. 7E. 0. Hulbert, Phys. Rev., 34, 344, 1929; 36, 1560, 1930. 8 S. Chapman and J. Bartels, op. cit. 9 M. Waldmeier, Z. Astrophys., 18, 241, 1939; 21, 275, 1942. 10 A. Shapley and W. 0. Roberts, Astrophys. J., 103, 257, 1946. 11 J. W. Lincoln and A. Shapley, T'rans. Am. Geophys. Union, 29, 849, 1946; A. Shapley, Terrestrial Magnetism and Atm., Elec., 51, 257, 1946; Trans. Am. Geophys. Union, 28, 715, 1947. 12 B. Bell and H. Glazer (unpublished). 13 W. 0. Roberts, Astrophys. J., 101, 136, 1945. 14 S. Chapman and V. C. A. Ferraro, Terrestrial Magnetism and Atm. Elec., 43, 77, 1938. Cf. also Chapman and Bartels, op. cit. GEOGRAPHIC BASIS FOR ANTARCTIC SCIENTIFIC OBSERVATIONS BY PAUL A. SIPLE DEPARTMENT OF THE ARMY, RESEARCH AND DEVELOPMENT DIVISION Antarctica has emerged from total terra incognita since the beginning of this century. Although it was recognized as a probable continent more than one hundred years ago, the contiguous coastal outline was not completed as a reliable sketch until the past decade. The state of current antarctic geographic knowledge might well be likened to that of the Americas in the sixteenth century. The task of classical exploration has virtually ended, and the period of detailed scientific study has already begun. With the exception of large sections of the interior, approximating the area of the United States, the major features have been sketched in (see Fig. 1). In contrast to sixteenth-century exploration tech- niques, those of the twentieth -century, together with scientific interest, have produced small sampling of intensive studies in Antarctica comparable in quality Downloaded by guest on September 30, 2021 VOL. 40, 1954 GEOPHYSICS: P. A. SIPLE 979 to scientific investigations in densely populated regions of the world. In some cases, such as certain aspects of oceanography, the detailed knowledge of the waters surrounding Antarctica is currently superior to that of some ocean areas more temperate and accessible. Thus Antarctica is a strange mixture of the unknown and the well known. Outside of the subantarctic whaling industry, commercial interests are nonexist- ent, and the most valuable resource of Antarctica is that pertaining to scientific knowledge. Therefore, in the proposed program of the International Geophysical Year, where phenomena affecting the earth as a whole are being studied simulta- neously, it is not surprising to find that the planners for each subject area desire to make observations from Antarctica concurrently with observations in the arctic regions, the tropics, and the mid-latitudes. The specific interest in Antarctica is based on several factors. 1. Antarctica lies as an insular continent in a vast expanse of surrounding oceans. To neglect observations from this region would effectively remove simultaneous observations from approximately one-tenth of the world's surface, neces- sitating interpolations for distances ranging between 4,000 and 6,000 miles. This is particularly significant to the circummeridional studies of meteorology and upper atmospheric research. 2. The intensity of the electromagnetic phenomena, such as those related to geomagnetism, aurora and airglow, cosmic rays, ionospheric physics, and solar activity, are directly or indirectly influenced by the earth's magnetic and geomagnetic poles. Evidence is inconclusive that the observed responses are similar at both poles, and it is scientifically desirable to make simultaneous observations for com- parative and analytic reasons and to check theories based on unipolar evidence. 3. The massive, isolated glacial covering of the antarctic continent undoubtedly provides invaluable clues to the recent past as well as current changes in world climate. We are apparently already sensing the significance of the warming trend which began about 1900 and which probably accounts for such problems as the in- creasing drought of our southwestern states and the corollary rise, iI water level of the Great Lakes. 4. The North Pole and much of the area involved in the polar geophysical phenomena lie in oceanic areas fraught with ice conditions limiting easy establish- ment of observing points at pertinent intervals. In addition, full scientific co- operation is lacking in the circumpolar effort because of international circumstances making ideal observation patterns deficient in the North. By contrast, the antarctic provides a circumpolar land surface which is fully available to scientific studies. As the only totally glaciated continent, Antarctica also provides an unequaled opportunity to study active continental glaciation, which has at various times in the past played an important role in the geologic history of many parts of the earth. Particularly, it permits the biologists to study the persistence and return of life during and after glaciation. Antarctica still largely holds the riddles to geologic interpolation between the southern limits of South America, Africa, Australia, and New Zealand. Geologic sampling shows the usual broad differences which char- acterize continents with dissimilar areas of fossiliferous sediments, vulcanism, and ancient metomorphics. Antarctica is the highest continent with an average alti- Downloaded by guest on September 30, 2021 980 GEOPHYSICS: P. A. SIPLE PRoc. N. A. S. tude of a. mile above sea level. The South Pole is on a great snow plateau nearly two miles high, and numerous mountain peaks rise to about three miles in height. Of particular interest is the great faulted Queen Maud Range, approaching within about two hundred miles of the South Pole, exhibiting open seams of Permian coal. ANTARCTIC STATIONS 0 Proposed U.S. 0 Some Existing Geophysical Stotions of Other Countries ANTARCTICA\ iER AII\ F- At ........:.!' A K . Iti-RLT;>F ..;\ v!.\ \ji\i. ; 4 FIG. 1 For the first time, during the International Geophysical Year, it will be possible to check not only the polar simultaneity of electromagnetic phenomena but also the circumpolar correlation. A series of antarctic stations is essential to achieve Downloaded by guest on September 30, 2021 Voi.. 40, 1954 GEOPHYSICS: P. A. SIPLE 981 both goals. Australia has already manned its new station, Mawson, on the antarctic coast at latitude 67036'21' S., longitude 62°52'48" E., directly under the belt of greatest auroral activities. It is also continuing its established island geophysical stations, including Miacquarie Island not far from the maximum auroral zone. France is considering reopening its Adelie Land Station, which is not far from the magnetic pole and is well inside the auroral zone belt. A proposed French icecap station might actually place a station closer to the geomagnetic pole than has been achieved to date. In addition to its subantarctic stations, New Zealand has been reported to be planning an antarctic station near Cape Adair, also inside the auroral zone and not far from the magnetic pole. The United States plans call for a main base camp at Little America, close to and just inside the auroral belt, with a subbase near latitude 800 S. and longitude 1200 W., nearly under the auroral belt. A second United States subbase has been under consideration at the South Pole itself, although logistic difficulties may render this impractical. Other IGY stations in the Palmer Peninsula region, south of South America, under the sponsorship of co-operating nations include ones to be manned by the United Kingdom, Chile, and Argentina. They form a vital link to the North and South American meridional observing stations leading to the North Pole, important to the meteorological research as well as the electromagnetic programs. In addition to the proposed IGY Antarctica geophysical studies, announcements have been made of geographical exploration plans for two independently sponsored Antarctic explorers. Rear Admiral Richard E. Byrd, USN (Ret.), the dean of American polar exploration, has announced his intention to renew his exploration of the antarctic. This would be his seventh command of major American polar ex- peditions over the last quarter-century. Two of the five carried out in the antarctic were government-sponsored. Admiral Byrd's plans were announced six months prior to the IGY antarctic plans. His expedition is primarily concerned with the geographical exploration of the unknown interior, although he will, as usual, provide an opportunity for scientists to take advantage of his visit to the antarctic.

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