4.0 Antarctica
Past and Present

Antarctica history is rich in adventure and science, yet human activity in the region extends back in time only about 200 years. In fact, most of what is known about Antarctica has been discovered in the present century.

4.1 Early Antarctic Activity

4.1.1 Exploration

Remote, inaccessible, and inhospitable, Antarctica was the last continent to be discovered, and knowledge of the south polar region was accumulated slowly. Until the present century the interior of Antarctica was unknown, and even the continental margins had been seen in only a few places. Of the world's 61,000 nonfiction papers and books published about the Antarctic since the earliest papers dating from the 1600s, 91 percent have been published since 1951. However, the historian Kenneth J. Bertrand (Americans in Antarctica 1775-1948, American Geographical Society, 1971) writes that "the success of recent operations in unveiling Antarctica with the aid of modern technology does not negate the importance of earlier efforts. Present accomplishments have been built on the past, developed step by step since 1674, sometimes haltingly and sometimes failing."

Explorations have been conducted for a variety of motives and sometimes accidentally, as was the case of the first discovery south of the Antarctic Convergence (where temperate and polar waters meet) of South Georgia in the 1670s when a commercial ship was blown off course. The true nature of the Antarctic as a frigid region of ice and snow was convincingly proved for the first time by the second voyage of the English navigator, Captain James Cook, between 1772 and 1775 (Exhibit 9). Until then, there was general belief in a large, still undiscovered continent in the southern hemisphere suitable for European settlement. Cook circumnavigated Antarctica, much of his course south of 60°S, and crossed the Antarctic Circle in three places. He failed to sight any part of the Antarctic continent, but disproved conclusively the existence of the mythical continent "Terra Australis Incognita" at latitudes north of 60°S. Mariners who followed Cook into high southern latitudes were attracted to the harsh environment by his reports of great numbers of whales and seals, particularly the latter.

Map of explorers' routes

Exhibit 9

Cook's voyage. Between 1772 and 1820 explorers neared but did not discover the Antarctic continent. Of greatest significance were the three expeditions of Captain James Cook, Great Britain, who in 1772-1775 established that a continent must exist south of his southernmost penetrations. "That there may be a Continent or large tract of land near the Pole, I will not deny," he wrote on 5 February 1775. "On the contrary I am of the opinion there is, and it is probable that we have seen a part of it. The excessive cold, the many islands and vast floats of ice all tend to prove that there must be land to the South." Shown are the cruise tracks of (1) Cook; (2) Captain William Smith, Great Britain, 1819; (5) Captain Thaddeus Bellingshausen, Russia, 1820; and (11) Captains James Weddell and Matthew Brisbane, Great Britain, 1823. Source: Antarctic Map Folio Series, 1975.


In 1820-1821 the American sealer Nathaniel B. Palmer of Stonington, Connecticut, saw the Antarctic Peninsula from his sloop Hero and met the Russian Captain Thaddeus Bellingshausen commanding the two ships Vostok and Mirnyy on a major national expedition that circumnavigated Antarctica eastward. Three other great national expeditions were made between 1819 and 1843 by the French Admiral Dumont d'Urville, who discovered the Adélie and Clarie coasts in 1840; by U.S. Navy Lieutenant Charles Wilkes, who mapped 1,500 miles of Antarctica's coast south of Australia in 1839-1840, proving Antarctica a continent; and by Britain's Sir James Clark Ross, who discovered the Ross Sea, Ross Island, and the Ross Ice Shelf in 1841.

Historians have not settled the question of who was first to see land in Antarctica. British, Russian, and U.S. ships all were in the Antarctic Peninsula area in the early 1820s, and the first sighting occurred during that time. The first documented landing on the continent was on 24 January 1895, when the Norwegian whaling ship Antarctic landed a party at Cape Adare on the northern Ross Sea. The party consisted of Captain Leonard Kristensen, second mate Carstens Borchgrevinck, and H. J. Bull, who wrote a book about their adventure. Bull called being first on the Antarctic mainland "both strange and pleasurable," although he thought the crew would have preferred to find a Right Whale "even of small dimensions."

In 1895 a resolution by the Sixth International Geographical Congress in London promoted Antarctic exploration and set into motion a series of expeditions known now as the "Heroic Era." Before World War I halted this activity, 16 exploring expeditions from Australia, Belgium, England, France, Germany, Japan, Norway, Scotland and Sweden (but not the U.S.) had visited Antarctica. This activity is exclusive of whalers, discussed below. The magnitude of this activity was unprecedented for Antarctica, and, considering the state of technology and size of the world's population and wealth, it probably was greater than that of the mechanical age that followed and comparable to the operations initiated with the International Geophysical Year (IGY), 1957-1958. The best known of the Heroic Age expeditions were those led by Roald Amundsen (Norway) and Robert F. Scott (England), who separately reached the geographic South Pole (and were the first to do so) a few weeks apart on 14 December 1911 and 17 January 1912, respectively (Exhibit 10).

Photo: Attainment of the South Pole

Exhibit 10

Attainment of the South Pole. Roald Amundsen's and Robert Scott's teams' arrivals at the South Pole in December 1911 and January 1912 concluded humankind's quest for the highest southern latitude, which had begun centuries earlier with the voyages of Drake, Cook, and others. Personal and national prestige motivated both Amundsen whose tent and flag stand here and Scott, whose party this is. "Thus we plant thee, beloved flag, at the South Pole," Amundsen said, "and give to the plain on which it lies the name of King Haakon VII's Plateau." Scott and his party, arriving second, were bitterly disappointed to miss "the reward of priority." They died on the return trek to the coast, having carried 31 pounds of geological specimens to the very end. The photograph shows, left to right, Evans, Wilson, Oates and Scott.


U.S. Antarctic activity in this century began with Richard E. Byrd's hugely popular, privately financed, expeditions in 1928-1930 and 1933-1935. Byrd's success led to Congressional appropriations of $10,000 in 1939 and $340,000 in 1940 (totaling about $4.1M in 1997 dollars) for the U.S. Antarctic Service, organized as a civilian entity under four cabinet agencies. Intended to be permanent but curtailed to a single winter and two summers because of World War II, the field work in 1939-1941 nevertheless was the largest Antarctic expedition up to that time, and it produced discoveries in a number of research disciplines.

After the War the U.S. Navy Antarctic Developments Project (Operation Highjump) in 1946-1947 was then (and remains) by far the largest Antarctic expedition, with more than 4,700 naval and marine personnel, 44 observers, 13 ships, and a number of aircraft. The expedition sighted more than 1.5-million square miles of Antarctica, half of it previously unexplored, and took 15,000 aerial trimetrogon (mapping) photographs. The following season the U.S. Navy Second Antarctic Developments Project (Operation Windmill) used ship-based helicopters to get geodetic ground control for the Highjump photographs. The expedition contributed to production of the first medium-scale maps of the region and influenced decisions regarding locations of stations for the International Geophysical Year the following decade. At a time when other nations had embarked on programs of permanent bases, the U.S. Navy Second Antarctic Developments Project also was a vehicle for continuing the U.S. presence in Antarctica.

4.1.2 Sealing, Whaling, and Fishing

British sealers first crossed the Antarctic Convergence in 1778, and Americans in about 1792. Profits were enormous. Around 1797 the Neptune of New Haven, a ship worth perhaps $3,000, gathered 45,000 skins at the Falklands and Juan Fernandez, sold them for $90,000 in Canton, bought Chinese goods there and sold them for $260,000 in New York. As subantarctic seals were decimated the sealers pushed farther south. In 1820-1821, at least 30 American, 24 British, and 1 Australian vessels were hunting seals in the South Shetlands. The next year the numbers were perhaps doubled. Landings were said to have been made on the Antarctic Peninsula, the South Orkney Islands were discovered, and at least one and maybe three Americans traveled as far south as 66°S on the west side of the Antarctic Peninsula. James Weddell (British) discovered the Weddell Sea. Fur seals and then elephant seals (for their oil) were reduced almost to extinction by the mid-1800s, at which point the sealers for all practical purposes abandoned this activity. In 1978 the Antarctic Treaty nations agreed to prohibit the taking of fur, elephant and Ross seals, and to limit the annual catch of various other species. No seal hunting has taken place in the Antarctic since 1964 and the populations of fur and elephant seals have significantly regenerated themselves in the last half of the 20th century.

Whaling began in Antarctic waters in the 19th century. The industry enlarged greatly in the early 1900s, when steamships, harpoon guns, and shore processing stations (notably at South Georgia) were introduced. During the 1912-1913 season 10,760 whales were caught. After that time nearly all the whales caught in the world were taken in Antarctic waters. In 1931, the peak year, 40,199 whales were caught in the Antarctic, while 1,124 were caught in the rest of the world. The whaling industry declined after 1960. In the 1980-1981 season fewer than 6,000 whales were caught in the Antarctic; all were Minke whales, a relatively small-sized species. In 1994 the member nations of the International Whaling Commission declared Antarctic waters a whale sanctuary in which no commercial whaling is allowed (Exhibit 11).

Photo: ultraviolet radiation monitor

Exhibit 11

The biggest environmental impact? In whaling's record year, 1931, that deliberate human action in the Antarctic managed to remove about two million tons of living whale biomass from the marine ecosystem. It is an ironic measure of humans' global reach that this amount is estimated to have been exceeded threefold by that resulting from the existence of the ozone hole, which was caused unintentionally by natural atmospheric transport of industrial chemicals to the Antarctic stratosphere. Because of the ozone hole, enough additional ultraviolet radiation from the Sun reaches the ocean surface to reduce the productivity of marine microorganisms in Antarctic waters by an amount estimated by experimental work to be seven million tons of carbon fixation annually. Here, an instrument that monitors the amount of ultraviolet radiation reaching the surface is operated at Palmer Station.


Commercial fishing was begun by the Soviet Union in 1967, and in 1971 a Soviet fleet of 40 trawlers and support ships in the southern ocean landed an estimated 300,000 tons mostly cod, herring, and whiting. In 1995-1996 ten nations landed 115,188 tons, of which 91 percent was krill and the rest finfish. Japan was the principal participant with more than half the catch; the other substantial fishers were Poland and Ukraine. This catch continued modest annual increases since 1993, but well below those taken during the years up through 1990-1991, when the Soviet Union disbanded its long-distance fleet.

Two American firms have engaged in crabbing in recent years, but the unfavorable economics of this activity have resulted in both companies abandoning their efforts.

The Antarctic fishery, a tiny fraction of the world's total annual catch of about 80 million tons, is regulated by the Antarctic Treaty's 1982 Convention for the Conservation of Antarctic Marine Living Resources.

4.1.3 Mineral Resources

The issue of exploitation of mineral resources in Antarctica is addressed in Article 7 of the Protocol on Environmental Protection to the Antarctic Treaty: "Any activity relating to mineral resources, other than scientific research, shall be prohibited." U.S. Public Law 104-227, the "Antarctic Science, Tourism, and Conservation Act of 1996," implements the provisions of the Protocol. President Clinton signed it into law on October 2, 1996. The Protocol will enter into force when all nations that signed it in 1991 deposit their instruments of ratification. There is no assurance that some nations will not challenge the agreement in the event of a major discovery of mineral reserves in Antarctica.

Based on current knowledge of the continent's geological setting, the chance that valuable mineral deposits exist in Antarctica appears reasonably high. Prior to approximately 200 million years ago, Antarctica was the centerpiece of a large Southern Hemisphere supercontinent, Gondwana, that included what is today South America, Africa, Madagascar, peninsular India, Antarctica, Australia, and New Zealand (Exhibit 12). The wide distribution of mineral resources across these other Gondwanan continents, including base metals and precious stones, implies that similar deposits probably exist in Antarctica. But with rare exception, the areas that are most likely to contain mineral deposits are covered by the ice sheet. The occurrence of major hydrocarbon deposits in Antarctica is uncertain because deep drilling has not been conducted on the continental shelf; however, the geological evolution of the Antarctic continental margin has resulted in the development of large sedimentary basins with known source rocks for hydrocarbons and likely reservoirs to store these hydrocarbons. Given the prevailing conditions, it is improbable that chance discoveries of mineral deposits will be made in Antarctica. Rather, exploration for mineral deposits would require a dedicated, costly program, including in many cases the development of new technologies.

Map: Gondwanaland vs. present

Exhibit 12

The pivotal position of Antarctica in the ancient supercontinent Gondwanaland can be seen in these illustrations. The supercontinent began to rift and break up 180 million years ago.


In his book Cold: The Record of an Antarctic Sledge Journey, Dr. Laurence M. Gould states that he "had rather go back to Antarctica and find a fossil marsupial than three gold mines." It is unrealistic to think that this philosophy will always prevail, especially if the global demand for mineral resources continues to escalate. Scientific research will undoubtedly lead to better assessment of Antarctica's resources and to better technology for exploiting these resources. To date, the U.S. has played a key oversight role in evaluating geological and geophysical research in Antarctica and in encouraging the exchange of geophysi cal and geological data, all while precluding the commercial exploitation of Antarctica.

4.1.4 Territorial Claims

Seven nations have asserted claims to pie-shaped sectors of Antarctica bounded by longitudinal lines: Great Britain (claim made formally in 1926), New Zealand (1923), Australia (1936), Norway (1939), Chile (1940), Argentina (no formal date), and France (1924). The initial claims were based on discovery, adjacency, or decree, and all but one of the claims extend from north of the coast to the South Pole. Three claims overlap. One sector is unclaimed. The claims occasionally have led to conflict; on 2 February 1952 the Argentine navy fired on the British when they tried to land at Hope Bay. Conflicts over other remote areas have not been unknown, including the U.K./Argentina war over the Falklands as recently as 1982. Other nations have acted to make claims, but not asserted them; for example, Germany sent an expedition for this purpose in 1938, and in 1939 Lincoln Ellsworth, heading his second Antarctic expedition (the first was a transantarctic flight in 1935), dropped from his plane a brass cylinder containing a note claiming territories for the U.S. "so far as this act allows."

Other than the claimant states, most nations do not recognize Antarctic claims. U.S. non-recognition, a cornerstone of the nation's Antarctic policy, dates to 1924, when Secretary of State Charles Evans Hughes wrote that discovery of lands unknown to civilization "does not support a valid claim of sovereignty unless the discovery is followed by an actual settlement of the discovered country." In 1934 the Assistant Secretary of State added: "I reserve all rights which the U.S. or its citizens may have with respect to this matter." President Franklin D. Roosevelt reaffirmed the U.S. stance in 1939: "The U.S. has never recognized any claims of sovereignty over territory in the Antarctic regions asserted by any foreign state." In 1947 Dean Acheson, then Under Secretary of State, wrote that the U.S. "has not recognized any claims of any other nations in the area and has reserved all rights which it may have in the area."

Despite the Antarctic Treaty provision that "no acts or activities taking place while the present Treaty is in force shall constitute a basis for asserting, supporting, or denying a claim to territorial sovereignty in Antarctica," some signatories have taken what appear to be assertive steps. For example, both Argentina and Chile publish their claimed Antarctic sectors on their official national maps, and both have established hotels and post offices. Chile has placed whole families in residence at its Antarctic stations, with schools, banks, and other evidence of "effective occupation," including the birth of a child. An Argentinian child was born at Argentina's Esperanza Station in the late 1970s.

4.1.5 International Geophysical Year

The IGY, 1 July 1957 to 31 December 1958, was a cooperative endeavor by scientists throughout the world to improve their understanding of the Earth and its environment. Much of the field activity took place in Antarctica, where 12 nations established some 60 research stations. Laurence M. Gould, who was Richard E. Byrd's chief scientist in Antarctica in the 1920s and 1930s and later chaired the National Academy of Sciences Polar Research Board and served on the National Science Board, called the IGY the most comprehensive scientific program ever undertaken and the first attempt at a total study of the environment. "No field of geophysics," he wrote in 1958, "can be understood or complete without specific data available only from this vast continent and its surrounding oceans."

The U.S. established six Antarctic IGY research stations: Little America (on the Ross Ice Shelf), Hallett (in Victoria Land), South Pole and Byrd (in Marie Byrd Land), plus Wilkes (on the coast of Wilkes Land, East Antarctica) and Ellsworth (on the Filchner Ice Shelf). Naval Air Facility, McMurdo Sound (now McMurdo Station), was set up as a logistics base from which to supply South Pole. Studies were directed toward geophysics and upper atmospheric physics and complemented simultaneous observations around the globe. Long traverses were made to collect data in glaciology, seismology, gravimetry, and meteorology. Geological and biological samples were also collected, although these disciplines were not formally part of the IGY (Exhibit 13).

Map: Antarctic Research Stations

Exhibit 13

Year-round stations serve as research and data collection centers and as support depots for temporary summer camps, traverses, and airborne data collection. In 1995, a typical recent year, 17 nations operated 37 year-round stations. During the intensive 18-month International Geophysical Year (1957-1958), 12 nations operated about 60 year-round stations in Antarctica. Most stations receive their personnel and supplies by ship. Only Marambio (Argentina), Frei (Chile), Rothera (U. K.), McMurdo (U. S.), and Mirnyy (Russia) can land wheeled airplanes. Most Antarctic stations have been established on the coast. Only Russia and the United States have operated year-round stations in the interior over the long term. Russia has closed all but three stations since the breakup of the former Soviet Union.


4.1.6 Antarctic Treaty

International cooperation in the IGY stimulated the Antarctic Treaty, signed by the 12 Antarctic IGY nations at Washington, D.C., in 1959 and entered into force in 1961. The treaty establishes a legal framework for the area south of 60°S, which includes all of Antarctica. There are two types of Antarctic Treaty parties. Consultative nations, now 26 in number (Exhibit 14), are empowered to meet periodically and to influence operation of the treaty. Acceding nations, of which there now are 17, agree to abide by the treaty, but, not being among the original signatories and not having substantial programs in Antarctica, do not participate in the consultative process.

Graph: Number of Antarctic Treaty Nations

Exhibit 14

Number of Antarctic Treaty nations, 1959-1997. Of the 43 nations that have signed the Antarctic Treaty, 26 are consultative (voting) nations because either they are original 1959 signatories or they perform substantial scientific research in the Antarctic. The 17 acceding nations participate in the annual Antarctic Treaty consultative meetings as observers. The treaty nations represent two-thirds of the world's human population and four-fifths of its economic output.

The 12 nations that performed Antarctic field research during the 1957-1958 International Geophysical Year signed the treaty at Washington, D. C., in December 1959. The treaty entered into force in June 1961 after these nations had deposited their instruments of ratification with the U. S. Department of State.

The 1964 Agreed Measures for the Conservation of Antarctic Fauna and Flora was particularly significant; it is only one of approximately 160 recommendations affecting management of Antarctica that have been adopted over the period covered by this graph. Another significant addition was CCAMLR, the Convention on the Conservation of Antarctic Marine Living Resources, which regulates the Antarctic fishery. CRAMRA, the Convention on the Regulation of Antarctic Mineral Resource Activities, did not achieve ratification; it was replaced by the Protocol on Environmental Protection, signed in 1991, which prohibits mining and strengthens environmental protection generally. As of early 1997, the Protocol appeared likely to achieve ratification by all 26 signing nations, after which it will enter into force.


The treaty provides that Antarctica shall be used for peaceful purposes only; it prohibits military operations except in support of peaceful activities. It provides that freedom of scientific investigation and cooperation shall continue and that nations shall exchange program plans, personnel, observations, and results. The treaty seeks to resolve the issue of territorial claims by simply not recognizing, disputing, or establishing claims; and it prohibits assertion of new claims. It prohibits nuclear explosions and disposal of radioactive waste. It guarantees access by any treaty nation to inspect others' stations and equipment. Appendix VI further summarizes the treaty.

The consultative meetings provided for by the treaty have generated a series of recommendations, most of which have been formally adopted by the treaty nations, that provide rules for operating on and around the continent. One of the most significant is the Agreed Measures for the Conservation of Antarctic Fauna and Flora, ratified by the U.S. as Public Law 95-541, the Antarctic Conservation Act of 1978. Other advances have included the Convention for the Conservation of Antarctic Seals and the Convention on the Conservation of Antarctic Marine Living Resources. A failed recommendation of significance is the 1988 Convention on the Regulation of Antarctic Mineral Resource Activities, which would have permitted mining if the proponent were to demonstrate that the environment would not be damaged. Instead, a 1991 Antarctic Treaty meeting adopted a protocol for improved environmental protection that prohibits mining; the U.S. signed this protocol into law (PL104-227) in October 1996 and is preparing to deposit its instrument of ratification with the Antarctic Treaty system. The U.S. and other Antarctic Treaty nations are complying with the protocol on a voluntary basis pending its entry into force, which will occur only after all 26 of the nations initially signing the 1991 agreement ratify it.

4.1.7 National Programs

Twenty-eight nations are now conducting Antarctic research programs. The activities range from summer-only seaborne expeditions that focus on particular science questions to year-round operations that span the research disciplines relevant to the Antarctic. In 1995 there were 37 year-round stations in operation: Argentina 6, Australia 3, Brazil 1, Chile 3, China 2, France 1, Germany 1, India 1, Japan 2, South Korea 1, New Zealand 1, Poland 1, Russia 5, South Africa 1, United Kingdom 4, United States 3, and Uruguay 1. Many of these nations, and other nations, operated additional summer stations and camps for research field work that is feasible only in summer.

4.2 Current U.S. Antarctic Program

Each year the USAP deploys approximately 3,500 scientists and support personnel to Antarctica and its surrounding seas to support basic research in many disciplines, including aeronomy and astrophysics, atmospheric chemistry, biology, Earth sciences, ocean and climate systems, glaciology, and environmental science. Although a far smaller effort, Antarctica also offers a promising environment for the conduct of certain types of applied research and technology development. In FY95 and FY96, U.S. researchers came from institutions in 26 states and the District of Columbia.

The budget for the (NSF) U.S. Antarctic Program is $193.5M in FY97. Of this amount $30.5M consists of grants to scientists at research institutions, $41.0M is spent on direct field support of these research projects, and the balance of $122.0M is spent on logistics and operations that provide the infrastructure enabling the U.S. presence and science. These figures reflect the high costs of working in so remote a location. Additionally, in FY97, a separate NSF account is funding a $25M emergency safety and environmental upgrade at South Pole Station.

The history of spending for the USAP is shown in Exhibit 15. Exhibit 16 presents research and operations costs assignable to each U.S. location in Antarctica. Exhibit 17 categorizes the research funding according to function.

Graph: U. S. Antarctic Program funding

Exhibit 15

U.S. Antarctic Program funding, 1955-1997. In 1955 the U.S. began preparing for the International Geophysical Year, which took place officially from 1 July 1957 to 31 December 1958. After the IGY, the decision was made to support a continuing, or post-IGY, research program; some facilities were closed, and others were added. Budget volatility in the years 1957-1962 reflects this transition.

Fluctuations in the period 1973-1977 are caused by LC-130 procurement and budget-base transfer of costs from DOD, a continuing multi-year result of DOD's action to quantify and transfer Antarctic costs pursuant to the 1970 decision to consolidate funding for the U. S. Antarctic Program at the National Science Foundation. Part of the rise in the 1980s is attributable to completion of this process; for example, the NSF began paying the Antarctic-attributable share of military retirement costs in 1985.

The years 1990-1994 contain a five-year $85M safety, environment and health initiative. The 1993 spike contains $49M for LC-130 procurement.

This graph includes DOD, USCG, and NSF Antarctic spending for all the years shown. The graph does not include research spending by other agencies; in FY96, other agency research accounted for about three percent of the U. S. Government's total funding of Antarctic research and research support. Years shown are fiscal years.

Graph: USAP fiscal year 1995 funding

Exhibit 16

USAP FY95 funding (totaling $196M) by facility. Most of this money is spent in the U.S. for acquisitions, salaries, equipment, planning, and follow-up research at home institutions. All science-grants funds are assigned to Antarctic locations even if the research was done entirely at home institutions. The $35.5M in "off-continent costs" is for contractor and military headquarters operations in the United States and for staging facilities in Christchurch, New Zealand, and Punta Arenas, Chile.

Graph: USAP fiscal year 1995 science grants

Exhibit 17

USAP FY 95 science grants to research institutions (totaling $29M) by discipline. These amounts do not include operational support in the Antarctic.

The NSF funds and manages the following major facilities as an integrated system for the support of research and related activities in Antarctica:

4.2.1 McMurdo Station, the principal U.S. facility, on Ross Island, coast of Antarctica (peak summer population capacity 1,258; 1996 winter, 232)

The largest Antarctic station, McMurdo (Exhibit 18) is built on the bare volcanic rock of Hut Point Peninsula on Ross Island, the most southerly solid ground that is accessible by ship. It is located just 20 miles south of Mt. Erebus, an active volcano that steams continually and erupts frequently though not violently.

Photo: McMurdo Station

Exhibit 18

McMurdo Station. McMurdo, Antarctica's largest station, has airports and a seaport, research laboratories and support facilities. The light-colored building at the center of this photo is the Albert P. Crary Science & Engineering Center. A Coast Guard icebreaker in Winter Quarters Bay is tied to the pier, which is built of ice.. The small hut on Hut Point in the background was built by Robert F. Scott in 1902 and is protected as a historic site under the Antarctic Treaty.


The station, established in December 1955, is the logistics hub of the USAP, with a harbor, landing strips on sea ice and shelf ice, and a helicopter pad. Its 85 or so buildings range in size from a small radio shack to large, three-story structures. Repair facilities, dormitories, administrative buildings, a firehouse, power plant, water distillation plant, wharf, stores, and warehouses are linked by above-ground water, sewer, telephone and power lines. The water and sewer lines are heat-taped and insulated.

The Albert P. Crary Science and Engineering Center at McMurdo was dedicated in November 1991. The laboratory is named in honor of geophysicist and glaciologist Albert P. Crary (1911-1987), the first person to set foot on both the North and South Poles. The laboratory contains state-of-the-art instrumentation to facilitate research and to advance science and technology. It contains personal computers and workstations and a local area network. It has laboratory space, analytical instrumentation and staging areas for a range of scientific disciplines. The laboratory also supports studies of snow and ice mechanics, meteorology and special activities, including environmental monitoring and enforcement. The lab has five pods built in three phases to provide 46,000 square ft. of working area. Phase I has a two-story core pod and a biology pod. Phase II has Earth sciences and atmospheric sciences pods. Phase III has an aquarium. Other facilities are maintained for atmospheric sciences and other disciplines.

Williams Field, a skiway ten miles from McMurdo on the Ross Ice Shelf, is the aerodrome for ski-equipped airplanes. Wheeled airplanes use a harder, smoother runway on sea ice in October, November and into December, at which time the sea ice usually softens and becomes unusable. A permanent, hard-ice runway for wheeled planes, the Pegasus site on the Ross Ice Shelf, completed in 1992, can be used in all but the warmest (and, unfortunately, busiest) months (mid December to late January). Although the surface is available during the winter months, there is currently no lighting or other airfield support planned to enable winter operations.

Low and high recorded temperature extremes at McMurdo are -58°F and 46°F, respectively. Annual mean is 0°F; monthly mean temperatures range from 27°F in January to -18°F in August. Drifting snow can accumulate about four ft. per year, although the station becomes snow-free in summer. Average wind is about 11 miles per hour with a gust of 116 miles per hour having been recorded in July 1968.

Research is performed at and near McMurdo in marine and terrestrial biology, biomedicine, geology and geophysics, glaciology and glacial geology, meteorology, aeronomy, and upper atmosphere physics. Air transportation to New Zealand is frequent between October and February the Antarctic summer. The winter population is isolated from late February to late August (Exhibit 19).

Graph: McMurdo Station annual population cycle

Exhibit 19

McMurdo Station annual population cycle. In August, several flights from New Zealand ("Winfly") raise McMurdo's population from its winter minimum with early science projects and an augmentation of the support staff to prepare for summer. In October the population rises quickly, and for the duration of the summer operating season people arrive and depart several times a week. In late December the "Christmas notch" coincides with the annual loss of nearby sea ice as a working platform and reflects the replacement of scientists (particularly biologists) who require it with those (such as geologists) who do not; the transition from the Fall to the Spring semesters at U.S. academic institutions also affects this population shift. In late February, when reduced daylight and plummeting temperatures make field research impractical, the population drops to the winter minimum.

The 96/97 curve (green line) shows a lower population in the 1996 Winfly period (August-September) and in the 1997 winter from March onward. This cost-saving measure has resulted from consolidation of functions. The 96/97 season also shows a USAP first a "reverse Winfly" in late February and early March. Instead of redeploying personnel in small numbers in several LC-130 trips, the USAP used an Air Force (wheeled) C-141 to redeploy a large number of personnel on one day, increasing the efficiency of McMurdo's late-summer tasks. The C-141 used McMurdo's recently developed Pegasus glacier runway.

In these curves, populations are plotted at weekly intervals for the three years June 1994 through May 1997.


4.2.2 Amundsen-Scott Station at the geographic South Pole (peak summer population capacity 173; 1996 winter, 27)

Americans have occupied the geographic South Pole continuously since November 1956. The central facility of the South Pole Station (Exhibit 20) was rebuilt in 1974 as a geodesic dome 160 ft. wide and 50 ft. high that covers modular buildings for living and science. Adjacent to the dome are steel archways, 22-ft. high, 44 ft. across, and 830 ft. long, that house the station's main fuel supply, the power house, a medical facility, and other functions. Detached buildings house instruments for monitoring the upper and lower atmosphere and for numerous complex projects in astronomy and astrophysics. Science and berthing structures were added in the 1990s, the former mostly for astronomy, and there is a summer camp which also serves as an emergency camp during winter in case the principal facilities should be lost. The station's winter personnel are isolated between mid-February and late October.

Photo: Main entrance to South Pole Station

Exhibit 20

Amundsen-Scott Station Shown is the main entrance to Amundsen-Scott South Pole Station. (The sign has been discolored by diesel-powered tractors delivering supplies.)


Recorded temperature has varied between 7°F and 117°F. Annual mean is -56°F; monthly means vary from -18°F in December to -76°F in July. During the warmest month of the year, temperatures of -38°F have been recorded, making construction difficult. Average wind is 12 miles per hour; peak gust recorded was 54 miles per hour. Snowfall is about four inches of ice equivalent per year, although drifting can and does add more around buildings. The station stands at an elevation of 9,300 ft. on interior Antarctica's nearly featureless ice sheet, about 9,350 ft. thick at that location.

Research at the station includes glaciology, geophysics, meteorology, upper atmosphere physics, astronomy, astrophysics, and biomedical studies.

The station's name honors Roald Amundsen and Robert F. Scott, who reached the South Pole the austral summer of 1911-1912.

4.2.3 Palmer Station, on Anvers Island immediately west of the Antarctic Peninsula (peak summer population capacity 43; 1996 winter, about 20)

Palmer Station (Exhibit 21), on a protected harbor on the southwestern coast of Anvers Island, off the Antarctica Peninsula, is the only U.S. Antarctic station north of the Antarctic Circle. The temperature is mild, with monthly averages ranging from +18°F in July and August to +36°F in January and February. The annual mean is 27°F. The extreme range is -24°F to 48°F. It has rained every month at Palmer Station, and in the year ended October 1981 Palmer received 10 inches of rain and over 100 inches of snowfall.

Photo: Palmer Station

Exhibit 21

Palmer Station, at 64°S, is north of the Antarctic Circle. It is supplied entirely by ship.


The station, built on solid rock, consists of two major buildings and three small ones plus two large fuel tanks, a helicopter pad, and a dock. Construction was completed in 1968, replacing a prefabricated wood structure ("Old Palmer," established in 1965) a mile away across Arthur Harbor. Old Palmer has been disassembled and removed from Antarctica. Palmer does not have a period of winter isolation as do McMurdo and South Pole; an ice-strengthened ship can transit to and from Palmer any month of the year, generally crossing the Drake Passage from South America.

Palmer Station is superbly located for biological studies of birds, seals, and other components of the marine ecosystem. It has a large and extensively equipped laboratory and sea water aquaria. In 1990 it was designated by the NSF as a long-term ecological research site. Meteorology, upper atmosphere physics, glaciology, and geology also have been pursued at and around Palmer. The station operates in conjunction with an ice-strengthened research ship described below.

Palmer Station is named for Nathaniel Brown Palmer, a Connecticut sealer who commanded the 46-ft. sloop Hero, which on 16 and 17 November 1820 entered Orleans Strait and came very close to the Antarctic Peninsula at about 63°45'S. At the time, Palmer was 21-years old. Later in his life, he won wealth and fame as a pioneer clipper ship master and designer.

4.2.4 The 219-ft. ice-strengthened research ship Polar Duke (year-round)

Polar Duke (Exhibit 22), built in 1983, is an ice-strengthened research ship under charter to the Foundation since January 1985. It operates in the Antarctic Peninsula area and calls at Punta Arenas, Chile, and, occasionally other South American ports, throughout the year. The ship resupplies Palmer Station, and it performs research and research support in collaboration with the station. It has a crew of 14 and can accommodate 23 scientific personnel. Polar Duke cruises at 12 knots, has an endurance of 90 days, and is well equipped with laboratories, winches, a piston corer, single channel seismic gear, and other equipment for biology, geology, and geophysics.

Photo: research ship Polar Duke

Exhibit 22

The research ship Polar Duke has been under charter to the U. S. Antarctic Program since 1984. It is performing a scientific mission here on the west side of the Antarctic Peninsula.


R/V Laurence M. Gould, a purpose-built ship under construction by Edison Chouest Offshore Inc., will replace Polar Duke in 1997. The NSF's contractor, Antarctic Support Associates, is procuring Gould as a one-for-one replacement charter vessel; Gould is slightly larger and more capable than Duke.

4.2.5 The R/V Nathaniel B. Palmer, a 309-foot research vessel with icebreaking capability (year-round)

Edison Chouest Offshore Inc., Galliano, Louisiana, in 1992 built and delivered this research vessel (Exhibit 23) with icebreaking capability for use by the USAP. The ship is a highly capable platform for global change studies, including biological, oceanographic, geological, and geophysical components. It can operate safely year-round in Antarctic waters that often are stormy or covered with sea ice. It accommodates 37 scientists, has a crew of 22, and is capable of 75-day missions.

Photo: research icebreaker Nathaniel B. Palmer

Exhibit 23

The research icebreaker Nathaniel B. Palmer has an A-frame for stern trawling and facilities on the starboard side for oceanographic sampling.


4.2.6 A U.S. Coast Guard Polar-class icebreaker (399 ft.) for icebreaking, channel tending, and supply-ship escort in McMurdo Sound and for additional support and science functions (austral summer)

A Polar-class (Exhibit 24), America's most powerful icebreaker, operates annually in the Antarctic. Either the Polar Star or the Polar Sea, operated by the U.S. Coast Guard, breaks a channel through McMurdo Sound and performs other logistics tasks.

Photo: Polar Sea breaking ice

Exhibit 24

USCGC Polar Sea breaking the annual resupply channel to McMurdo Station. Photograph © 1989 Neelon Crawford.


Polar-class icebreakers displace 14,700 tons. Their diesel engines provide 18,000 hp for normal operations. When required for icebreaking, gas turbines can be operated to increase the power to nearly 60,000 hp. In open water these ships cruise at 13 knots, maximum speed of 17 knots. Each ship carries two helicopters. Crew size is 154; the ship can accommodate 20 scientists.

4.2.7 Military Sealift Command ice-strengthened cargo and tank ships (one each, once per year) for cargo and fuel delivery to and waste removal from McMurdo Station.

Each year an ice-strengthened tanker delivers approximately six million gallons of fuel to McMurdo Station. It is operated under contract to the Military Sealift Command.

A yearly visit by USNS Green Wave (Exhibit 25) or a similar ice-strengthened container ship delivers most of the cargo used at McMurdo and inland stations, and takes USAP waste to the U.S. for recycling or disposal. The ship is operated under contract to the Military Sealift Command.

Photo: cargo ship Green Wave

Exhibit 25

Green Wave. This cargo ship re-supplies McMurdo once per year at mid-summer and removes the year's accumulated collection of waste. It is not an icebreaker and requires icebreaker escort to assure entry to McMurdo's port, even in a light ice year. The pier is constructed of ice, built up in layers and reinforced with steel cable. Locally obtained aggregate paves the surface during the offload period.


4.2.8 LC-130 ski-equipped aircraft operated by the Navy and the Air National Guard (August and October-March)

The LC-130 four-engine turboprop transport aircraft (Exhibit 26) is the backbone of U.S. transportation within Antarctica and also provides air service between McMurdo Station and New Zealand. The LC-130 is the polar version of the familiar C-130 cargo plane; its major unique feature is the ski-equipped landing gear which enables operation on snow or ice surfaces throughout Antarctica. The plane, introduced to the Antarctic program in 1960, also has wheels for landing on prepared hard surfaces. As discussed elsewhere in this report, the NSF's fleet of seven aircraft has been operated by the U.S. Navy. One NSF LC-130 is operated by the Air National Guard in Antarctica. Two additional LC-130s, owned and operated by the Air National Guard, also are used in the U.S. Antarctic Program. These two groups, the Navy and Air National Guard, are the only LC-130 operators in the world, and the Air National Guard is in the process of assuming operational control of all LC-130s.

Photo: LC-130 Hercules

Exhibit 26

LC-130 Hercules is equipped for both ski and wheel takeoffs and landings.


The aircraft has a cargo box of 40x10x10 ft. It can, as an example, carry 27,000 pounds of personnel and/or cargo from McMurdo to South Pole (728 nautical miles), then return to McMurdo without refueling (aircraft engines are never shut down at the Pole). It cruises at 275 knots.

4.2.9 Contract operation of smaller (e.g., Twin Otter) research and support airplanes (austral summer)

When required, deHavilland Twin Otter turboprop airplanes (Exhibit 27) have been chartered for operations in Antarctica. These aircraft have proved so useful that they are now employed each summer season. Skis are fitted and the planes can land on open snow and ice. The payload and range of a Twin Otter are substantially less than those of the LC-130 but greater than those of helicopters used in the program.

Photo: Twin Otter

Exhibit 27

Ski-equipped Twin Otter under seasonal charter to the U. S. Antarctic Program.


4.2.10 Contract helicopter operations (austral summer)

Petroleum Helicopters Inc. (PHI) of Lafayette, Louisiana, in 1996 won a competitively bid contract from the NSF to provide McMurdo-based helicopter operations (Exhibit 28) as a part of the planned withdrawal of the U.S. Navy from Antarctica. The first austral summer season of operation was 1996-1997. This transition has had a favorable impact on cost and operations.

Photo: helicopter being unloaded from USAF C-5 airplane

Exhibit 28

A PHI contract helicopter being unloaded from a USAF C-5 on the sea-ice runway at McMurdo, October 1996.


The number of personnel dedicated to McMurdo helicopter operations has decreased from 52 to 12. The aircraft complement has decreased from six Navy Hueys to four commercial helicopters: three AS350B2 Squirrels and one Bell 212 civilian Huey. The Squirrels are smaller than the Huey, carrying half the passengers and 60 percent of the maximum cargo load, but have an altitude and airspeed advantage over the medium-lift Huey.

Helicopter operations costs have decreased from $5M to $2.5M annually, with no concomitant decrease in flight hours (1,800 per season). The safety record in recent years has been excellent. The NSF anticipates a 22 percent reduction in flight hours with no decrease in effective support through such innovations as further utilizing a special fueling station established at Marble Point near to the Dry Valleys. Dry Valley science support can then be conducted without nonproductive transits to and from McMurdo's main fueling station.

The learning curve for this new commercial operation was generally as the NSF had anticipated. Subsequent season ramp-ups are expected to be more efficient, with pilot training reduced to a few hours of refresher flying in the first week of operations assuming higher season-to-season retention and reassignments of pilots and mechanics and level of experience than was the case with military pilots.

PHI will leave its helicopters in Antarctica over the winter for the duration of the contract (five years), whereas the Navy returned some of its helicopters to California at the end of each season. This change will decrease airlift requirements for the helicopters.

The Office of Aircraft Services, Department of the Interior, provided contract acquisition support to the NSF and provides one employee at McMurdo during the operating season to perform technical contract oversight.

4.2.11 Specially equipped aircraft, balloons, and other remote-sensing platforms

Research grantees occasionally require specialized support operations in Antarctica for various types of remote sensing from aircraft, high altitude balloon operations, remotely operated underwater vehicles, etc. The NSF either approves services arranged by the grantees themselves or arranges for support of these operations by its support contractor, Antarctic Support Associates (ASA).

4.2.12 Unattended, automated weather stations and geophysical observatories

The USAP automatic weather station project, conducted by the University of Wisconsin with the support of an NSF grant, places weather units in remote areas of Antarctica in support of meteorological research and operations. The data are collected by the ARGOS Data Collection System on board the National Oceanic and Atmospheric Administration series of polar-orbiting satellites. In 1995 there were 49 units at locations around Antarctica. The development of low-power computer components made possible the development of low-power automated weather units capable of operating in the extreme climate of Antarctica and the distribution of the data globally in near real time.

Automated geophysical observatories (Exhibit 29), with six installed on the Antarctic polar plateau, collect a variety of geophysical data for investigators. The Science Support Division of ASA manages this project in the field.

Photo: geophysical observatory

Exhibit 29

This automatic geophysical observatory is one of six deployed to various locations throughout Antarctica. The Program's 50 Antarctic weather stations are smaller devices.


4.2.13 Field camps placed widely across the continent

Approximately 30 field camps are established each austral summer to support specific projects (Exhibit 30).

Photo: typical field camp

Exhibit 30

A typical field camp, using tents and a portable shelter. Major camps

During some summer seasons, the U.S. establishes and operates one or more major summer research camps in areas of particular scientific interest. Typically these camps consist of Jamesways (quickly erected structures made of canvas and wood), which support a population of 40 to 60 during the November-January period. Helicopters or Twin Otter airplanes are taken to the site and used to support scientific operations. Motor toboggans also are employed. Such camps have been operated at a variety of locations: on the Siple Coast, the Shackleton Glacier, at "Beardmore South" in the central Transantarctic Mountains (1985-1986), northern Victoria Land (1981-1982), the Ellsworth Mountains (1979-1980), at Darwin Glacier in the Transantarctic Mountains (1978-1979), and in the mountains of northern Marie Byrd Land (1977-1978). Geology, geophysics, glacial-geology, glaciology, and terrestrial biology have been pursued at these camps, which often have significant international involvement (Exhibit 31).

Graphic: The Cape Roberts Project

Exhibit 31

International cooperation in Antarctic research can be as simple as a scientist working at another nation's station or as complex a project as the Antarctic Stratigraphic Drilling Project at Cape Roberts. Field work is to begin in the 1997-1998 austral summer. Illustration courtesy of Peter N. Webb, Byrd Polar Research Center, The Ohio State University. Huts

If summer research projects are expected to continue over several seasons at the same location, huts may be erected. Huts can be expected to last for several years, and they provide space, stable working areas, and comfort not achievable with tents or Jamesways. Huts have been used in recent years in Taylor Valley (an ice-free, dry valley in southern Victoria Land) for study of lake ecosystems, at Cape Crozier on Ross Island for population and behavioral studies of penguin rookeries, and near the summit of Mount Erebus for volcanology. Resupply and transport are by helicopter or tracked vehicle from McMurdo Station. Tents

Small parties requiring temporary shelter use single- or double-walled tents of several designs, both modern and traditional. These designs include the Scott tent, a pyramid shaped tent similar to the design used by Robert F. Scott early in this century. These tents are stable in high winds and can be erected quickly. Cold-weather sleeping bags are used on ground cushions, and cooking is by portable stoves. Tent camps usually are placed or moved by helicopter or motor toboggan. Extended backpacking trips generally are not practical in Antarctica owing to the weight of the equipment and the fuel required to melt ice for water, to cook, and to combat the cold. All tent camps and huts are required to have radios, and all parties maintain daily contact with the nearest station.

4.2.14 Antarctic Activities of Other Federal Agencies

Presidential Memorandum 6646 (1982) states that, "Other agencies (than NSF) may, however, fund and undertake directed short-term programs of scientific activity . . . . Such activities shall be coordinated within the framework of the National Science Foundation logistics support."

The National Aeronautics and Space Administration's (NASA) Antarctic activity includes suborbital studies of cosmic radiation and the Sun, study and archiving of meteorites, microbial studies with extraterrestrial applications, sea ice and ice sheet studies, stratospheric measurements related to ozone, a synthetic-aperture radar ground station, technology development (e.g., a food growth and waste recycling system for South Pole Station), and human factors including isolation and confinement and other analog studies. Using 1995 as an indicator, NASA funding was about $6M, in addition to expenditures for staff. The National Oceanic and Atmospheric Administration (NOAA) funds Antarctic climate monitoring, ozone studies, remote sensing (e.g., sea surface temperature, atmospheric temperature, cloud imagery), sea ice and iceberg analyses, and marine living resources research at about $4M per year. The U.S. Geological Survey (USGS) performs Antarctic mapping, geology, geophysics, glaciology, and long-term ecological monitoring at about $2M per year. The Department of Energy and the Smithsonian Center for Astrophysics fund astrophysics in the Antarctic at $140,000 and $115,000 per year, respectively.

Other agencies dealing with Antarctic matters include the U.S. Coast Guard, the Marine Mammal Commission, the Department of State (international representation, the U.S. role under the Antarctic Treaty, and chairing the interagency policy mechanism), the Environmental Protection Agency (environmental advice and oversight), and the Council on Environmental Quality (environmental protection policy).

Through NSF reimbursement, the Department of the Interior provides leasing services for non-DOD aircraft; the Naval Electronics Command, satellite communications expertise; the Department of Transportation, variable costs of icebreaker operations; and the Department of Defense, as discussed throughout the report, the backbone of Antarctic heavy-lift air and sea logistics.

4.3 Recent History of U.S. Science in Antarctica

U.S. researchers working in Antarctica have seen many changes in science support in the last two decades. The primary changes have been in the shift from predominantly military to predominantly contractor support and in the greater emphasis placed on research as the primary expression of the U.S. presence in Antarctica.

In the 1970s, there were approximately six support personnel (military and civilian) on the Ice for every scientist. The scientific facilities onshore at Palmer, McMurdo, and South Pole stations were generally unsuitable for conducting "cutting-edge" research. Scientific instrumentation in the laboratories was minimal and often outdated. Communication with fellow scientists back in the U.S. was poor to non-existent, and there was no efficient way to transmit data back to the U.S. Aside from a decade of research in the 1970s supported capably by the ice-strengthened USNS Eltanin, the primary oceanographic effort in Antarctica was based on U.S. Coast Guard icebreakers. Two icebreakers sailed to the Ice each year, one Polar-class ship whose mission was to break the passage to McMurdo Station, and another ship, the Glacier, whose mission was intended to be science. From 1968 to 1984 the program had a 125-ft. ice-capable wood ship, Hero, that complemented Palmer Station; in 1985 the ice-strengthened, 219-ft. research vessel Polar Duke was acquired on a long-term lease to replace Hero. The Polar Duke was a substantial improvement over the Hero and the Glacier, but could not compare to research vessels in the U.S. academic fleet, all but one of which are not ice-capable.

Considerable improvement in the infrastructure for support of Antarctic research has occurred in the past two decades, particularly since 1990 (Exhibit 32). Improved facilities and new instrumentation at South Pole Station have provided atmospheric scientists and astronomers with the first real opportunity to conduct cutting edge science on the Ice, demonstrated by projects such as the Center for Astrophysical Research in Antarctica (CARA), which began in 1991. In 1991-92 the new research laboratory, the Albert P. Crary Science and Engineering Center, opened at McMurdo Station. This facility provides scientists with state of the art instrumentation, particularly for biology and biochemistry. Also, a new research vessel, R/V Nathaniel B. Palmer, was launched in 1992. The Palmer is the first U.S. icebreaking research vessel with scientific capabilities equal to those of other research vessels in the U.S. scientific fleet. It is also the first U.S. Antarctic research icebreaker capable of accommodating more scientists and science support staff than crew.

Graph: Number of projects and research personnel

Exhibit 32

Number of projects and research personnel compared to budget. Research-support capability has changed significantly in the USAP from 1985 to 1997, with more added than deleted. Exploiting these new capabilities, the number of research projects and research personnel (rough measures of science productivity) has grown, and at a rate faster than that of the USAP budget. Two budget initiatives during this time were for SEH (safety, environmental protection and health upgrades) in FY90-FY94 and LC-130 aircraft procurement in FY93. Most cited facilities and activities are described in the text. Glacier was an icebreaker configured to support onboard research. Siple Station, near the base of the Antarctic Peninsula, supported upper atmosphere research. LTER: Long term ecological research.


Because the improved scientific infrastructure in Antarctica enables better science, a greater number of scientists have turned their attention to Antarctica and the level of sophistication of experiments being conducted there has increased.

The portion of the USAP budget spent in research grants to scientists has risen from 10 percent in 1984-85 to nearly 16 percent in 1996-97 (Exhibit 33) and the portion of the budget directly attributable to field support of research has kept pace with this change. In FY95, total research grants and research support was 36 percent of the USAP budget, with the balance (64 percent) providing operations and logistics (station operations, etc.) not directly attributable to specific research projects.

Graph: USARP and Operational Support Budgets

Exhibit 33

USARP (U. S. Antarctic Research Program) and Operational Support Budgets, FY85-FY97. The USARP budget that part of the USAP budget that consists of direct award of funds to scientists at institutions for research projects rose from 10 percent of the USAP in FY85 to 16 percent in FY97. In FY95 the USARP portion was 14.8 percent of the USAP budget of $196M; funds expended in direct operational support of each of these research projects equaled 21.5 percent, and funds expended for logistics and operations not attributable to specific research projects equaled 63.7 percent.


Since FY89, the number of research projects and scientific personnel working in the Antarctic has increased more-or-less steadily so that the USAP dollars per project has decreased (Exhibit 34 and Exhibit 35).

Graph: number of research projects

Graph: number of research personnel

Exhibits 34 and 35

These graphs compare (upper) the number of research projects (which vary significantly in size within any year) and (lower) the number of research personnel to the total USAP budget for the years FY85-FY97, showing a downward trend in the cost per project and per researcher.


Within the research enterprise itself, modern science has tended to become more complex, demanding research teams composed of individuals with differing expertise and talents, and placing a greater demand on the science support infrastructure. Even with computers, more advanced communications and automated data gathering, as the science becomes more "high tech," the pressure for support personnel tends to increase.

Increased U.S. Antarctic scientific productivity since FY89 can be attributed to better utilization of the infrastructure during a period when the overall USAP budget (in 1997 constant dollars) was both rising (FY89-FY93) and falling (FY93-FY97). Based on the admittedly broad measures shown in the exhibits, productivity during the later years of the FY89-FY97 period compares very favorably with 1981-1985, when the number of science personnel was half today's number. The number of scientists in the 1981-1985 period exceeds the number in the years 1967-1971 by about 50 percent although in both these periods the USAP annual budget (in 1997 constant dollars) was about the same (Exhibit 15).