The station is at 3,488 metres (11,444 ft) abovesea level and is one of the most isolated established research stations on the Antarctic continent.[4] The station was supplied fromMirny Station on the Antarctic coast.[5] The station normally hosts 30 scientists and engineers in the summer. In winter, their number drops to 15.[1]
The only permanent research station located farther south is theAmundsen–Scott South Pole Station, operated by the United States at the geographicSouth Pole. The ChineseKunlun Station is farther south than Vostok but is occupied only during summers.
Some of the challenges faced by those living on the station were described inVladimir Sanin's books such asNewbie in the Antarctic (1973),72 Degrees Below Zero (1975), and others.
Ice cores at Vostok, with a portion of the station behind
Vostok Station was established on 16 December 1957 (during theInternational Geophysical Year) by the2nd Soviet Antarctic Expedition and was operated year-round for more than 72 years.[6] The station was temporarily closed from January 1962 to January 1963,[7] from February to November 1994,[6] and during the winter of 2003.[8]
In 1974, when British scientists in Antarctica performed an airborne ice-penetratingradar survey and detected strange radar readings at the site, the presence of a liquid, freshwater lake below the ice did not instantly spring to mind.[9] In 1991, Jeff Ridley, a remote-sensing specialist with theMullard Space Science Laboratory atUniversity College London, directed a European satellite calledERS-1 to turn its high-frequency array toward the center of the Antarctic ice cap. It confirmed the 1974 discovery,[10] but it was not until 1993 that the discovery was published in theJournal of Glaciology. Space-based radar revealed that the subglacial body of fresh water was one of the largest lakes in the world—and one of some 140subglacial lakes in Antarctica. Russian and British scientists delineated the lake in 1996 by integrating a variety of data, including airborne ice-penetrating radar imaging observations and spaceborne radaraltimetry.Lake Vostok lies some 4,000 metres (13,000 ft) below the surface of the central Antarctic ice sheet and covers an area of 14,000 square kilometres (5,400 sq mi).[11]
In 2019, the Russian government began construction on a new, modern station building to replace the aging facilities. Construction of the new facility was completed inSaint Petersburg to be transported to Vostok Station by ship, but continuing delays have pushed back completion of the new station to no earlier than 2023.[12]
On January 28, 2024, Russian PresidentVladimir Putin took part in the ceremony of commissioning the station's wintering complex via video link. The ceremony was also attended by President of Belarus Alexander Lukashenko.[13]
Professor Kudryashov's Drilling Complex Building: The drilling complex building stands close to Vostok Station at an elevation of 3,488 metres (11,444 ft). It was built in the summer season of 1983–1984. Under the leadership of Professor Boris Kudryashov, ancientice core samples were obtained. The building has been designated a Historic Site or Monument (HSM 88), following a proposal by Russia to the Antarctic Treaty Consultative Meeting.[15]
Vostok Station has anice cap climate (EF), with subzero temperatures year round, typical as with much of Antarctica. Annual precipitation is only 22 millimetres (0.87 in) (all occurring as snow),[16] making it one of the driest places onEarth. On average, Vostok station receives 26 days of snow per year.[16] It is also one of the sunniest places on Earth, despite having no sunshine at all between May and August; there are more hours of sunshine per year than even the sunniest places inSouth Africa,Australia and theArabian Peninsula, where they approach those of theSahara inNorthern Africa.[17] Vostok has the highest sunshine total for any calendar month on Earth, at an average of 708.8 hours of sunshine in December, or 22.9 hours daily. It also has the lowest sunshine for any calendar month, with an absolute maximum of 0 hours of sunshine per month during polar night.[18]
Of official weather stations that are currently in operation, Vostok is the coldest on Earth in terms of mean annual temperature. However, it has been disputed that Vostok Station is the coldest-known location on Earth. The now inactivePlateau Station, located on the central Antarctic plateau, is believed to have recorded an average yearly temperature that was consistently lower than that of Vostok Station during the 37-month period that it was active in the late 1960s,[19] and satellite readings have routinely detected colder temperatures in areas between Dome A and Dome F.[citation needed] The most recent record set was the October record low, set on 1 October 2021.[20]
Source 2: Pogoda.ru.net (data for record highs/lows, except for March and August lows, and March high)[22]; (March record low)[23], (August record low)[24], and (March record high)[25]
Panoramic photo of Vostok Station showing the layout of the camp. The striped building on the left is the power station while the striped building on the right is where researchers sleep and take meals. The building in the background with the red- and white-striped ball on top is the meteorology building. Caves were dug into the ice sheet for storage, keeping cores at an ideal −55 °C (−67 °F) year-round. (Credit: Todd Sowers LDEO, Columbia University, Palisades, New York)
Vostok is one of thecoldest places on Earth. The average temperature of the cold season (from April to September) is about −66 °C (−87 °F), while the average temperature of the warm season (from October to March) is about −44 °C (−47 °F).[4]
Thelowest reliably measured temperature on Earth of −89.2 °C (−128.6 °F) was in Vostok on 21 July 1983 at 05:45Moscow Time,[26][27] which was 07:45 for Vostok's time zone, and 01:45UTC (SeeList of weather records). This beat the station's former record of −88.3 °C (−126.9 °F) on 24 August 1960.[24] Lower temperatures occurred higher up towards the summit of the ice sheet as temperature decreases with height along the surface.
Though unconfirmed, it has been reported that Vostok reached a temperature of −91 °C (−132 °F) on 28 July 1997.[28]
The warmest recorded temperature at Vostok is −14.0 °C (6.8 °F), which occurred on 5 January 1974.[22]
The coldest month was August 1987 with a mean temperature of −75.4 °C (−103.7 °F) and the warmest month was December 1989 with a mean temperature of −28 °C (−18 °F).[21]
In addition to the extremely cold temperatures, other factors make Vostok one of the most difficult places on Earth for human habitation:
Apolar night that lasts approximately 120 days, from late April to mid-August, including 85 continuous days of civil polar night (i.e. too dark to read, during which the sun is more than 6 degrees below the horizon)[29]
Acclimatization to such conditions can take from a week to two months and is accompanied byheadaches, eye twitches, ear pains, nose bleeds, perceived suffocation, sudden rises inblood pressure, loss of sleep, reducedappetite,vomiting, joint and muscle pain, arthritis, and weight loss of 3–5 kg (7–11 lb) (sometimes as high as 12 kg (26 lb)).[citation needed]
420,000 years of ice core data from Vostok, Antarctica, research station. Current period is at left. From bottom to top:insolation at 65°N due toMilankovitch cycles (connected to18O);18O isotope ofoxygen; levels ofmethane (CH4); relative temperature; levels ofcarbon dioxide (CO2)
In the 1970s, theSoviet Union drilled a set of cores 500–952 metres (1,640–3,123 ft) deep. These have been used to study the oxygen isotope composition of the ice, which showed that ice of the last glacial period was present below about 400 metres' depth. Then three more holes were drilled: in 1984, Hole 3G reached a final depth of 2,202 m; in 1990, Hole 4G reached a final depth of 2,546 m; and in 1993 Hole 5G reached a depth of 2,755 m; after a brief closure, drilling continued during the winter of 1995. In 1996 it was stopped at a depth of 3,623 m, by the request of theScientific Committee on Antarctic Research which expressed worries about possible contamination ofLake Vostok. Thisice core, drilled collaboratively with the French, produced a record of past environmental conditions stretching back 420,000 years and covering four previous glacial periods. For a long time, it was the only core to cover several glacial cycles; but in 2004 it was exceeded by theEPICA core, which, while shallower, covers a longer time span. In 2003, drilling was permitted to continue but was halted at the estimated distance to the lake of only 130 metres (430 ft).
The ancient lake was finally breached on 5 February 2012 when scientists stopped drilling at the depth of 3,770 metres (12,370 ft) and reached the surface of the subglacial lake.
Although the Vostok core reached a depth of 3,623 metres (11,886 ft) the usable climatic information does not extend down this far. The very bottom of the core is ice refrozen from the waters of Lake Vostok and contains no climate information. The usual data sources give proxy information down to a depth of 3,310 metres (10,860 ft) or 414,000 years.[31] Below this there is evidence of ice deformation. It has been suggested that the Vostok record may be extended down to 3,345 m or 436,000 years, to include more of the interesting MIS11 period, by inverting a section of the record.[32] This then produces a record in agreement with the newer, longer EPICA record, although it provides no new information.
^Dubrovin and Petrov, L. I. and V. N. (1967).Scientific Stations in Antarctica, 1882-1963(PDF). Indian National Scientific Documentation Centre, New Delhi. (English translation 1971). Retrieved2 February 2021.
^Raynaud, Dominique; Barnola, Jean-Marc; Souchez, Roland; Lorrain, Reginald; Petit, Jean-Robert; Duval, Paul; Lipenkov, Vladimir Y. (2005). "Palaeoclimatology: The record for marine isotopic stage 11".Nature.436 (7047):39–40.Bibcode:2005Natur.436...39R.doi:10.1038/43639b.PMID16001055.S2CID4363692.