From Surf Wiki (app.surf) — the open knowledge base
Vostok Station
Russian research station in Antarctica
Russian research station in Antarctica
| Field | Value |
|---|---|
| name | Vostok Station |
| native_name | станция Восток |
| native_name_lang | ru |
| settlement_type | Antarctic base |
| image_skyline | Vostok Station 2024.png |
| imagesize | 300 |
| image_caption | Vostok Station as of 2024 |
| flag_size | 110px |
| flag_border | no |
| mapsize | 270px |
| pushpin_map | Antarctica |
| pushpin_map_alt | Location of Vostok Station in Antarctica |
| pushpin_map_caption | Location of Vostok Station in Antarctica |
| pushpin_mapsize | 270 |
| pushpin_relief | yes |
| coordinates | |
| subdivision_type | Country |
| subdivision_name | Russia |
| subdivision_type1 | Location |
| subdivision_name1 | Princess Elizabeth Land |
| Antarctica | |
| subdivision_type3 | Administered by |
| subdivision_name3 | Arctic and Antarctic Research Institute |
| established_title | Established |
| established_date | |
| named_for | Vostok |
| elevation_footnotes | |
| elevation_m | 3,488 |
| population_as_of | 2017 |
| population_footnotes | |
| population_blank1_title | Summer |
| population_blank1 | 30 |
| population_blank2_title | Winter |
| population_blank2 | 15 |
| utc_offset1 | +5 |
| blank_name_sec1 | Type |
| blank_info_sec1 | All-year round |
| blank1_name_sec1 | Period |
| blank1_info_sec1 | Annual |
| blank2_name_sec1 | Status |
| blank2_info_sec1 | Operational |
| blank_name_sec2 | Activities |
| blank_info_sec2 | |
| code1_name | UN/LOCODE |
| code1_info | AQ VOS |
| website |
Antarctica
| nativename-a = | nativename-r = | image-width = | image2-width = | owner-oper = | city-served = | elevation-f = 11,447 | elevation-m = 3,489 | metric-elev = | r1-number = 03/21 | r1-length-f = 11,933 | r1-length-m = 3,637 | r1-surface = Ice | metric-rwy = | h1-number = | h1-length-f = | h1-length-m = | h1-surface = | stat1-header = | stat1-data = | stat-year =

Vostok Station (, , ) is a Russian research station in inland Princess Elizabeth Land, Antarctica. Founded by the Soviet Union in 1957, the station lies at the southern Pole of Cold, with the lowest reliably measured natural temperature on Earth of −89.2 C. Research includes ice core drilling and magnetometry. Vostok was named after Vostok, the lead ship of the First Russian Antarctic Expedition captained by Fabian von Bellingshausen. The Bellingshausen Station was named after this captain (the second ship, Mirny, captained by Mikhail Lazarev, became the namesake for Mirny Station).
Description
Vostok Research Station is around 1301 km from the Geographic South Pole, at the middle of the East Antarctic Ice Sheet.
Vostok is located near the southern pole of inaccessibility and the south geomagnetic pole, making it one of the optimal places to observe changes in the Earth's magnetosphere. Other studies include actinometry, geophysics, medicine and climatology.
The station is at 3488 m above sea level and is one of the most isolated established research stations on the Antarctic continent. The station was supplied from Mirny Station on the Antarctic coast. The station normally hosts 30 scientists and engineers in the summer. In winter, their number drops to 15.
The only permanent research station located farther south is the Amundsen–Scott South Pole Station, operated by the United States at the geographic South Pole. The Chinese Kunlun 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 in Vladimir Sanin's books such as Newbie in the Antarctic (1973), 72 Degrees Below Zero (1975), and others.
History

Vostok Station was established on 16 December 1957 (during the International Geophysical Year) by the 2nd Soviet Antarctic Expedition and was operated year-round for more than 72 years. The station was temporarily closed from January 1962 to January 1963, from February to November 1994,
In 1974, when British scientists in Antarctica performed an airborne ice-penetrating radar 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. In 1991, Jeff Ridley, a remote-sensing specialist with the Mullard Space Science Laboratory at University College London, directed a European satellite called ERS-1 to turn its high-frequency array toward the center of the Antarctic ice cap. It confirmed the 1974 discovery, but it was not until 1993 that the discovery was published in the Journal 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 140 subglacial 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 radar altimetry. Lake Vostok lies some 4000 m below the surface of the central Antarctic ice sheet and covers an area of 14000 km2.
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 in Saint 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.
On January 28, 2024, Russian President Vladimir 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.
Historic monuments
Vostok Station Tractor: Heavy tractor AT-T 11, which participated in the first traverse to the south geomagnetic pole, along with a plaque to commemorate the opening of the station in 1957, has been designated a Historic Site or Monument (HSM 11) following a proposal by Russia to the Antarctic Treaty Consultative Meeting.
Professor Kudryashov's Drilling Complex Building: The drilling complex building stands close to Vostok Station at an elevation of 3488 m. It was built in the summer season of 1983–1984. Under the leadership of Professor Boris Kudryashov, ancient ice 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.
Climate
Vostok Station has an ice cap climate (EF), with subzero temperatures year round, typical as with much of Antarctica. Annual precipitation is only 22 mm (all occurring as snow), making it one of the driest places on Earth. On average, Vostok station receives 26 days of snow per year. 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.
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 inactive Plateau 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, and satellite readings have routinely detected colder temperatures in areas between Dome A and Dome F. The most recent record set was the October record low, set on 1 October 2021.

Vostok is one of the coldest places on Earth. The average temperature of the cold season (from April to September) is about -66 C, while the average temperature of the warm season (from October to March) is about -44 C.
The lowest reliably measured temperature on Earth of -89.2 C was in Vostok on 21 July 1983 at 05:45 Moscow Time, which was 07:45 for Vostok's time zone, and 01:45 UTC (See List of weather records). This beat the station's former record of -88.3 C on 24 August 1960. 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 on 28 July 1997.
The warmest recorded temperature at Vostok is -14.0 C, which occurred on 5 January 1974.
The coldest month was August 1987 with a mean temperature of -75.4 C and the warmest month was December 1989 with a mean temperature of -28 C.
In addition to the extremely cold temperatures, other factors make Vostok one of the most difficult places on Earth for human habitation:
- An almost complete lack of moisture in the air
- An average windspeed of 5 m/s, sometimes rising to as high as 27 m/s
- The lack of oxygen in the air because of its high elevation at 3488 m
- A higher ionization of the air
- A polar 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)
Acclimatization to such conditions can take from a week to two months and is accompanied by headaches, eye twitches, ear pains, nose bleeds, perceived suffocation, sudden rises in blood pressure, loss of sleep, reduced appetite, vomiting, joint and muscle pain, arthritis, and weight loss of 3-5 kg (sometimes as high as 12 kg).
Ice core drilling
In the 1970s, the Soviet Union drilled a set of cores 500 – 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 the Scientific Committee on Antarctic Research which expressed worries about possible contamination of Lake Vostok. This ice 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 the EPICA 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 m.
The ancient lake was finally breached on 5 February 2012 when scientists stopped drilling at the depth of 3770 m and reached the surface of the subglacial lake.
The brittle zone is approximately between 250 and 750 m and corresponds to the Last Glacial Maximum, with the end of the Holocene climatic optimum at or near the 250-metre depth.
Although the Vostok core reached a depth of 3623 m 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 3310 m or 414,000 years. 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. This then produces a record in agreement with the newer, longer EPICA record, although it provides no new information.
References
References
- (August 2017). "Antarctic Station Catalogue". [[Council of Managers of National Antarctic Programs]].
- "Vostok Skiway".
- [http://www.ncdc.noaa.gov/oa/climate/globalextremes.html Global Measured Extremes of Temperature and Precipitation.] [[National Climatic Data Center]]. Retrieved on 21 June 2007.
- Winchester, Simon. (2003). "Extreme Earth". Collins.
- (14 July 2018). "Mirny Observatory".
- "Deep drilling at Vostok station, Antarctica: history and recent events".
- (1967). "Scientific Stations in Antarctica, 1882-1963". Indian National Scientific Documentation Centre, New Delhi. (English translation 1971).
- (4 March 2003). "Russia abandons Ice Station Vostok".
- Oswald, G. K. A.. (1973). "Lakes beneath the Antarctic Ice Sheet". Nature.
- Morton, Oliver. (April 2000). "Ice Station Vostok".
- (2006). "Antarctica: contributions to global earth sciences : proceedings of the IX International Symposium of Antarctic Earth Sciences Potsdam, 2003". Birkhäuser.
- (27 December 2020). "A New Vostok!".
- (2024-01-28). "Путин дал старт вводу в эксплуатацию зимовочного комплекса станции "Восток"".
- (2012). "List of Historic Sites and Monuments approved by the ATCM (2012)". Antarctic Treaty Secretariat.
- (2013). "List of Historic Sites and Monuments approved by the ATCM (2013)". Antarctic Treaty Secretariat.
- "Vostok Station". Antarctic Research and Investigation.
- (24 June 2011). "Where are the World's Sunniest Destinations?".
- (2016). "Vostok station (89606)".
- Mary Albert. (March 2018). "Discovering historic Plateau Station". Norwegian-U.S. Scientific Traverse of East Antarctica}}{{dead link.
- "Vostok (Antarctica)". Ogimet.
- Budretsky, A.B.. (1984). "New absolute minimum of air temperature". [[Gidrometeoizdat]].
- Budretsky, A.B.. (1984). "New absolute minimum of air temperature (English Version)". [[Gidrometeoizdat]].
- Liang, Yong Li. (2000). "Coldest Temperature on Earth". The Physics Factbook.
- "Sunrise and sunset times in Vostok Station, May 2015".
- (1997). "Bubbly-ice densification in ice sheets: 11. Applications". J. Glaciol..
- [http://www.ncdc.noaa.gov/paleo/icecore/antarctica/vostok/vostok_data.html Vostok Ice Core Data] www.ncdc.noaa.gov, 2005-12-22. Retrieved 27 March 2007.
- (2005). "Palaeoclimatology: The record for marine isotopic stage 11". Nature.
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
Ask Mako anything about Vostok Station — get instant answers, deeper analysis, and related topics.
Research with MakoFree with your Surf account
Create a free account to save articles, ask Mako questions, and organize your research.
Sign up freeThis content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.
Report