@prefix ns0: <https://gcmd.earthdata.nasa.gov/kms#> .
@prefix skos: <http://www.w3.org/2004/02/skos/core#> .

<https://gcmd.earthdata.nasa.gov/kms/concept/208283b3-1869-46df-8d4d-5b52c799a149>
  ns0:altLabel [ ] ;
  skos:broader <https://gcmd.earthdata.nasa.gov/kms/concept/996e8a4b-e690-4a9c-afcf-205fff95b38b> ;
  skos:prefLabel "JARE 25"@en ;
  skos:inScheme <https://gcmd.earthdata.nasa.gov/kms/concepts/concept_scheme/projects> ;
  skos:definition """A number of governmental agencies cooperatively conduct Japanese
 Antarctic research under the name of the Japanese Antarctic
 Research Expedition (JARE). All decisions and approval of
 proposals for research activities rest with the Headquarters of
 JARE under the chairmanship of the Minister of Education,
 Culture, Sports, Science and Technology. The Secretariat of the
 JARE Headquarters belongs to the Science and International
 Affairs Bureau, Monbukagakusho.  The task of NIPR is to operate
 JARE both for scientific programs and logistics, except the
 transportation of personnel and materials by the icebreaker
 Shirase from Japan to Antarctica. Scientific programs at Syowa
 Station cover the following fields: upper atmosphere physics,
 meteorology, seismology, gravimetry, geodesy and cartography,
 oceanography, glaciology, geology, geography, marine and
 terrestrial biology, and medical research. Programs offered on
 board the Shirase include the following subjects: ionosphere,
 meteorology, geomagnetism, gravimetry, and physical, chemical
 and biological oceanography.  All Japanese scientific stations
 in Antarctica belong to NIPR. Syowa Station, the mother station
 of JARE, was established in January 1957, at 69?00'S and
 39?35'E on East Ongul Island, Lutzow-Holm Bay, East
 Antarctica. The total floor area of the buildings has increased
 from 184m? (3 buildings) in 1957 to 5,930.5m? (48 buildings)
 and other outdoor facilities in 2001.  Mizuho Station was
 established in July 1970 along the geomagnetic meridian passing
 through Syowa Station. It is located on the inland ice sheet at
 70?42'S and 44?20'E (2,230m above sea level), about 270km
 southeast of Syowa. After intermittent occupation, a few
 members maintained year-round operation from 1976 to 1986,
 making observations on meteorology, glaciology, and upper
 atmosphere physics.  It has been closed since 1987 and is
 occasionally visited by some parties for meteorological and
 glaciological observations.  Asuka Station was established in
 December 1984 on the ice sheet north of the Sor-Rondane
 Mountains, at 71?32'S and 24?08'E (930m above sea level). Most
 of the station facilities of about 450m? in total floor area
 have become buried under snow. The principal role of the
 station is to support field work in geology, geomorphology,
 meteorite searches, glaciology and biology in the Sor-Rondane
 Mountains. However, year-round observations including
 meteorology, glaciology, solid earth geophysics, and upper
 atmosphere physics were conducted between 1987 to 1991. Since
 1991, the station activities have been suspended. Dome Fuji
 Station equipped with 8 buildings, 407m? in total, was
 established in 1995 at 77?19'01"S and 39?42'12"E (3,810m above
 sea level) for the deep drilling program and atmospheric
 observations.  In recent years, environmental protection of
 Antarctica and its unique ecosystems has become increasingly
 important in planning and conducting Antarctic research. In
 accordance with the protocol on environmental protection in the
 Antarctic Treaty, appropriate procedures for environmental
 protection are followed in the Japanese Antarctic Research
 Expeditions.  A new program for monitoring changes in global
 and regional environments and ecosystems was started at Syowa
 Station and its coastal and inland vicinity in 1997. The
 monitoring programs include major parameters of atmospheric
 glaciological, solid geophysical and biological changes, such
 as atmospheric carbon dioxide concentration, sea level,
 population of penguins etc. Pollutants in seawater, ice or snow
 and in animals, such as heavy metals and organic chlorinated
 compounds derived from global and regional sources, are
 occasionally measured. The monitoring of global environmental
 change is an essential part of basic scientific programs as
 described in the previous chapter.

For more information,
link to "http://www.nipr.ac.jp/english/antarctic/t01_jare.html"

[Summary provided by National Institute of Polar Research]"""@en ;
  a skos:Concept .

<https://gcmd.earthdata.nasa.gov/kms/concept/996e8a4b-e690-4a9c-afcf-205fff95b38b>
  skos:prefLabel "J - L"@en ;
  a skos:Concept ;
  skos:narrower <https://gcmd.earthdata.nasa.gov/kms/concept/208283b3-1869-46df-8d4d-5b52c799a149> .

