@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/846c4465-17df-47c5-b5e7-7486765a2d5d>
  ns0:altLabel [ ] ;
  skos:broader <https://gcmd.earthdata.nasa.gov/kms/concept/996e8a4b-e690-4a9c-afcf-205fff95b38b> ;
  skos:prefLabel "JARE 18"@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/846c4465-17df-47c5-b5e7-7486765a2d5d> .

