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Iceberg C-19 is an iceberg that calved from the Ross Ice Shelf in May 2002 on a fissure scientists had been watching since the 1980s. After that the Ross Ice Shelf returned to the size it was in 1911, when it was mapped by Robert F. Scott’s party. It was the second-largest iceberg to calve in the region in a few years (after B-15). It had a surface area larger than 5500 km2. In summer 2003 C-19 moved northward very rapidly, passed Cape Adare, and broke in two pieces: C-19A and C-19B.

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  • Iceberg C-19 (en)
  • C-19 (ja)
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  • 氷山C-19は、1980年代から科学者たちが監視していた亀裂の場所で2002年5月にロス棚氷から分離した氷山。C-19の分離後、ロス棚氷は1911年にロバート・スコット隊により調査された時のサイズに戻った。C-19は最近この地域で生まれた氷山ではに次いで大きなものであり、面積は5,500平方キロメートル以上あった。 2002年中、C-19はロス海南部からの氷の移動を妨げた。その結果、春から夏の間氷の量が増加し植物プランクトンの大幅な減少をもたらした。 2003年夏、C-19は非常に速い速度で北へ向かいってを通過し、C-19AとC-19Bの2つに割れた。 2年間ビクトリアランド沿岸に留まった後、2005年9月にC-19Aは北へ流れ始めた。2006年3月時点の位置はバレニー諸島の西200キロメートルの太平洋であった。2008年5月時点での面積はおよそ5,141平方キロメートルであった。 (ja)
  • Iceberg C-19 is an iceberg that calved from the Ross Ice Shelf in May 2002 on a fissure scientists had been watching since the 1980s. After that the Ross Ice Shelf returned to the size it was in 1911, when it was mapped by Robert F. Scott’s party. It was the second-largest iceberg to calve in the region in a few years (after B-15). It had a surface area larger than 5500 km2. In summer 2003 C-19 moved northward very rapidly, passed Cape Adare, and broke in two pieces: C-19A and C-19B. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/C19a.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Iceberg_C19.jpg
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  • Iceberg C-19 is an iceberg that calved from the Ross Ice Shelf in May 2002 on a fissure scientists had been watching since the 1980s. After that the Ross Ice Shelf returned to the size it was in 1911, when it was mapped by Robert F. Scott’s party. It was the second-largest iceberg to calve in the region in a few years (after B-15). It had a surface area larger than 5500 km2. During 2002 C-19 prevented sea ice from moving out of the southwestern Ross Sea region and this blockage resulted in an unusually high sea ice level during spring and summer, thus provoking a huge reduction in phytoplankton production which is at the base of the food chain. In summer 2003 C-19 moved northward very rapidly, passed Cape Adare, and broke in two pieces: C-19A and C-19B. In September 2005, after a two-year stay along the coast of Victoria Land (west of French station Dumont d'Urville) C-19A started drifting northward. In March 2006 its location was in the Pacific Ocean, 200 km west of Balleny Islands. In 2008, C-19A was renamed Melting Bob by Max Dolan as a result of a contest sponsored by the Hay Festival and the Scott Polar Research Institute. As of May 2008, its surface area was approximately 5141 km2. (en)
  • 氷山C-19は、1980年代から科学者たちが監視していた亀裂の場所で2002年5月にロス棚氷から分離した氷山。C-19の分離後、ロス棚氷は1911年にロバート・スコット隊により調査された時のサイズに戻った。C-19は最近この地域で生まれた氷山ではに次いで大きなものであり、面積は5,500平方キロメートル以上あった。 2002年中、C-19はロス海南部からの氷の移動を妨げた。その結果、春から夏の間氷の量が増加し植物プランクトンの大幅な減少をもたらした。 2003年夏、C-19は非常に速い速度で北へ向かいってを通過し、C-19AとC-19Bの2つに割れた。 2年間ビクトリアランド沿岸に留まった後、2005年9月にC-19Aは北へ流れ始めた。2006年3月時点の位置はバレニー諸島の西200キロメートルの太平洋であった。2008年5月時点での面積はおよそ5,141平方キロメートルであった。 (ja)
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