https://repository.kopri.re.kr/handle/201206/9784 Tue, 14 Apr 2026 12:01:36 GMT 2026-04-14T12:01:36Z https://repository.kopri.re.kr/handle/201206/13024 Title: Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet Authors: Wei, Wei; Blankenship, Donald D.; Greenbaum, Jamin S.; Gourmelen, Noel; Dow, Christine F.; Richter, Thomas G.; Greene, Chad A.; Young, Duncan A.; Lee, SangHoon; Kim, Tae-Wan; Lee, Won Sang; Assmann, Karen M. Abstract: Antarctica’s Getz Ice Shelf has been rapidly thin- ning in recent years, producing more meltwater than any other ice shelf in the world. The influx of fresh water is known to substantially influence ocean circulation and bi- ological productivity, but relatively little is known about the factors controlling basal melt rate or how basal melt is spatially distributed beneath the ice shelf. Also unknown is the relative importance of subglacial discharge from the grounded ice sheet in contributing to the export of fresh water from the ice shelf cavity. Here we compare the ob- served spatial distribution of basal melt rate to a new sub-ice- shelf bathymetry map inferred from airborne gravity surveys and to locations of subglacial discharge from the grounded ice sheet. We find that melt rates are high where bathymet- ric troughs provide a pathway for warm Circumpolar Deep Water to enter the ice shelf cavity and that melting is en- hanced where subglacial discharge fresh water flows across the grounding line. This is the first study to address the rela- tive importance of meltwater production of the Getz Ice Shelf from both ocean and subglacial sources. Mon, 27 Apr 2020 00:00:00 GMT https://repository.kopri.re.kr/handle/201206/13024 2020-04-27T00:00:00Z https://repository.kopri.re.kr/handle/201206/10947 Title: Observations of the Antarctic Circumpolar Current Over the Udintsev Fracture Zone, the Narrowest Choke Point in the Southern Ocean Authors: Park, Y-H; Park, T.; Kim, Tae-Wan; Lee, Sang H.; Hong, C-S; Lee, J-H; Rio, M-H; Pujol, M-I; Ballarotta, M.; Durand, I.; Provost, C. Abstract: An up­to­date map of the Antarctic Circumpolar Current (ACC) fronts is constructed from the latest version of mean dynamic topography (MDT) from satellite altimetry and reveals the narrowest ACC width in the Udintsev Fracture Zone (UFZ), with the strongest concentration of the three major ACC fronts within a limited distance as short as 170 km, about 40% narrower than that at Drake Passage. At 144°W, at the entrance of the UFZ, which lies between the Pacific­Antarctic Ridge (PAR) and its eastwardly offset segment (offset PAR segment), there is a triple confluence of the Subantarctic Front, Polar Front, and Southern ACC Front . Downstream of this longitude, the Subantarctic Front progressively meanders northward over the relatively shallow offset PAR segment before channeling through the Eltanin Fracture Zone, thus diverging from the Polar Front which proceeds through the UFZ. In situ observations from two recent cruises at 144°W confirm the satellite altimetry­derived frontal circulation in the UFZ region and yield a baroclinic transport relative to the bottom of 113 × 106 m3/s, comparable to that through Drake Passage. The hydrographic sections show no Antarctic bottom water colder than 0.2 °C. Characteristics of major water masses are described, and the implications for their potential downstream modifications at Drake Passage are discussed in terms of the meridional overturning circulation across the ACC. Mesoscale eddy activity with periods shorter than 90 days is predominantly concentrated in the immediate downstream area of the offset PAR segment, suggesting a substantial poleward eddy heat flux there. Mon, 01 Jul 2019 00:00:00 GMT https://repository.kopri.re.kr/handle/201206/10947 2019-07-01T00:00:00Z https://repository.kopri.re.kr/handle/201206/10509 Title: Production of tyrosine-like fluorescence and labile chromophoric dissolved organic matter (DOM) and low surface accumulation of low molecular weight-dominated DOM in a productive Antarctic sea Authors: Chen, Meilian; Jung, Jinyoung; Lee, Yun Kyung; Kim, Tae-Wan; Hur, Jin Abstract: The Antarctic seas play critical roles in global carbon cycling. Yet, little is known about the dissolved organic matter (DOM) characteristics and the dynamics there. Here, we conducted an extensive study on the seawater DOM in the Amundsen Sea in the Pacific sector of the Southern Ocean. We found that low molecular weight fractions quantitatively dominated the DOM composition at the surface of the highly productive Amundsen Sea Polynya with the relative abundance reaching up to ~89%. Moreover, CDOM and tyrosine-like fluorescence generation were observed, with the average values of~2.4？2.6m？1 (a254) and ~0.3 RU, respectively. While there is a net positive accumulation of dissolved organic carbon (DOC) at the ocean's surface, the net accumulation was negative for the chromophoric DOM (CDOM), which suggests a labile nature for the freshly produced CDOM. The estimated net DOC production ratio was only ~9 ± 6%, which was less than the global level (~17%). This finding signified a low surface accumulation of DOM in the austral summer, which is potentially explained by its nonlimiting nutrients, photo- and/or bio-labile nature of produced DOM, and long water residence time. Mon, 01 Jul 2019 00:00:00 GMT https://repository.kopri.re.kr/handle/201206/10509 2019-07-01T00:00:00Z https://repository.kopri.re.kr/handle/201206/10946 Title: Collection of large benthic invertebrates in sediment traps in the Amundsen Sea, Antarctica Authors: Kim, Minkyoung; Yang, Eun Jin; Kim, Hyung Jeek; Kim, Dongseon; Kim, Tae-Wan; La, HyoungSul; Lee, Sang Hoon; Hwang, Jeomshik Abstract: To study sinking particle sources and dynamics, sediment traps were deployed at three sites in the Amundsen Sea for 1 year from February？March 2012 and at one site from February 2016 to February 2018. Unexpectedly, large benthic invertebrates were found in three sediment traps deployed 130？567？m above the sea floor. The organisms included long and slender worms, a sea urchin, and juvenile scallops of varying sizes. This is the first reported collection of these benthic invertebrates in sediment traps. The collection of these organisms, predominantly during the austral winter, and their intact bodies suggests they were trapped in anchor ice, incorporated into the overlying sea ice, and subsequently transported by ice rafting. The observations imply that anchor ice forms episodically in the Amundsen Sea and has biological impacts on benthic ecosystems. An alternative hypothesis that these organisms spend their juvenile period underneath the sea ice and subsequently sink to the seafloor is also suggested. Mon, 01 Jul 2019 00:00:00 GMT https://repository.kopri.re.kr/handle/201206/10946 2019-07-01T00:00:00Z