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Articles by Tae Siek
EGUsphere - SPBM v2.0: Extension of a 1-D sea-ice biogeochemical model with ice-algal ecophysiology and zooplankton seasonal vertical migration for coupled ice-pelagic ecosystem simulations in Antarctic coastal seas
Status: this preprint is open for discussion and under review for Geoscientific Model Development (GMD). Status: open (until 11 Dec 2026) Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse Please provide a reason why you see this comment as being abusive. You might include your name and email but you can also stay anonymous. Please provide a reason why you see this comment as being abusive. Please confirm reCaptcha.
Potential impact of the sea-ice ecosystem to the polar seas biogeochemistry
1 Introduction Sea-ice, one of the largest biomes on Earth (Dieckmann and Hellmer, 2010), plays a significant role in the seasonal primary production of the polar oceans, particularly in the marginal sea-ice zone (Arrigo et al., 2010). Understanding the biology of sea-ice is essential due to the significant impact it has on these regions. Most of the regions covered by seasonal sea-ice are known to exhibit high productivity with intense, albeit brief, algal blooms (Thomas et al., 2012).
Potential impact of the sea-ice ecosystem to the Polar Seas biogeochemistry
Young Shin Kwon1, Tae Siek Rhee2* and Karsten Bolding3 1Korea Institute of Ocean Science and Technology (KIOST), Republic of Korea 2Korea Polar Research Institute, Republic of Korea 3Independent researcher, Italy The final, formatted version of the article will be published soon.
Identification of ventilated and submarine glacial meltwaters in the Amundsen Sea, Antarctica, using noble gases
1 Introduction Antarctic ice shelves lose 2400–2800 Gt of mass every year (Depoorter et al., 2013; Rignot et al., 2013). Ice calving, the falling down of ice chunks from the edge of a glacier, has long been considered an important process responsible for the loss of ice shelves (Jacobs et al., 1992; Depoorter et al., 2013). Along with ice calving, recent studies have suggested that basal melting, i.e., melting at depth by warm seawater, is equally responsible for the loss of ice shelves.
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