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        • AWI-Meereisphysikers arbeiten auch bei auffrischendem Wind und zunehmender Schneedrift auf dem Meereis.


Polarsternexpedition ANT-XXIX/6; 8. Juni - 12. August 2013; Kapstadt-Punta Arenas
Ziel der Expedition: Ein interdisziplinäres Forschungsprogramm in Atmosphäre, Meereis, Ozean und Ökosystem im antarktischen Winter, um die physikalischen und biogeochemischen Eigenschaften und Prozesse während der Wachstumsphase des Meereises besser zu verstehen. Fahrt war die erste antarktische Winterexpedition seit dem Jahr 2006. (Kurs wie im Winterexperiment 1992) 


English

AWI sea-ice physicists are working on the sea ice, while the wind is acclerating and the snow drift is increasing.

Polarsternexpedition ANT-XXIX/6; 8. June - 12. August 2013; Cape Town -Punta Arenas (Chile); The aim of the cruise is to carry out an interdisciplinary research programm on atmosphere, sea ice, ocean, and ecosystem during winter to obtain an understanding of physical and biogeochemical properties and processes during the sea ice growth season. It was the first Antarctic winter expedition since the year 2006.


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      Publications

      Crosta et al., 2022. Antarctic sea ice over the past 130.000 years – Part 1: a review of what proxy records tell us. Climate of the Past, 18, 1729–1756.

      Sánchez Montes et al., 2022. Plio-Pleistocene ocean circulation changes in the GOA and its impacts on the carbon and nitrogen cycles and the CIS development. Paleoceanography and Paleoclimatology, 37, e2021PA004341.

      Corella et al., 2022. Climate changes modulated the history of Arctic iodine during the Last Glacial Cycle. Nature Communications, v. 13, pp. 88.

      Romero et al., 2022. Orbital and Suborbital-Scale Variations of Productivity and Sea Surface Conditions in the Gulf of Alaska During the Past 54,000 Years: Impact of Iron Fertilization by Icebergs and Meltwater. Paleoceanography and Paleoclimatology 37, e2021PA004385.

      Lamping et al., 2021. Evaluation of lipid biomarkers as proxies for sea ice and ocean temperatures along the Antarctic continental margin. Climate of the Past 17, 2305-2326.

      Spencer-Jones et al., 2021. Archaeal intact polar lipids in polar waters: a comparison between the Amundsen and Scotia seas. Biogeosciences 18, 3485-3504.

      Zimmermann et al., 2020. Changes in the composition of marine and sea-ice diatoms derived from sedimentary ancient DNA of the eastern Fram Strait over the past 30 000 years. Ocean Science, v. 16, 1017–1032.

      Vorrath et al., 2020. Sea ice dynamics in the Bransfield Strait, Antarctic Peninsula, during the past 240 years: a multi-proxy intercomparison study. Climate of the Past, v. 16, 2459–2483.

      Cowan et al., 2020. Sediment controls dynamic behavior of a Cordilleran Ice Stream at the Last Glacial Maximum. Nature Communications, v. 11, no. 1, p. 1826.

      Klages et al., 2020. Temperate rainforests near the South Pole during peak Cretaceous warmth. Nature, v. 580, no. 7801, p. 81-86.

      Lamping et al., 2020. Highly branched isoprenoids reveal onset of deglaciation followed by dynamic sea-ice conditions in the western Amundsen Sea, Antarctica. Quaternary Science Reviews, v. 228, p. 106103.

      Allaart et al., 2020. Late Quaternary glacier and sea-ice history of northern Wijdefjorden, Svalbard. Boreas.

      Sánchez-Montes et al., 2020. Late Pliocene Cordilleran Ice Sheet development with warm Northeast Pacific sea surface temperatures. Clim. Past Discuss., v. 2020, p. 1-23.

      Thomas et al., 2019. Antarctic Sea Ice Proxies from Marine and Ice Core Archives Suitable for Reconstructing Sea Ice over the Past 2000 Years. Geosciences, v. 9, no. 12, p. 506.

      Corella et al., 2019. Holocene atmospheric iodine evolution over the North Atlantic. Clim. Past, v. 15, no. 6, p. 2019-2030.

      Vorrath et al., 2019. Highly branched isoprenoids for Southern Ocean sea ice reconstructions: a pilot study from the Western Antarctic Peninsula. Biogeosciences, v. 16, no. 15, p. 2961-2981.

      Cárdenas et al., 2019. Biogeochemical proxies and diatoms in surface sediments across the Drake Passage reflect oceanic domains and frontal systems in the region. Progress in Oceanography, v. 174, p. 72-88.

      Müller et al., 2018, Cordilleran ice-sheet growth fueled primary productivity in the Gulf of Alaska, northeast Pacific Ocean. Geology, v. 46, no. 4, p. 307-310.

      Last update: 25.08.2022
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