Relevant bibliographies by topics / Atlantification

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Atlantification'

Author: Grafiati
Published: 25 May 2024
Last updated: 31 July 2025

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Journal articles on the topic "Atlantification"

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Polyakov, Igor V., Randi B. Ingvaldsen, Andrey V. Pnyushkov, et al. "Fluctuating Atlantic inflows modulate Arctic atlantification." Science 381, no. 6661 (2023): 972–79. http://dx.doi.org/10.1126/science.adh5158.

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Enhanced warm, salty subarctic inflows drive high-latitude atlantification, which weakens oceanic stratification, amplifies heat fluxes, and reduces sea ice. In this work, we show that the atmospheric Arctic Dipole (AD) associated with anticyclonic winds over North America and cyclonic winds over Eurasia modulates inflows from the North Atlantic across the Nordic Seas. The alternating AD phases create a “switchgear mechanism.” From 2007 to 2021, this switchgear mechanism weakened northward inflows and enhanced sea-ice export across Fram Strait and increased inflows throughout the Barents Sea.
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Kujawa, Agnieszka, Magdalena Łącka, Natalia Szymańska, Joanna Pawłowska, Maciej M. Telesiński, and Marek Zajączkowski. "Could Norwegian fjords serve as an analogue for the future of the Svalbard fjords? State and fate of high latitude fjords in the face of progressive “atlantification”." Polar Biology 44, no. 12 (2021): 2217–33. http://dx.doi.org/10.1007/s00300-021-02951-z.

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AbstractBenthic foraminifera are one of the most widely and abundantly distributed organisms in the fjords of Svalbard and Norway. Due to their short life span and quick reactivity to environmental changes they can be used as indicators of the “atlantification” process. Here, we compare the benthic foraminifera assemblages along the latitudinal gradient, from the fjords of northern Svalbard to southern Norway to assess whether the “atlantification” process may homogenise the foraminiferal assemblages in terms of their abundance and species composition. Furthermore, the previously published dat
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Ingvaldsen, Randi B., Karen M. Assmann, Raul Primicerio, Maria Fossheim, Igor V. Polyakov, and Andrey V. Dolgov. "Physical manifestations and ecological implications of Arctic Atlantification." Nature Reviews Earth & Environment 2, no. 12 (2021): 874–89. http://dx.doi.org/10.1038/s43017-021-00228-x.

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Blum, Hester. "Atlantification: Facing the Atlantic from the Arctic – a provocation." Atlantic Studies 21, no. 1 (2024): 192–94. http://dx.doi.org/10.1080/14788810.2023.2287277.

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Aksenov, P. V., and V. V. Ivanov. "“Atlantification” as a Possible Cause for Reducing of the Sea-Ice Cover in the Nansen Basin in winter." Arctic and Antarctic Research 64, no. 1 (2018): 42–54. http://dx.doi.org/10.30758/0555-2648-2018-64-1-42-54.

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The paper presents arguments in favor of an explanation of the reduction of the ice-covered area in the Nansen basin of the Arctic Ocean (AO) in winter by the so-called “atlantification “ — the strengthening of the influence of waters of Atlantic origin on the hydrological regime of the Arctic Ocean. We hypothesize that the main agent of “atlantification” in theWesternNansenBasinis winter thermal convection, which delivers heat from the deep to the upper mixed layer, thus melting sea ice and warming the near-surface air. To check up this hypothesis we used ocean reanalysis MERCATOR data for ti
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Weydmann-Zwolicka, Agata, Paula Prątnicka, Magdalena Łącka, Sanna Majaneva, Finlo Cottier, and Jørgen Berge. "Zooplankton and sediment fluxes in two contrasting fjords reveal Atlantification of the Arctic." Science of The Total Environment 773 (June 2021): 145599. http://dx.doi.org/10.1016/j.scitotenv.2021.145599.

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Belter, H. Jakob, Thomas Krumpen, Luisa von Albedyll, et al. "Interannual variability in Transpolar Drift summer sea ice thickness and potential impact of Atlantification." Cryosphere 15, no. 6 (2021): 2575–91. http://dx.doi.org/10.5194/tc-15-2575-2021.

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Abstract. Changes in Arctic sea ice thickness are the result of complex interactions of the dynamic and variable ice cover with atmosphere and ocean. Most of the sea ice exiting the Arctic Ocean does so through Fram Strait, which is why long-term measurements of ice thickness at the end of the Transpolar Drift provide insight into the integrated signals of thermodynamic and dynamic influences along the pathways of Arctic sea ice. We present an updated summer (July–August) time series of extensive ice thickness surveys carried out at the end of the Transpolar Drift between 2001 and 2020. Overal
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Ahme, Antonia, Anabel Von Jackowski, Rebecca A. McPherson, et al. "Winners and Losers of Atlantification: The Degree of Ocean Warming Affects the Structure of Arctic Microbial Communities." Genes 14, no. 3 (2023): 623. http://dx.doi.org/10.3390/genes14030623.

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Arctic microbial communities (i.e., protists and bacteria) are increasingly subjected to an intrusion of new species via Atlantification and an uncertain degree of ocean warming. As species differ in adaptive traits, these oceanic conditions may lead to compositional changes with functional implications for the ecosystem. In June 2021, we incubated water from the western Fram Strait at three temperatures (2 °C, 6 °C, and 9 °C), mimicking the current and potential future properties of the Arctic Ocean. Our results show that increasing the temperature to 6 °C only minorly affects the community,
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Schiaparelli, Stefano, Maria Chiara Alvaro, Alice Guzzi, and Marco Grillo. "Cymbulia parvidentata Pelseneer, 1888 (Mollusca, Cymbuliidae) in the Ligurian Sea: further evidence of Atlantic species incursions in the Mediterranean area." Biodiversity Data Journal 11 (February 21, 2023): e99108. https://doi.org/10.3897/BDJ.11.e99108.

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We report the first record of a stranded specimen of <i>Cymbulia parvidentata</i>, a pteropod species of Atlantic origin, in the Ligurian Sea. On 27 February 2022, six <i>C. peronii</i> and one <i>C. parvidentata</i> were collected on Borgio-Verezzi Beach (Savona, Italy - 44.16° N, 8.304633° W). Specimens were examined morphologically and biometrically. Measurements (length, width, height and wet weight) separated the two taxa, <i>C. peronii</i> being larger than <i>C. parvidentata</i>. The finding of <i>C. parvidentata</i>, which has only occasionally been reported in southern Italy, is remar
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Freer, Jennifer J., Malin Daase, and Geraint A. Tarling. "Modelling the biogeographic boundary shift of Calanus finmarchicus reveals drivers of Arctic Atlantification by subarctic zooplankton." Global Change Biology 28, no. 2 (2021): 429–40. http://dx.doi.org/10.1111/gcb.15937.

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Dissertations / Theses on the topic "Atlantification"

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Bertosio, Cécilia. "On the evolution of the halocline in the upper Arctic Ocean since 2007." Electronic Thesis or Diss., Sorbonne université, 2021. http://www.theses.fr/2021SORUS423.

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Dans l'océan Arctique, la stratification est déterminée par la salinité, contrairement aux océans des latitudes moyennes qui sont stratifiés par la température. En d'autres termes, en Arctique, les eaux salées se retrouvent au fond, même si elles sont plus chaudes. La halocline de l'océan Arctique correspond à une couche épaisse de 100-200m avec de forts gradients verticaux de salinité et est située entre 100 et 350m de profondeur. Elle s'insère entre la glace de mer située en surface et la couche relativement chaude des eaux Atlantiques. La halocline isole ainsi la glace du réservoir de chale
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Book chapters on the topic "Atlantification"

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Blum, Hester. "Atlantification: Facing the Atlantic from the Arctic – A provocation." In Charting the Future. Routledge, 2025. https://doi.org/10.4324/9781003644040-10.

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Lein, A. Yu, M. D. Kravchishina, G. A. Pavlova, et al. "Salt composition and biogenic elements in modern pore waters of the Barents Sea (1997–2019)." In THE BARENTS SEA SYSTEM. Shirshov Institute of Oceanology Publishing House, 2021. http://dx.doi.org/10.29006/978-5-6045110-0-8/(28).

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The data (Cl-, SO42-, Ca2+ Alk and biogenic elements) on the salt composition of pore water and the isotopic organic carbon composition of suspended particulate matter, fluffy layer and surface layers (0–30 cm) of bottom sediments in the Barents and Norwegian seas are discussed during the period of the supposed maximum warming in the Arctic region in the 21st century associated with the “atlantification” of the Arctic Ocean.
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Pautova, L. A. "Phytoplankton of the Вarents sea." In THE BARENTS SEA SYSTEM. Shirshov Institute of Oceanology Publishing House, 2021. http://dx.doi.org/10.29006/978-5-6045110-0-8/(25).

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On the basis of the analysis of summer plankton phytocenosis structure, 4 areas representing various stages of a succession cycle are allocated for water areas of the Barents Sea. In the most productive places of the water area the level of phytoplankton growth corresponded to indicators of mesotrophic-eutrophic waters and was maximum in the northern area. Concentration of phosphates was the main regulator of bloom of coccolithophore Emilianiahuxleyi, besides water temperature. The presence in the modern plankton phytoсenosis structure in the northern part of sea (80ºN) of the Atlantic species
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Conference papers on the topic "Atlantification"

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Bensi, Manuel, Helene Olsen, Vedrana Kovačević, Patrizia Giordano, and Leonardo Langone. "A Multi-Platform Approach to Investigate the Signals of Atlantification in the Arctic." In 2024 IEEE International Workshop on Metrology for the Sea; Learning to Measure Sea Health Parameters (MetroSea). IEEE, 2024. https://doi.org/10.1109/metrosea62823.2024.10765745.

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Journal articles
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