Academic literature on the topic 'Past interglacials'

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Journal articles on the topic "Past interglacials"

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Cluett, Allison A., and Elizabeth K. Thomas. "Summer warmth of the past six interglacials on Greenland." Proceedings of the National Academy of Sciences 118, no. 20 (2021): e2022916118. http://dx.doi.org/10.1073/pnas.2022916118.

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The relative warmth of mid-to-late Pleistocene interglacials on Greenland has remained unknown, leading to debates about the regional climate forcing that caused past retreat of the Greenland Ice Sheet (GrIS). We analyze the hydrogen isotopic composition of terrestrial biomarkers in Labrador Sea sediments through interglacials of the past 600,000 y to infer millennial-scale summer warmth on southern Greenland. Here, we reconstruct exceptionally warm summers in Marine Isotope Stage (MIS) 5e, concurrent with strong Northern Hemisphere summer insolation. In contrast, “superinterglacial” MIS11 dem
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Bridgland, David. "The Climate of Past Interglacials." Quaternary Science Reviews 29, no. 15-16 (2010): 1952–53. http://dx.doi.org/10.1016/j.quascirev.2010.04.008.

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Coletti, A. J., R. M. DeConto, J. Brigham-Grette, and M. Melles. "A GCM comparison of Pleistocene super-interglacial periods in relation to Lake El'gygytgyn, NE Arctic Russia." Climate of the Past 11, no. 7 (2015): 979–89. http://dx.doi.org/10.5194/cp-11-979-2015.

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Abstract. Until now, the lack of time-continuous, terrestrial paleoenvironmental data from the Pleistocene Arctic has made model simulations of past interglacials difficult to assess. Here, we compare climate simulations of four warm interglacials at Marine Isotope Stages (MISs) 1 (9 ka), 5e (127 ka), 11c (409 ka) and 31 (1072 ka) with new proxy climate data recovered from Lake El'gygytgyn, NE Russia. Climate reconstructions of the mean temperature of the warmest month (MTWM) indicate conditions up to 0.4, 2.1, 0.5 and 3.1 °C warmer than today during MIS 1, 5e, 11c and 31, respectively. While
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Schreve, Danielle. "All is flux: the predictive power of fluctuating Quaternary mammalian faunal-climate scenarios." Philosophical Transactions of the Royal Society B: Biological Sciences 374, no. 1788 (2019): 20190213. http://dx.doi.org/10.1098/rstb.2019.0213.

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The long-term impact of Middle and Late Pleistocene glacial-interglacial change led to the major reorganization of mammalian faunal communities in northern Europe through species origination, extinction, evolutionary change and distributional shifts. A Bray–Curtis cluster analysis with single linkage to examine relative faunal similarity was performed on mammalian assemblages from five successively older interglacials (MIS 1, 5e, 7c-a, 9 and 11) in Britain, a region with an exceptionally well-resolved faunal record for this time period. The results indicate a degree of continuity in terms of c
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McManus, Jerry, D. Raynaud, and PC Tzedakis. "The 3rd PAGES Past Interglacials workshop." PAGES news 19, no. 2 (2011): 80–81. http://dx.doi.org/10.22498/pages.19.2.80.

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Tzedakis, Polychronis C., JF McManus, D. Raynaud, DA Hodell, LC Skinner, and EW Wolff. "The 4th PAGES past interglacials workshop." PAGES news 21, no. 1 (2013): 42. http://dx.doi.org/10.22498/pages.21.1.42.

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Jiang, Zhiyi, Chris Brierley, David Thornalley, and Sophie Sax. "No changes in overall AMOC strength in interglacial PMIP4 time slices." Climate of the Past 19, no. 1 (2023): 107–21. http://dx.doi.org/10.5194/cp-19-107-2023.

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Abstract. The Atlantic Meridional Overturning Circulation (AMOC) is a key mechanism of poleward heat transport and an important part of the global climate system. How it responded to past changes in forcing, such as those experienced during Quaternary interglacials, is an intriguing and open question. Previous modelling studies suggest an enhanced AMOC in the mid-Holocene compared to the preindustrial period. In earlier simulations from the Palaeoclimate Modelling Intercomparison Project (PMIP), this arose from feedbacks between sea ice and AMOC changes, which were dependent on resolution. Her
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Galaasen, Eirik Vinje, Ulysses S. Ninnemann, Augustin Kessler, et al. "Interglacial instability of North Atlantic Deep Water ventilation." Science 367, no. 6485 (2020): 1485–89. http://dx.doi.org/10.1126/science.aay6381.

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Disrupting North Atlantic Deep Water (NADW) ventilation is a key concern in climate projections. We use (sub)centennially resolved bottom water δ13C records that span the interglacials of the last 0.5 million years to assess the frequency of and the climatic backgrounds capable of triggering large NADW reductions. Episodes of reduced NADW in the deep Atlantic, similar in magnitude to glacial events, have been relatively common and occasionally long-lasting features of interglacials. NADW reductions were triggered across the range of recent interglacial climate backgrounds, which demonstrates t
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Tzedakis, Chronis, D. Raynaud, and JF McManus. "The 2nd PAGES past interglacials (PIGS) workshop." PAGES news 18, no. 1 (2010): 38–39. http://dx.doi.org/10.22498/pages.18.1.38.

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Coletti, A. J., R. M. DeConto, J. Brigham-Grette, and M. Melles. "A GCM comparison of Plio–Pleistocene interglacial–glacial periods in relation to Lake El'gygytgyn, NE Arctic Russia." Climate of the Past Discussions 10, no. 4 (2014): 3127–61. http://dx.doi.org/10.5194/cpd-10-3127-2014.

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Abstract. Until now, the lack of time-continuous, terrestrial paleoenvironmental data from the Pleistocene Arctic has made model simulations of past interglacials difficult to assess. Here, we compare climate simulations of four warm interglacials at Marine Isotope Stage (MIS) 1 (9 ka), 5e (127 ka), 11c (409 ka), and 31 (1072 ka) with new proxy climate data recovered from Lake El'gygytgyn, NE Russia. Climate reconstructions of the Mean Temperature of the Warmest Month (MTWM) indicate conditions 2.1, 0.5 and 3.1 °C warmer than today during MIS 5e, 11c, and 31, respectively. While the climate mo
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Dissertations / Theses on the topic "Past interglacials"

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Torner, Perez Judit. "Paleoclimatic reconstruction of past interglacial periods and their transitions in the Iberian Peninsula and its surrounding seas = Reconstruccions paleoclimàtiques dels interglacials recents i les seves transicions a la Península Ibèrica i mars circumdants." Doctoral thesis, Universitat de Barcelona, 2020. http://hdl.handle.net/10803/672465.

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This study combines cave speleothems and marine sediments to gain an insight into the climate variability of the Iberian Peninsula (IP) and its surrounding seas associated with previous warm interglacial periods. In particular, it centres in the interglacials comprised within the Marine Isotopic Stages (MIS) 13, 11, 9, 7, and 5, and their associated transitions. The speleothems are used as archives for changes in atmospheric moisture availability by means of stable isotopes and Mg/Ca analysis. The studied speleothems correspond mostly from the Balearic Islands (Minorca and Mallorca) but also f
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Rioual, Patrick. "Diatom assemblages and water chemistry of lakes in the French Massif Central : a methodology for reconstruction of past limnological and climate fluctuations during the Eemian period." Thesis, University College London (University of London), 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.326170.

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Ullermann, Johannes [Verfasser], Frank [Akademischer Betreuer] Lamy, Ralf [Akademischer Betreuer] Tiedemann, and Gesine [Akademischer Betreuer] Mollenhauer. "Glacial-interglacial oceanic changes in the central Pacific sector of the Southern Ocean during the past 500 ka / Johannes Ullermann. Betreuer: Frank Lamy. Gutachter: Ralf Tiedemann ; Gesine Mollenhauer." Bremen : Staats- und Universitätsbibliothek Bremen, 2015. http://d-nb.info/1079652353/34.

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Toti, Francesco. "A Mediterranean perspective on the Early-Middle Pleistocene transition with emphasis on marine isotope stage 19." Doctoral thesis, 2018. http://hdl.handle.net/2158/1124617.

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In this thesis, we discuss pollen and dinocysts data from the western and central Mediterranean to reconstruct vegetation and climate during the Early-Middle Pleistocene transition, with emphasis on MIS 19, i.e. the best analogue of the present interglacial.
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WILSON, CHERYL R. "A lacustrine sediment record of the last three interglacial periods from Clyde Foreland, Baffin Island, Nunavut: biological indicators from the past 200,000 years." Thesis, 2009. http://hdl.handle.net/1974/1872.

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The study of long-term climatic change in the Arctic, a region both particularly sensitive to the effects of a warming climate and an important driver of global climate, is pertinent to understanding the rates and magnitude of current ecosystem changes. Analyses on geological time frames provide insight into the variability of Arctic climate, allowing a contextualized understanding of recent ecosystem changes that have been documented across the Arctic. Lake CF8, a mid-Arctic lake on Clyde Foreland, Baffin Island, contains a unique sedimentary archive of the present and last two interglacial
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Books on the topic "Past interglacials"

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Frank, Sirocko, ed. The climate of past interglacials. Elsevier, 2007.

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Litt, T., F. Sirocko, M. Claussen, and M. F. Sanchez-Goni. Climate of Past Interglacials. Elsevier Science & Technology Books, 2006.

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The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)x8024-2.

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(Editor), F. Sirocko, M. Claussen (Editor), T. Litt (Editor), and M. F. Sanchez-Goni (Editor), eds. The Climate of Past Interglacials, Volume 7 (Developments in Quaternary Sciences) (Developments in Quaternary Sciences). Elsevier Science, 2007.

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Lézine, Anne-Marie. Vegetation at the Time of the African Humid Period. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.530.

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An orbitally induced increase in summer insolation during the last glacial-interglacial transition enhanced the thermal contrast between land and sea, with land masses heating up compared to the adjacent ocean surface. In North Africa, warmer land surfaces created a low-pressure zone, driving the northward penetration of monsoonal rains originating from the Atlantic Ocean. As a consequence, regions today among the driest of the world were covered by permanent and deep freshwater lakes, some of them being exceptionally large, such as the “Mega” Lake Chad, which covered some 400 000 square kilom
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Book chapters on the topic "Past interglacials"

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Rapp, Donald. "Overview of the various models for ice ages in the recent past (3 MYBP to present)." In Ice Ages and Interglacials. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30029-5_8.

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Gómez-Navarro, Juan Jose, Johannes P. Werner, Sebastian Wagner, Eduardo Zorita, and Jürg Luterbacher. "Precipitation in the Past Millennium in Europe—Extension to Roman Times." In Integrated Analysis of Interglacial Climate Dynamics (INTERDYNAMIC). Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-00693-2_22.

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Petit-Maire, N. "Interglacial Environments in Presently Hyperarid Sahara : Palaeoclimatic Implications." In Paleoclimatology and Paleometeorology: Modern and Past Patterns of Global Atmospheric Transport. Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0995-3_27.

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Berger, A., M. F. Loutre, F. Kaspar, and S. J. Lorenz. "2. Insolation during interglacial." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80027-3.

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Kiefer, Thorsten, and Christoph Kull. "Preface: Climates of Past Interglacials — a PAGES Perspective." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80024-8.

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"Acknowledgements." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80025-x.

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Claussen, Martin. "1. Introduction to climate forcing and climate feedbacks." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80026-1.

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Claussen, Martin, André Berger, and Hermann Held. "3. A survey of hypotheses for the 100-kyr cycle." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80028-5.

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Berger, André, and Marie-France Loutre. "4. Modelling the 100-kyr cycle — an example from LLN EMICs." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80029-7.

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Sirocko, Frank. "5. Introduction — palaeoclimate reconstructions and dating." In The Climate of Past Interglacials. Elsevier, 2007. http://dx.doi.org/10.1016/s1571-0866(07)80030-3.

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Conference papers on the topic "Past interglacials"

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Feng, Dong. "Enhanced marine methane seepage during past interglacials: Evidence from the South China Sea." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.9299.

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Blanchet, Cecile, Anne Osborne, Rik Tjallingii, et al. "Erosion dynamics in semi-arid areas of the Mediterranean Sea during past interglacials." In Goldschmidt2021. European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.5697.

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Rouyer, L., A. Govin, I. Bouloubassi, et al. "Reconstruction of Past Environmental Variations in the Semi-Arid Brazilian Nordeste Through Last Interglacials." In 30th International Meeting on Organic Geochemistry (IMOG 2021). European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202134367.

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Yamamoto, Masanobu, Sohei Kikuchi, Samantha Bova, and Yair Rosenthal. "Drier climates in Papua New Guinea during interglacials over the past 1.68 million years." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10041.

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Lindborg, Tobias, Ulrik Kautsky, and Lars Brydsten. "Landscape Modeling for Dose Calculations in the Safety Assessment of a Repository for Spent Nuclear Fuel." In The 11th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2007. http://dx.doi.org/10.1115/icem2007-7115.

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The Swedish Nuclear Fuel and Waste Management Co., (SKB), pursues site investigations for the final repository for spent nuclear fuel at two sites in the south eastern part of Sweden, the Forsmark- and the Laxemar site (figure 1). Data from the two site investigations are used to build site descriptive models of the areas. These models describe the bedrock and surface system properties important for designing the repository, the environmental impact assessment, and the long-term safety, i.e. up to 100,000 years, in a safety assessment. In this paper we discuss the methodology, and the interim
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