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Stadial interstadial

Ein Stadial bezeichnet eine Kältephase (in der Regel zugleich Eisvorstoß-Phase) innerhalb eines Glazials oder Interglazials und wird in der Fachliteratur oft mit dem Kürzel GS abgekürzt.. Die ca. 100.000 Jahre dauernden Glaziale und Interglaziale treten nie als kontinuierlicher, ununterbrochener Eisvorstoß oder -rückzug während einer stets gleich kalten oder warmen Klimaperiode auf. The odd-numbered interstadial MIS 5, also known as the Sangamonian interglacial, contains two periods of relative cooling, and so is subdivided into three interstadials (5a, 5c, 5e) and two stadials (5b, 5d). A stadial isotope stage like MIS 6 would be subdivided by periods of relative warming, and so in that case the first and last subdivisions would be stadials; MIS 6a, 6c and 6e are. Das Huneborg-Stadial folgt auf das Hengelo-Interstadial und wird seinerseits vom Denekamp-Interstadial überlagert. Es ereignete sich während des MIS 3 und korreliert mit den Dansgaard-Oeschger-Ereignissen DO10, das den Beginn des Stadials markiert, sowie DO9 und DO8.Zwischen DO9 und DO8 fällt das Heinrich-Ereignis H4.. Das Huneborg-Stadial ist keine durchgehende Kälteanomalie, es wird. Definition, Rechtschreibung, Synonyme und Grammatik von 'stadial' auf Duden online nachschlagen. Wörterbuch der deutschen Sprache

Stadial. Ein Stadial bezeichnet eine Kältephase (in der Regel zugleich Eisvorstoß-Phase) innerhalb eines Glazials oder Interglazials und wird in der Fachliteratur oft mit dem Kürzel GS abgekürzt.. Die ca. 100.000 Jahre dauernden Glaziale und Interglaziale treten nie als kontinuierlicher, ununterbrochener Eisvorstoß oder -rückzug während einer stets gleich kalten oder warmen Klimaperiode. sta | di | a l 〈 Adj. , o. Steig. 〉 abschnitts-, stufenweise [→ Stadium ].. Stadial und Akkumulation (Geowissenschaften) · Mehr sehen » Alleröd-Interstadial. Das Alleröd-Interstadial, auch Allerød-Interstadial oder Alleröd-Schwankung, ist die letzte Warmphase (Interstadial) kurz vor dem Ende der letzten Kaltzeit (Quartär). Neu!!: Stadial und Alleröd-Interstadial · Mehr sehen » Ältere Dryaszei The Younger Dryas (around 12,900 to 11,700 years BP) was a return to glacial conditions after the Late Glacial Interstadial, which temporarily reversed the gradual climatic warming after the Last Glacial Maximum (LGM) started receding around 20,000 BP. It is named after an indicator genus, the alpine-tundra wildflower Dryas octopetala, as its leaves are occasionally abundant in late glacial.

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Interglazial s [von *inter-, Glazial], (O. Heer 1865), Interglazialzeit, Zwischeneiszeit, Warmzeit, Wärmezwischenzeit, Warmzeit zwischen zwei Vereisungsperioden (Glazialen, Eiszeit), die durch wärmeliebende Organismen in Ablagerungen dieses Zeitraums gekennzeichnet ist.Infolge der Erkenntnis, daß es wesentlich mehr Warm- und Kaltzeiten gab als man früher annahm, sind auch die älteren. One major benefit of her erudition is to situate the Scottish debate on race and gender in a truly European intellectual context that includes not only the avowed favorite of the Scottish literati, Montesquieu, and other French thinkers who are commonly cited by Scottish Enlightenment scholars because of their prominence or their relevance for Scottish stadial theory, such as Rousseau. Interstadiál je částečně teplejší období v glaciálu.Mezi dvěma interstadiály starším a mladším probíhalo období studeného podnebí, stadiál.Interstadiál měl výrazně vyšší průměrnou teplotu než stadiál, ale v porovnaní s dneškem se vyznačoval nižšími teplotami Of or relating to discrete stages of development: stadial theories of history. n. A comparatively brief period of climatic cooling during an... n. A comparatively brief period of climatic cooling during an.. Interstadial. Interstadials kurze warme Perioden zwischen Stadials innerhalb einer Eiszeit sind. Am besten zu rekonstruieren, die Stadial und interstadials der letzten Eiszeit können sogenannte Würm-oder weichsel Eiszeit, als durch Ihre geologische Spuren sind besser erhalten als die des vorherigen ausprobieren

ABSTRACT This paper systematically reviews the glacial geomorphological evidence of the Loch Lomond Stadial (LLS; Younger Dryas) glaciation in Britain (12.9-11.7 ka). The geomorphology of sub‐regio..

  1. Das Huneborg-Stadial folgt auf das Hengelo-Interstadial und wird seinerseits vom Denekamp-Interstadial überlagert. Es ereignete sich während des MIS 3 und korreliert mit den Dansgaard-Oeschger-Ereignissen DO10, das den Beginn des Stadials markiert, sowie DO9 und DO8. Zwischen DO9 und DO8 fällt das Heinrich-Ereignis H4.. Das Huneborg-Stadial ist keine durchgehende Kälteanomalie, es wird.
  2. Michael Houmark-Nielsen, in Developments in Quaternary Sciences, 2004. The Late Weichselian. The Sandnes interstadial beds antedates the Late Weichselian glaciation in Denmark and during the Jylland stadial, glaciers reached their final and most extensive distribution. The ice stream reached the Polish coast slightly before 20 ka BP (Kozarski, 1988; Wysota, 1999)
  3. Stadial: | |Stadials| and |interstadials| are phases dividing the |Quaternary| period, the last... World Heritage Encyclopedia, the aggregation of the largest online encyclopedias available, and the most definitive collection ever assembled
  4. g at the onset of the present interglacial. Again, the Younger Dryas is a period whose fauna is largely known from radiocarbon dates on individual bones rather than from discrete assemblages. A site that would have been critical to a.
  5. stadial sta | di | a l 〈 Adjektiv 〉 abschnittweise, stufenweise [ → Stadium ]..

Stadial-interstadial transitions were most probably caused by changes in the strength of the thermohaline circulation in the North Atlantic Ocean 5. Further study of these climatic shifts and their impact on the envrionment is important, as this provides information on the response of the geo-system during phases of rapid climate change. We have used an atmospheric general circulation model. Marine Isotope Stages are sometimes further subdivided into stadials and interstadials by minor climate fluctuations within the overall stadial or interstadial regime, which are indicated by letters. The odd-numbered interstadial MIS 5 , also known as the Sangamonian interglacial, contains two periods of relative cooling, and so is subdivided into three interstadials (5a, 5c, 5 The term Dimlington Stadial is proposed as a climatostratigraphic name fer the main glacial episode of the Late Devensian in Britain, in preference to stratigraphically unsatisfactory terms, such as Late Devensian Glaciation (which includes the Windermere Interstadial and the Loch Lomond Stadial), icesheet glaciation or maximum of ice expansion, that are currently in use Ein Stadial bezeichnet eine Kältephase (in der Regel zugleich Eisvorstoß-Phase) innerhalb eines Glazials und wird in der Fachliteratur oft mit dem Kürzel GS abgekürzt.. Die ca. 100.000 Jahre dauernden Glaziale treten nie als kontinuierlicher, ununterbrochener Eisvorstoß während einer stets gleich kalten Klimaperiode auf, sondern als Perioden mit zwar langfristig (100.000 Jahre. The Loch Lomond Stadial came right at the end of the British-Irish Ice Sheet, during the Late Pleistocene. After a period known as the Windermere Interstadial, around 14,000 years ago, where the temperature was warmer, ice had retreated to ice caps mountainous regions. It is likely that some small ice caps survived the Windermere Interstadial 2

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Duden stadial Rechtschreibung, Bedeutung, Definition

Staatlich geprüfter und zugelassener Fernlehrgang inkl. drei Wochenendseminaren. Führen Sie erfolgreich Erziehungs- und Entwicklungsberatungen durch. Jetzt informieren (geology) Pertaining to a glacial stade.· (archaeology, sociology) Pertaining to or existing in successive stages of a given culture, society etc. 2002, Colin Jones, The Great Nation, Penguin 2003, p. 188: He drew on the growing ethnographic record contained in travellers' tales about extra-European societies to develop a stadial view of human. Interstadial definition: of a relatively warm period during a glacial epoch , when glaciers temporarily stop or... | Meaning, pronunciation, translations and example Definition of stadial in the Definitions.net dictionary. Meaning of stadial. What does stadial mean? Information and translations of stadial in the most comprehensive dictionary definitions resource on the web Stadiál je kratší studenější a sušší klimatické období v rámci jednoho glaciálu.Během jednoho glaciálu mohlo dojít k několika studenějším výkyvům - stadiálům, mezi kterými probíhaly teplejší období - interstadiály. Literatura. MIKULA, Jiří

Stadial - de.LinkFang.or

This environment-related article is part of the WikiProject Environment to improve Wikipedia's coverage of the environment.The aim is to write neutral and well-referenced articles on environment-related topics, as well as to ensure that environment articles are properly categorized. Read Wikipedia:Contributing FAQ and leave any messages at the project talk page The interstadial states are observed to have a characteristic {}sawtooth{} shape, indicating a gradual drift of the stable interstadial state toward the stable stadial state. In order to contrast the two climate states, we have separated the delta(18)O signal from the Greenland Icecore Project ice core into periods corresponding to the two states. The climate variability in the two different.

stadial Rechtschreibung - wie schreibt man stadial

What does interstadial mean? interstadial is defined by the lexicographers at Oxford Dictionaries as Relating to a minor period of less cold climate during a glacial period Das Maisières Interstadial, Französisch, Oszillation de Maisières, in der Archäologie als Maisièrien bezeichnet, nach dem eponymen archäologische open-Land archäologischen Stätte von Maisières-Canal bei Mons in Belgien, benannt. Der Standort befindet sich auf dem Canal du Centre, zwischen den Gemeinden von Maisières und Obourg

stadial definition: adjectiveOf or relating to discrete stages of development: stadial theories of history. nounA comparatively brief period of climatic cooling during an interglacial, often characterized by glacial advances.Origin of stadial stadi.. The fast climate fluctuations during the stadial and interstadial climate states PeterD. DITLEVSEN, 1SusanneDITLEVSEN,2KatrineK.ANDERSEN 1TheNielsBohrInstitute ,Department ofGeophysicsUniversity CopenhagenJulianeMariesVej30 DK-2100Copenhagen,Denmark E-mail:pditlev@gfy.ku.dk 2Department ofBiostatistics ,University Copenhagen,Blegdamsvej3DK-2200. Emeleus, C H, and Bell, B R. 2005. British regional geology: The Palaeogene volcanic districts of Scotland. Fourth edition. Keyworth, Nottingham: British Geological Survey. Contents. 1 Pre-Late Devensian glaciations; 2 Dimlington Stadial. 2.1 Main Late Devensian Glaciation; 3 Windermere Interstadial; 4 Loch Lomond Stadial; 5 References; Pre-Late Devensian glaciations . Glacially polished. Stadial definition is - of or relating to a stage, stadial, or stadium

Stadial - Unionpedi

Stadial: Kaltphase mit Gletschervorstoß innerhalb einer Eiszeit. Interstadial: Warmphase innerhalb einer Eiszeit. LGM: Das Last Glacial Maximum bezeichnet die Maximalausdehnung des Eises zur letzten Kaltzeit, bzw. die größte Eismasse oder auch den größten peak in den Isotopenkurve A stadial is a period of lower temperatures during an interglacial (warm period) separating the glacial periods of an ice age. Such periods are of insufficient duration or intensity to be considered glacial periods. Notable stadials include the Older Dryas and Younger Dryas stadials and the Little Ice Age. An interstadial is a warm period during a glacial period of an ice age that is of. The nature of MIS 3 stadial-interstadial transitions in Europe: New insights from model-data comparisons Article (PDF Available) in Quaternary Science Reviews 30:3618-3637 · December 2011 with. We compare reconstructed climatic and vegetation changes between a stadial and subsequent interstadial - correlated to GS15 and GI14 (∼55 ka BP) - with a simulated AMOC resumption using a three-dimensional earth system model setup with early-MIS 3 boundary conditions. Over western Europe (12°W-15°E), we simulate twice the annual precipitation, a 17 °C warmer coldest month, a 8 °C warmer.

Schalkholz-Stadial Odderade-Interstadial Redderstall-Stadial Herning-Stadial Brörup-Interstadial Fluviatil-(Nieder-terrassen-) Komplex O b e r e s W e i c h s e l Weichsel - Spätglazial W e i c h s e l - H o c h g l a z i a l U n t e r e s We i c h s e l Weichsel- Frühglazial Eem-Warmzeit Jüngeres Saale-Stadium (Warthe) Saale-Spätglazial J u n g p l e i s t o z ä n W e i c h s e l - K. Onset and duration of transitions into Greenland Interstadials 15.2 and 14 in northern China constrained by an annually laminated stalagmite Skip to main content Thank you for visiting nature.com

Younger Dryas - Wikipedi

11 Beziehungen: Alleröd-Interstadial, Ältere Dryaszeit, Dansgaard-Oeschger-Ereignis, Holozän, Jüngere Dryaszeit, Kaltzeit, Letzte Kaltzeit, Stadial, Warmzeit, Würm-Kaltzeit, Weichsel-Kaltzeit. Alleröd-Interstadial. Das Alleröd-Interstadial, auch Allerød-Interstadial oder Alleröd-Schwankung, ist die letzte Warmphase (Interstadial) kurz vor dem Ende der letzten Kaltzeit (Quartär) Otto Stadial and Gowanda Interstadial. Information compiled by Liesel Rickert and Chantel Abramowski 5/31/2012 for the Cattaraugus County Geology Trail. Stadial site in Otto. The stadial site in Otto is a place like no other. Otto is one of only two known places in New York to have preserved till layers from first three glacier movements (of four) during the Pleistocene Ice Age. Here you will. Interstadial sind kurzzeitige (relative) Warmperioden zwischen Stadialen (Eisvorstößen) innerhalb eines Glazials.. Am besten rekonstruieren lassen sich die Stadiale und Interstadiale des letzten, jüngsten Glazials (Würm-bzw.Weichselglazial), da ihre geologischen Spuren besser erhalten sind als die vorheriger Vereisungen.Innerhalb des Würm-/Weichsel-Glazialkomplexes werden zahlreiche. Ebersdorf-Stadial: 53.500 Oerel-Interstadial: 57.700 Weichsel ääder kuultidj: Schalkholz-Stadial: 60.000 Odderade-Interstadial: 74.000 Rederstall-Stadial? Brörup-Interstadial? Amersfoort-Interstadial? Herning-Stadial: 115.000 Eem waremtidj: 126.000 Futnuuten.

Interglazial - Lexikon der Biologi

as interstadial, because the overlying mo-raine was supposed to be not Wiirm-glacial but Biihl-stadial. Quite obviously, the or-ganic content of the coal had been consid-ered as of secondary importance. This is also expressed in Penck and Brtickner's volume 1 (p. 338), where the last interglacial lignites of Grossweil had unhesitatingly been desig Stadial B Stadial A Pritzwalk-Interstadial Holstein-Warmzeit Elster-Spätglazial Elster-Kaltzeit Oberes Elster Elster-Hochglazial? Altpleistozän 2. Elster-Eisvorstoß (Jüngeres Stadial) 1. Elster-Eisvorstoß (Älteres Stadial) Saale-Kaltzeit (-Komplex) Quartär Mittelpleistozän Unteres Elster Elster-Frühglazial Frühpleistozäne Kalt-/Warmzeiten-Komplexe Holstein-Komplex Berliner Elbelauf. Hengelo interstadial CATEGORY: chronology DEFINITION: A Continental Middle Pleniglacial interstadial of the Weichselian cold stage, starting around 39,000 BP. It occurred during the final glaciation between the Moershooft and Denekamp interstadials. Loch Lomond stadial SYNONYMS OR RELATED TERMS: Younger Dryas CATEGORY: chronolog Late-glacial mean July air temperature reconstruction (a) at Whitrig Bog, southeast Scotland (from Brooks & Birks, 2000a) compared to the GRIP oxygen isotope data (b). Abbreviations: H = Holocene, YD = Younger Dryas , IS = Interstadial, S = Stadial, GS = Greenland Stadial, GI = Greenland Interstadial

Stadial Article about Stadial by The Free Dictionar

Interstadial and stadial conditions over Reykjanes Ridge In nearly all D-O events, maximum temperature occurs in the early part of the interstadials ( Fig. 4g ) A stadial is a period of lower temperatures during an interglacial (warm period) separating the glacial periods of an ice age.Such periods are of insufficient duration or intensity to be considered glacial periods. Notable stadials include the Older Dryas and Younger Dryas stadials and the Little Ice Age.. An interstadial is a warm period during a glacial period of an ice age that is of. The most recent glaciation of the English Lake District occurred during the Loch Lomond Stadial (Younger Dryas) when full glacial conditions returned to the British Isles. The largest ice mass formed over the Western Scottish Highlands with smaller ice masses developing throughout the British uplands. In the Lake District, our understanding of the extent and timing of the Loch Lomond Stadial. Termination-II interstadial/stadial climate change recorded in two stalagmites from the north European Alps. Gina E. Moseley, Christoph Spötl, Hai Cheng, Ronny Boch, Angela Min, R. Lawrence Edwards. Earth Sciences; Research output: Contribution to journal › Article. 22 Scopus citations. Abstract. Understanding the sequence of events that take place during glacial-interglacial climate. Stadials and interstadials are phases dividing the Quaternary period, i.e., the last 2.6 million years. Stadials are colder periods and interstadials are warmer. Each phase has a Marine Isotope Stage (MIS) number, working backwards from the present, with stadial having even numbers and interstadials odd numbers. Thus the current Holocene is MIS1 and the Last glacial period is MIS2. Stages are.

Interstadiál - Wikipedi

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Interstadial - .. historische geologie .. Informationen ..

As adjectives the difference between interglacial and stadial is that interglacial is occurring between ice ages while stadial is (geology) pertaining to a glacial stade. As nouns the difference between interglacial and stadial is that interglacial is the relatively warm period between ice ages while stadial is (geology) a short, colder period within an interglacial; a stade The fast climate fluctuations during the stadial and interstadial climate states Article (PDF Available) in Annals of Glaciology 35(1):457-462 · January 2002 with 205 Reads How we measure 'reads

The glacial geomorphology of the Loch Lomond (Younger

WikiZero - Stadial

Erstbeschreibung und Typlokalitä

interstadials. This can be interpreted as synchronous change of high-latitude temperature and lower-latitude hydrological cycle (relative humidity at the oceanic source of evaporation or change in the water mass trajectory/recharge) and/or an influence of local temperature on 17O-excess through kinetic effect at snow formation. As an exception from this gen-eral pattern, stadial 9 consists of. Windermere Interstadial and Loch Lomond Stadial Deglaciation of the Firth of Clyde area was followed by the deposition of the Clyde Beds , which began to form about 13 000 to 12 800 BP, when glaciers finally retreated to within the mouths of the sea lochs in response to the sharp climatic amelioration marking the beginning of the Windermere Interstadial (Sutherland, 1984)

Abrupt warming events drove Late Pleistocene Holarctic

Solar radiation varies smoothly through time (top, orange line) with a strong cyclicity of ~23,000 years, as seen in this time series of July incoming solar radiation at 65°N (Berger and Loutre 1991).In contrast, glacial-interglacial cycles last ~100,000 years (middle, black line) and consist of stepwise cooling events followed by rapid warmings, as seen in this time series inferred from. 15 abrupt warming transitions perturbed glacial climate in Greenland during Marine Isotope Stage 3 (MIS 3, 60-27 ka BP). One hypothesis states that the 8-16° C warming between Greenland Stadials (GS) and Interstadials (GI) was caused by enhanced hea H. Renssen Æ P.W. Bogaart Atmospheric variability over the 14.7 kyr BP stadial-interstadial transition in the North Atlantic region as simulated by an AGCM Received: 7 December 2001 /Accepted: 14 June 2002 / Published online: 5 September 2002 Springer-Verlag 2002 Abstract The ECHAM4-T42 atmospheric general cir- culation model was applied to study the change in at-mospheric variability in the. Environmental records in permafrost of East Siberian Arctic during the MIS2 Stadial and the MIS3 Interstadial . By Natalia Rudaya, Andreev Andreev, Sebastian Wetterich, Vladimir Tumskoy and Lutz Schirrmeister. Abstract. In East Siberian Arctic permafrost deposits is increasingly employed as an archive that preserves records of regional environmental history. Pollen records play a leading role.

Rederstall-Stadial (auch WF III). In Norddeutschland weisen die Pollenspektren auf eine Grastundra mit später folgender Strauchtundra hin. das Brörup-Interstadial (auch WF II). In einigen Profilen findet kurz nach dem Beginn des Brörup-Interstadials eine kurze Abkühlungsphase, die aber nicht in allen Profilen nachweisbar ist. Dies. interstadial-El Abra stadial-early Holocene sequence is radiocarbon dated by some 45 dates and evidence is shown from 14 areas, mostly located at high elevations (2000-4000 m) in the Eastern and Central Cordillera and in the Sierra Nevada de Santa Marta, but some from the tropical low- lands. Although more precise dating of the boundaries is desirable, we interpret the Guantiva-El Abra. Correction to Arsenic in a Speleothem from Central China: Stadial-Interstadial Variations and Implications Environmental Science & Technology DOI: 10.1021/es201158h Autoren Glazial-Interglaziale Klimaschwankungen. Die Erde hat in den letzten 1,8 Millionen Jahren glaziale Zyklen durchlaufen, die durch ihre sich periodisch verändernde Umlaufbahn um die Sonne bestimmt sind

Devensian, Quaternary, Midland Valley of Scotland - Earthwise

Stadiale sind Kaltphasen mit deutlichem Gletschervorstoß, und Interstadiale sind klimatisch mildere Zeiten mit zeitweisem Rückschmelzen der Gletscher. Während der Stadiale war weltweit das Eisvolumen mehr als 2,5 mal größer als heute, und die eisbedeckte Fläche vergrößerte sich auf ca. 55 Mio. km 2 gegenüber derzeit 15 Mio. km 2 The Kargin Interstadial optimum between 48.5 and 37 kyr BP promoted low-centered polygon tundra with shallow water in polygon centers. Moister conditions in the landscape than during the previous Zyryan Stadial are assumed while the general summer climate conditions likely remained dry, but slightly warmer as reflected by higher Salix abundances. Warmer summer air temperatures and moister.

Early Midlandian–Middle Midlandian, Pleistocene, NorthernHas the puzzle of rapid climate change in the last ice ageThe effect of millennial-scale changes in Arabian Sea

Interstadiale sind kurzzeitige (relative) Warmperioden zwischen Stadialen (Eisvorstößen) innerhalb eines Glazials.. Am besten rekonstruieren lassen sich die Stadiale und Interstadiale des letzten Glazials (Würm-bzw. Weichselglazial), da ihre geologischen Spuren besser erhalten sind als die vorheriger Vereisungen.Innerhalb des Würm-/Weichsel-Glazialkomplexes werden zahlreiche Stadiale und. interstadial definition: of a relatively warm period during a glacial epoch, when glaciers temporarily stop or retreat..

Links between salinity variation in the Caribbean andHuman DNA - WikiversityJüngere Dryaszeit – WikipediaDFG Projekt - Löss in Zentralspanien — Professur fürPPT - Introduction to Quaternary Palaeoecology PowerPoint

zwischen Drenthe- und Warthe-Stadial in Norddeutschland Von ERWIN KOPP und PAUL WOLDSTEDT, Bonn Mit 4 Abbildungen im Text Zusammenfassung : Zwischen Saale- und Warthe-Stadial liegt keine echte Interglazial- zeit, sondern ein Abschnitt, in dem es zwar zu einer Wiederbewaldung kam, aber nur mit Nadel­ bäumen, nicht mit wärmeliebendem Laubwald. Es fand wohl im Norden eine früh-interstadiale. What's the plural form of stadial? Here's the word you're looking for 11 500 - 13 000 Loch Lomond stadial Younger Dryas stadial cold, glacial re-advance 13 000 - 15 000 Windermere interstadial Allerød interstadial Older Dryas Bølling interstadial moderately warm a brief cool interval warm 15 000 - 18 000 Devensian glaciation Oldest Dryas cold Before 18 000 Devensian glaciation Weichselian glaciation glacial The potential causes of the succession of glacial. Early-Warning Signals for the onsets of Greenland Interstadials and the Younger Dryas-Preboreal transition Martin Rypdal Department of Mathematics and Statistics, UiT The Arctic University of Norway, Norway ABSTRACT The high-frequency band of the 18O variations in the North Greenland Ice Core Project displays uctuation levels that increase as one approaches the onset of an interstadial (warm. The climate over the last glacial period was characterized by a series of abrupt, millennial-scale climate oscillations known as Dansgaard-Oeschger (DO) events, marked by a rapid warming followed by a slow cooling, referred to as Greenland Interstadial (GIS) and Greenland Stadial (GS) 1,2.These rapid climate swings in polar climate associated with transitions between extreme conditions provide.

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