40. Chronology and climate forcing of the last four interglacials

Frank Sirocko; Martin Claussen; Thomas Litt; Maria Fernanda Sánchez Goñi; Andre Berger; Tatjana Boettger; Markus Diehl; Stéphanie Desprat; Barbara Delmonte; Detlev Degering; Manfred Frechen; Mebus A. Geyh; Matthias Groeger; Masa Kageyama; Frank Kaspar; Norbert Kühl; Claudia Kubatzki; Gerrit Lohmann; Marie France Loutre; Ulrich Müller; Bert Rein; Wilfried Rosendahl; Katy Roucoux; Denis Didier Rousseau; Klemens Seelos; Mark Siddall; Denis Scholz; Christoph Spötl; Brigitte Urban; Maryline Vautravers; Andrei Velichko; Stefan Wenzel; Martin Widmann; Bernd Wünnemann

doi:10.1016/S1571-0866(07)80065-0

40. Chronology and climate forcing of the last four interglacials

Frank Sirocko
, Martin Claussen
, Thomas Litt
, Maria Fernanda Sánchez Goñi
, Andre Berger
, Tatjana Boettger
, Markus Diehl
, Stéphanie Desprat
, Barbara Delmonte
, Detlev Degering
, Manfred Frechen
, Mebus A. Geyh
, Matthias Groeger
, Masa Kageyama
, Frank Kaspar
, Norbert Kühl
, Claudia Kubatzki
, Gerrit Lohmann
, Marie France Loutre
, Ulrich Müller

Bert Rein, Wilfried Rosendahl, Katy Roucoux, Denis Didier Rousseau, Klemens Seelos, Mark Siddall, Denis Scholz, Christoph Spötl, Brigitte Urban, Maryline Vautravers, Andrei Velichko, Stefan Wenzel, Martin Widmann, Bernd Wünnemann

Publikation: Beiträge in Zeitschriften › Konferenzaufsätze in Fachzeitschriften › Forschung › Begutachtung

10 Zitate (Scopus)

Abstract

The last four interglacials (intervals during which global ice volume was similar to, or less than, that of our current warm stage) correspond to the warmest parts of the marine oxygen isotope stages MIS 5, 7, 9, 11. These interglacials ffollowed the 100-kyr rhythm of eccentricity, but each had different insolation regimes, different durations, different ice volumes and different sea-level heights, bur atmospheric greenhouse gas concentrations were similar and reached values which, by and large, were close to those of the current interglacial (Holocene or MIS1) before the industrial revolution led to the artificial enrichment of the atmosphere's greenhouse gas concentrations via the burning of fossil fuels ...

Originalsprache	Englisch
Zeitschrift	Developments in Quaternary Science
Jahrgang	7
Ausgabenummer	C
Seiten (von - bis)	597-614
Seitenumfang	18
ISSN	1571-0866
DOIs	https://doi.org/10.1016/S1571-0866(07)80065-0
Publikationsstatus	Erschienen - 01.01.2007

UN SDGs

Dieser Output leistet einen Beitrag zu folgendem(n) Ziel(en) für nachhaltige Entwicklung

SDG 13 – Klimaschutzmaßnahmen
SDG 14 – Lebensraum Wasser

Fachgebiete und Schlagwörter

Umweltplanung, Landschaftsentwicklung

ASJC Scopus Sachgebiete

Erdoberflächenprozesse
Geologie

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10.1016/S1571-0866(07)80065-0

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Sirocko, F., Claussen, M., Litt, T., Fernanda Sánchez Goñi, M., Berger, A., Boettger, T., Diehl, M., Desprat, S., Delmonte, B., Degering, D., Frechen, M., A. Geyh, M., Groeger, M., Kageyama, M., Kaspar, F., Kühl, N., Kubatzki, C., Lohmann, G., Loutre, M. F., ... Wünnemann, B. (2007). 40. Chronology and climate forcing of the last four interglacials. Developments in Quaternary Science, 7(C), 597-614. https://doi.org/10.1016/S1571-0866(07)80065-0

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abstract = "The last four interglacials (intervals during which global ice volume was similar to, or less than, that of our current warm stage) correspond to the warmest parts of the marine oxygen isotope stages MIS 5, 7, 9, 11. These interglacials ffollowed the 100-kyr rhythm of eccentricity, but each had different insolation regimes, different durations, different ice volumes and different sea-level heights, bur atmospheric greenhouse gas concentrations were similar and reached values which, by and large, were close to those of the current interglacial (Holocene or MIS1) before the industrial revolution led to the artificial enrichment of the atmosphere's greenhouse gas concentrations via the burning of fossil fuels ...",

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month = jan,

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doi = "10.1016/S1571-0866(07)80065-0",

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Sirocko, F, Claussen, M, Litt, T, Fernanda Sánchez Goñi, M, Berger, A, Boettger, T, Diehl, M, Desprat, S, Delmonte, B, Degering, D, Frechen, M, A. Geyh, M, Groeger, M, Kageyama, M, Kaspar, F, Kühl, N, Kubatzki, C, Lohmann, G, Loutre, MF, Müller, U, Rein, B, Rosendahl, W, Roucoux, K, Rousseau, DD, Seelos, K, Siddall, M, Scholz, D, Spötl, C, Urban, B, Vautravers, M, Velichko, A, Wenzel, S, Widmann, M & Wünnemann, B 2007, '40. Chronology and climate forcing of the last four interglacials', Developments in Quaternary Science, Jg. 7, Nr. C, S. 597-614. https://doi.org/10.1016/S1571-0866(07)80065-0

TY - JOUR

T1 - 40. Chronology and climate forcing of the last four interglacials

AU - Sirocko, Frank

AU - Claussen, Martin

AU - Litt, Thomas

AU - Fernanda Sánchez Goñi, Maria

AU - Berger, Andre

AU - Boettger, Tatjana

AU - Diehl, Markus

AU - Desprat, Stéphanie

AU - Delmonte, Barbara

AU - Degering, Detlev

AU - Frechen, Manfred

AU - A. Geyh, Mebus

AU - Groeger, Matthias

AU - Kageyama, Masa

AU - Kaspar, Frank

AU - Kühl, Norbert

AU - Kubatzki, Claudia

AU - Lohmann, Gerrit

AU - Loutre, Marie France

AU - Müller, Ulrich

AU - Rein, Bert

AU - Rosendahl, Wilfried

AU - Roucoux, Katy

AU - Rousseau, Denis Didier

AU - Seelos, Klemens

AU - Siddall, Mark

AU - Scholz, Denis

AU - Spötl, Christoph

AU - Urban, Brigitte

AU - Vautravers, Maryline

AU - Velichko, Andrei

AU - Wenzel, Stefan

AU - Widmann, Martin

AU - Wünnemann, Bernd

PY - 2007/1/1

Y1 - 2007/1/1

N2 - The last four interglacials (intervals during which global ice volume was similar to, or less than, that of our current warm stage) correspond to the warmest parts of the marine oxygen isotope stages MIS 5, 7, 9, 11. These interglacials ffollowed the 100-kyr rhythm of eccentricity, but each had different insolation regimes, different durations, different ice volumes and different sea-level heights, bur atmospheric greenhouse gas concentrations were similar and reached values which, by and large, were close to those of the current interglacial (Holocene or MIS1) before the industrial revolution led to the artificial enrichment of the atmosphere's greenhouse gas concentrations via the burning of fossil fuels ...

AB - The last four interglacials (intervals during which global ice volume was similar to, or less than, that of our current warm stage) correspond to the warmest parts of the marine oxygen isotope stages MIS 5, 7, 9, 11. These interglacials ffollowed the 100-kyr rhythm of eccentricity, but each had different insolation regimes, different durations, different ice volumes and different sea-level heights, bur atmospheric greenhouse gas concentrations were similar and reached values which, by and large, were close to those of the current interglacial (Holocene or MIS1) before the industrial revolution led to the artificial enrichment of the atmosphere's greenhouse gas concentrations via the burning of fossil fuels ...

KW - Environmental planning

UR - https://www.scopus.com/pages/publications/40849125641

U2 - 10.1016/S1571-0866(07)80065-0

DO - 10.1016/S1571-0866(07)80065-0

M3 - Conference article in journal

SN - 1571-0866

VL - 7

SP - 597

EP - 614

JO - Developments in Quaternary Science

JF - Developments in Quaternary Science

IS - C

ER -

40. Chronology and climate forcing of the last four interglacials

Abstract

UN SDGs

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