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

Research output: Journal contributions › Conference article in journal › Research › peer-review

Standard

40. Chronology and climate forcing of the last four interglacials. / Sirocko, Frank; Claussen, Martin; Litt, Thomas et al.
In: Developments in Quaternary Science, Vol. 7, No. C, 01.01.2007, p. 597-614.

Research output: Journal contributions › Conference article in journal › Research › peer-review

Harvard

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, vol. 7, no. C, pp. 597-614. https://doi.org/10.1016/S1571-0866(07)80065-0

APA

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

Vancouver

Sirocko F, Claussen M, Litt T, Fernanda Sánchez Goñi M, Berger A, Boettger T et al. 40. Chronology and climate forcing of the last four interglacials. Developments in Quaternary Science. 2007 Jan 1;7(C):597-614. doi: 10.1016/S1571-0866(07)80065-0

Bibtex

@article{7fd9d004b62743329318e9215cb50dd6,

title = "40. Chronology and climate forcing of the last four interglacials",

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 ...",

keywords = "Environmental planning",

author = "Frank Sirocko and Martin Claussen and Thomas Litt and {Fernanda S{\'a}nchez Go{\~n}i}, Maria and Andre Berger and Tatjana Boettger and Markus Diehl and St{\'e}phanie Desprat and Barbara Delmonte and Detlev Degering and Manfred Frechen and {A. Geyh}, Mebus and Matthias Groeger and Masa Kageyama and Frank Kaspar and Norbert K{\"u}hl and Claudia Kubatzki and Gerrit Lohmann and Loutre, {Marie France} and Ulrich M{\"u}ller and Bert Rein and Wilfried Rosendahl and Katy Roucoux and Rousseau, {Denis Didier} and Klemens Seelos and Mark Siddall and Denis Scholz and Christoph Sp{\"o}tl and Brigitte Urban and Maryline Vautravers and Andrei Velichko and Stefan Wenzel and Martin Widmann and Bernd W{\"u}nnemann",

year = "2007",

month = jan,

day = "1",

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

language = "English",

volume = "7",

pages = "597--614",

journal = "Developments in Quaternary Science",

issn = "1571-0866",

publisher = "Elsevier Ltd",

number = "C",

}

RIS

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 - http://www.scopus.com/inward/record.url?scp=40849125641&partnerID=8YFLogxK

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

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

M3 - Conference article in journal

VL - 7

SP - 597

EP - 614

JO - Developments in Quaternary Science

JF - Developments in Quaternary Science

SN - 1571-0866

IS - C

ER -

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