Solar forced Dansgaard-Oeschger events and their phase relation with solar proxies

Peter Ditlevsen; H. Braun; D. R. Chialvo

doi:10.1029/2008GL033414

Solar forced Dansgaard-Oeschger events and their phase relation with solar proxies

Peter Ditlevsen, H. Braun, D. R. Chialvo

Is-, Klima- og Geofysik

25 Citationer (Scopus)

Abstract

North Atlantic climate during glacial times was characterized by large-amplitude switchings, the Dansgaard-Oeschger (DO) events, with an apparent tendency to recur preferably in multiples of about 1470 years. Recent work interpreted these intervals as resulting from a subharmonic response of a highly nonlinear system to quasi-periodic solar forcing plus noise. This hypothesis was challenged as inconsistent with the observed variability in the phase relation between proxies of solar activity and Greenland climate. Here we reject the claim of inconsistency by showing that this phase variability is a robust, generic feature of the nonlinear dynamics of DO events, as described by a model. This variability is expected from the fact that the events are threshold crossing events, resulting from a cooperative process between the periodic forcing and the noise. This process produces a fluctuating phase relation with the periodic forcing, consistent with proxies of solar activity and Greenland climate.
Udgivelsesdato: 25 March

Originalsprog	Engelsk
Tidsskrift	Geophysical Research Letters
Vol/bind	35
Udgave nummer	6
Sider (fra-til)	L06703
ISSN	0094-8276
DOI	https://doi.org/10.1029/2008GL033414
Status	Udgivet - 2008

Adgang til dokumentet

10.1029/2008GL033414

Citationsformater

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title = "Solar forced Dansgaard-Oeschger events and their phase relation with solar proxies",

abstract = "North Atlantic climate during glacial times was characterized by large-amplitude switchings, the Dansgaard-Oeschger (DO) events, with an apparent tendency to recur preferably in multiples of about 1470 years. Recent work interpreted these intervals as resulting from a subharmonic response of a highly nonlinear system to quasi-periodic solar forcing plus noise. This hypothesis was challenged as inconsistent with the observed variability in the phase relation between proxies of solar activity and Greenland climate. Here we reject the claim of inconsistency by showing that this phase variability is a robust, generic feature of the nonlinear dynamics of DO events, as described by a model. This variability is expected from the fact that the events are threshold crossing events, resulting from a cooperative process between the periodic forcing and the noise. This process produces a fluctuating phase relation with the periodic forcing, consistent with proxies of solar activity and Greenland climate. Udgivelsesdato: 25 March",

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T1 - Solar forced Dansgaard-Oeschger events and their phase relation with solar proxies

AU - Ditlevsen, Peter

AU - Braun, H.

AU - Chialvo, D. R.

PY - 2008

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N2 - North Atlantic climate during glacial times was characterized by large-amplitude switchings, the Dansgaard-Oeschger (DO) events, with an apparent tendency to recur preferably in multiples of about 1470 years. Recent work interpreted these intervals as resulting from a subharmonic response of a highly nonlinear system to quasi-periodic solar forcing plus noise. This hypothesis was challenged as inconsistent with the observed variability in the phase relation between proxies of solar activity and Greenland climate. Here we reject the claim of inconsistency by showing that this phase variability is a robust, generic feature of the nonlinear dynamics of DO events, as described by a model. This variability is expected from the fact that the events are threshold crossing events, resulting from a cooperative process between the periodic forcing and the noise. This process produces a fluctuating phase relation with the periodic forcing, consistent with proxies of solar activity and Greenland climate. Udgivelsesdato: 25 March

AB - North Atlantic climate during glacial times was characterized by large-amplitude switchings, the Dansgaard-Oeschger (DO) events, with an apparent tendency to recur preferably in multiples of about 1470 years. Recent work interpreted these intervals as resulting from a subharmonic response of a highly nonlinear system to quasi-periodic solar forcing plus noise. This hypothesis was challenged as inconsistent with the observed variability in the phase relation between proxies of solar activity and Greenland climate. Here we reject the claim of inconsistency by showing that this phase variability is a robust, generic feature of the nonlinear dynamics of DO events, as described by a model. This variability is expected from the fact that the events are threshold crossing events, resulting from a cooperative process between the periodic forcing and the noise. This process produces a fluctuating phase relation with the periodic forcing, consistent with proxies of solar activity and Greenland climate. Udgivelsesdato: 25 March

U2 - 10.1029/2008GL033414

DO - 10.1029/2008GL033414

M3 - Journal article

SN - 0094-8276

VL - 35

SP - L06703

JO - Geophysical Research Letters

JF - Geophysical Research Letters

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