Skip to Main content Skip to Navigation
Journal articles

Abrupt climate changes and the astronomical theory

Abstract : Abrupt climate changes constitute a relatively new field of research, which addresses variations occurring in a relatively short time interval of tens to a hundred years. Such time scales do not correspond to the tens or hundreds of thousands of years that the astronomical theory of climate addresses. The latter theory involves parameters that are external to the climate system and whose multi-periodic variations are reliably known and almost constant for a large extent of Earth history. Abrupt changes, conversely, appear to involve fast processes that are internal to the climate system; these processes varied considerably during the past 2.6 Myr, and yielded more irregular fluctuations. In this paper, we reexamine the main climate variations determined from the U1308 North Atlantic marine record, which yields a detailed calving history of the Northern Hemisphere ice sheets over the past 3.2 Myr. The magnitude and periodicity of the ice-rafted debris (IRD) events observed in the U1308 record allow one to determine the timing of several abrupt climate changes, the larger ones corresponding to the massive iceberg discharges labeled Heinrich events (HEs). In parallel, abrupt warmings, called Dansgaard-Oeschger (DO) events, have been identified in the Greenland records of the last glaciation cycle. Combining the HE and DO observations, we study a complex mechanism that may lead to the observed millennial-scale variability corresponding to the abrupt climate changes of last 0.9 Myr. This mechanism relies on amended Bond cycles, which group DO events and the associated Greenland stadials into a trend of increased cooling, with IRD events embedded into every stadial, the latest of these being an HE. These Bond cycles may have occurred during the last 0.9 Ma when Northern Hemisphere ice sheets reached their maximum extent and volume, thus becoming a major player in this time interval's climate dynamics. Since the waxing and waning of ice sheets during the Quaternary period are orbitally paced, we conclude that the abrupt climate changes observed during the Mid and Upper Pleistocene are therewith indirectly linked to the astronomical theory of climate.
Complete list of metadata

https://hal-insu.archives-ouvertes.fr/insu-03319020
Contributor : Denis-Didier Rousseau Connect in order to contact the contributor
Submitted on : Wednesday, August 11, 2021 - 3:19:37 PM
Last modification on : Friday, October 15, 2021 - 1:41:39 PM

File

DDR.ea_CP_v8.pdf
Files produced by the author(s)

Identifiers

  • HAL Id : insu-03319020, version 1

Citation

Denis-Didier Rousseau, Witold Bagniewski, Michael Ghil. Abrupt climate changes and the astronomical theory. Climate of the Past Discussions, European Geosciences Union (EGU), 2021. ⟨insu-03319020⟩

Share

Metrics

Record views

38

Files downloads

44