Mid- to Late Holocene climate change

Metadata Label Value
Author(s) Wanner, Heinz, Beer, Jürg, Bütikofer, Jonathan, Crowley, Thomas J., Cubasch, Ulrich, Flückiger, Jacqueline, Goosse, Hugues, Grosjean, Martin, Joos, Fortunat, Kaplan, Jed O., Küttel, Marcel, Müller, Simon A., Prentice, I. Colin, Solomina, Olga, Stocker, Thomas F., Tarasov, Pavel, Wagner, Mayke, Widmann, Martin
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley

Detailed Information

Metadata Field Content
Title Mid- to Late Holocene climate change
Subtitle An overview
Author(s) Wanner, Heinz
Beer, Jürg
Bütikofer, Jonathan
Crowley, Thomas J.
Cubasch, Ulrich
Flückiger, Jacqueline
Goosse, Hugues
Grosjean, Martin
Joos, Fortunat
Kaplan, Jed O.
Küttel, Marcel
Müller, Simon A.
Prentice, I. Colin
Solomina, Olga
Stocker, Thomas F.
Tarasov, Pavel
Wagner, Mayke
Widmann, Martin
Journal or Series Title Quaternary science reviews
Volume Number 27
Issue Number 19-20
Start Page 1791
End Page 1828
ISSN 0277-3791
Publisher Elsevier
Publication Place Amsterdam
Publication Date 2008-00-00
Abstract The last 6000 years are of particular interest to the understanding of the Earth System because the boundary conditions of the climate system did not change dramatically (in comparison to larger glacial–interglacial changes), and because abundant, detailed regional palaeoclimatic proxy records cover this period. We use selected proxy-based reconstructions of different climate variables, together with state-of-the-art time series of natural forcings (orbital variations, solar activity variations, large tropical volcanic eruptions, land cover and greenhouse gases), underpinned by results from General Circulation Models (GCMs) and Earth System Models of Intermediate Complexity (EMICs), to establish a comprehensive explanatory framework for climate changes from the Mid-Holocene (MH) to pre-industrial time. The redistribution of solar energy, due to orbital forcing on a millennial timescale, was the cause of a progressive southward shift of the Northern Hemisphere (NH) summer position of the Intertropical Convergence Zone (ITCZ). This was accompanied by a pronounced weakening of the monsoon systems in Africa and Asia and increasing dryness and desertification on both continents. The associated summertime cooling of the NH, combined with changing temperature gradients in the world oceans, likely led to an increasing amplitude of the El Niño Southern Oscillation (ENSO) and, possibly, increasingly negative North Atlantic Oscillation (NAO) indices up to the beginning of the last millennium. On decadal to multi-century timescales, a worldwide coincidence between solar irradiance minima, tropical volcanic eruptions and decadal to multi-century scale cooling events was not found. However, reconstructions show that widespread decadal to multi-century scale cooling events, accompanied by advances of mountain glaciers, occurred in the NH (e.g., in Scandinavia and the European Alps). This occurred namely during the Little Ice Age (LIA) between AD 1350 and 1850, when the lower summer insolation in the NH, due to orbital forcing, coincided with solar activity minima and several strong tropical volcanic eruptions. The role of orbital forcing in the NH cooling, the southward ITCZ shift and the desertification of the Sahara are supported by numerous model simulations. Other simulations have suggested that the fingerprint of solar activity variations should be strongest in the tropics, but there is also evidence that changes in the ocean heat transport took place during the LIA at high northern latitudes, with possible additional implications for climates of the Southern Hemisphere (SH).
DOI 10.1016/j.quascirev.2008.06.013
Additional Notes Received 26 March 2008, Received in revised form 20 June 2008, Accepted 23 June 2008, Available online 27 September 2008
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 000015707
Source Database ID PP-43938
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

  author = "Wanner, Heinz and Beer, J{\"{u}}rg and B{\"{u}}tikofer, Jonathan and Crowley, Thomas J. and Cubasch, Ulrich and Fl{\"{u}}ckiger, Jacqueline and Goosse, Hugues and Grosjean, Martin and Joos, Fortunat and Kaplan, Jed O. and K{\"{u}}ttel, Marcel and M{\"{u}}ller, Simon A. and Prentice, I. Colin and Solomina, Olga and Stocker, Thomas F. and Tarasov, Pavel and Wagner, Mayke and Widmann, Martin",
  title = "{M}id- to {L}ate {H}olocene climate change: {A}n overview",
  journal = "Quaternary science reviews",
  year = 2008,
  volume = "27",
  number = "19-20",
  pages = "1791--1828",

E-Citations record created: Fri, 02 Apr 2010, 00:33:44 CET