Journal cover Journal topic
Climate of the Past An interactive open-access journal of the European Geosciences Union
CP cover

Climate of the Past (CP) is an international scientific journal dedicated to the publication and discussion of research articles, short communications, and review papers on the climate history of the Earth. CP covers all temporal scales of climate change and variability, from geological time through to multidecadal studies of the last century. Studies focusing mainly on present and future climate are not within scope.


Geographical distribution of views now available in journal ALMs

08 Sep 2016

Copernicus Publications has extended the article level metrics (ALMs) by showing the geographical distribution of views. This information is available for articles published after 3 August 2016.

Institutional agreement for CP authors affiliated with the Leibniz Association

01 Sep 2016

Copernicus Publications and the Leibniz Association have agreed on a central billing of article processing charges (APCs) to facilitate the publication procedure for authors. So far three Leibniz institutes are participating in this agreement.

CP editor Appy Sluijs receives James B. Macelwane Medal

03 Aug 2016

We are delighted that CP editor Appy Sluijs is among the awardees of the 2016 AGU James B. Macelwane Medal. Congratulations!

Recent articles

Highlight articles

This paper focuses on early Holocene rapid climate changes in the Mediterranean zone, which are under-represented in continental archives, and on their impact on prehistoric societies from the eastern to central Mediterranean (central Anatolia, Cyprus, NE and NW Greece). Our study demonstrates the reality of hydrogeomorphological responses to early Holocene RCCs in valleys and alluvial fans and lake-marsh systems. We finally question their socio-economic and geographical adaptation capacities.

J.-F. Berger, L. Lespez, C. Kuzucuoğlu, A. Glais, F. Hourani, A. Barra, and J. Guilaine

Past intervals in Earth history provide unique windows into conditions much different than those observed today. We investigated the paleoenvironments of a past warm interval (~3 million years ago). Our reconstruction includes data sets for surface temperature, vegetation, soils, lakes, ice sheets, topography, and bathymetry. These data are being used along with global climate models to expand our understanding of the climate system and to help us prepare for future changes.

H. Dowsett, A. Dolan, D. Rowley, R. Moucha, A. M. Forte, J. X. Mitrovica, M. Pound, U. Salzmann, M. Robinson, M. Chandler, K. Foley, and A. Haywood

We use an isotope-equipped GCM and develop original theoretical expression for the precipitation composition to assess δ18O of paleo-precipitation changes with the Tibetan Plateau uplift. We show that δ18O of precipitation is very sensitive to climate changes related to the growth of mountains, notably changes in relative humidity and precipitation amount. Topography is shown to be not an exclusive controlling factor δ18O in precipitation that have crucial consequences for paleoelevation studies.

S. Botsyun, P. Sepulchre, C. Risi, and Y. Donnadieu

This study presents an average of seven Late Pleistocene sea level records, which improves the signal-to-noise ratio for estimates of sea level change during glacial cycles of the past 800 000 years.

R. M. Spratt and L. E. Lisiecki

We demonstrate for the first time the direct link between dust accumulation in marine sediment cores and Saharan land surface by simulating the mid-Holocene and pre-industrial dust cycle as a function of Saharan land surface cover and atmosphere-ocean conditions using the coupled atmosphere-aerosol model ECHAM6-HAM2.1. Mid-Holocene surface characteristics, including vegetation cover and lake surface area, are derived from proxy data and simulations.

S. Egerer, M. Claussen, C. Reick, and T. Stanelle

Publications Copernicus