Articles | Volume 12, issue 3
https://doi.org/10.5194/cp-12-713-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-713-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
21 Mar 2016
Research article |
| 21 Mar 2016
A distal 140 kyr sediment record of Nile discharge and East African monsoon variability
Universität Leipzig, Institut für Geophysik und Geologie,
Talstraße 35, 04103 Leipzig, Germany
Gerhard Schmiedl
Universität Hamburg, Centrum für Erdsystemforschung und
Nachhaltigkeit, Bundesstraße 55, 20146 Hamburg, Germany
Martin Seidel
Universität Leipzig, Institut für Geophysik und Geologie,
Talstraße 35, 04103 Leipzig, Germany
Stefan Krüger
Universität Leipzig, Institut für Geophysik und Geologie,
Talstraße 35, 04103 Leipzig, Germany
Hartmut Schulz
Universität Tübingen, Fachbereich Geowissenschaften,
Hölderlinstraße 12, 72074 Tübingen, Germany
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H. Schulz and U. von Rad
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Y. Milker, M. Wilken, J. Schumann, D. Sakuna, P. Feldens, K. Schwarzer, and G. Schmiedl
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Related subject area
Subject: Feedback and Forcing | Archive: Marine Archives | Timescale: Pleistocene
Insolation evolution and ice volume legacies determine interglacial and glacial intensity
The transient impact of the African monsoon on Plio-Pleistocene Mediterranean sediments
Bispectra of climate cycles show how ice ages are fuelled
Land–sea coupling of early Pleistocene glacial cycles in the southern North Sea exhibit dominant Northern Hemisphere forcing
Takahito Mitsui, Polychronis C. Tzedakis, and Eric W. Wolff
Clim. Past, 18, 1983–1996, https://doi.org/10.5194/cp-18-1983-2022, https://doi.org/10.5194/cp-18-1983-2022, 2022
Short summary
Short summary
We provide simple quantitative models for the interglacial and glacial intensities over the last 800 000 years. Our results suggest that the memory of previous climate states and the time course of the insolation in both hemispheres are crucial for understanding interglacial and glacial intensities. In our model, the shift in interglacial intensities at the Mid-Brunhes Event (~430 ka) is ultimately attributed to the amplitude modulation of obliquity.
Bas de Boer, Marit Peters, and Lucas J. Lourens
Clim. Past, 17, 331–344, https://doi.org/10.5194/cp-17-331-2021, https://doi.org/10.5194/cp-17-331-2021, 2021
Diederik Liebrand and Anouk T. M. de Bakker
Clim. Past, 15, 1959–1983, https://doi.org/10.5194/cp-15-1959-2019, https://doi.org/10.5194/cp-15-1959-2019, 2019
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We present a new analysis and interpretation of a well-established climate record that spans the past 5 million years. We describe how the energy the Earth receives from the Sun is transferred among climate cycles with different duration. This analysis offers new insights into the complex evolution of the global climate system and land-ice volumes during this time. Furthermore, it provides a more complete solution to the long-standing 40 000- and ~100 000-year problems of the ice ages.
Timme H. Donders, Niels A. G. M. van Helmond, Roel Verreussel, Dirk Munsterman, Johan ten Veen, Robert P. Speijer, Johan W. H. Weijers, Francesca Sangiorgi, Francien Peterse, Gert-Jan Reichart, Jaap S. Sinninghe Damsté, Lucas Lourens, Gesa Kuhlmann, and Henk Brinkhuis
Clim. Past, 14, 397–411, https://doi.org/10.5194/cp-14-397-2018, https://doi.org/10.5194/cp-14-397-2018, 2018
Short summary
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The buildup and melting of ice during the early glaciations in the Northern Hemisphere, around 2.5 million years ago, were far shorter in duration than during the last million years. Based on molecular compounds and microfossils from sediments dating back to the early glaciations we show that the temperature on land and in the sea changed simultaneously and was a major factor in the ice buildup in the Northern Hemisphere. These data provide key insights into the dynamics of early glaciations.
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