Articles | Volume 11, issue 10
https://doi.org/10.5194/cp-11-1335-2015
© Author(s) 2015. 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-11-1335-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Obliquity forcing of low-latitude climate
Faculty of Geosciences, Utrecht University, the Netherlands
Royal Netherlands Meteorological Institute (KNMI), the Netherlands
now at: Faculty of Geosciences, Utrecht University, the Netherlands
Invited contribution by J. H. C. Bosmans, recipient of the EGU Outstanding Student Poster (OSP) Awards 2013.
F. J. Hilgen
Faculty of Geosciences, Utrecht University, the Netherlands
E. Tuenter
Faculty of Geosciences, Utrecht University, the Netherlands
Royal Netherlands Meteorological Institute (KNMI), the Netherlands
now at: Royal Netherlands Meteorological Institute (KNMI), the Netherlands
L. J. Lourens
Faculty of Geosciences, Utrecht University, the Netherlands
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Short summary
Our study shows that the influence of obliquity (the tilt of Earth's rotational axis) can be explained through changes in the insolation gradient across the tropics. This explanation is fundamentally different from high-latitude mechanisms that were previously often inferred to explain obliquity signals in low-latitude paleoclimate records, for instance glacial fluctuations. Our study is based on state-of-the-art climate model experiments.
Our study shows that the influence of obliquity (the tilt of Earth's rotational axis) can be...