EGU25-4520, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-4520
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 08:30–10:15 (CEST), Display time Monday, 28 Apr, 08:30–12:30
 
Hall X2, X2.60
Using data assimilation to combine model outcomes and reconstructions of seasonality during past warm periods
Niels de Winter1, Barbara Goudsmit-Harzevoort2,3, Brendan Oerlemans1, Rob Witbaard2, Pepijn Bakker1, Julia Tindall4, Alexander Farnsworth5, and Martin Ziegler3
Niels de Winter et al.
  • 1Department of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, Netherlands (n.j.de.winter@vu.nl)
  • 2Royal Netherlands Institute for Sea Research, Texel, the Netherlands
  • 3Department of Earth Sciences, Utrecht University, Utrecht, the Netherlands
  • 4School of Earth and Environment, University of Leeds, Leeds, United Kingdom
  • 5School of Geographical Sciences, University of Bristol, Bristol, United Kingdom

Anthropogenic global change necessitates the improvement of our understanding of the dynamics of warmer climates in the past. Combining information from Earth’s climate history with numerical simulations of past climate helps us to identify gaps in our knowledge of climate mechanisms and improves projections for future climate1,2. Data assimilation is a valuable tool to reconcile information from climate reconstructions and models in a consistent statistical framework3. These data assimilation efforts have focused mostly on climate variability on geological timescales (thousands to millions of years). However, seasonal changes in climate parameters such as temperature and precipitation are a defining characteristic of climate zones and have a dominant impact on the impact of climate on nature and human society4.

This work lays the foundations for applying data assimilation techniques to compare and combine reconstructions and model information on a seasonal scale. We use seasonal-scale temperature reconstructions from incrementally grown fossil mollusc shells which record seasonality in their living environment during modern5, Pliocene4 and Cretaceous periods6. We combine these data with model outcomes from the same periods to arrive at a combined estimate of seasonal temperature variability and discuss the methodological choices that lead to this result. Using this data analysis product allows us to more easily interrogate the outcomes from climate models with various boundary conditions using proxy-based information on select climate variables. The aim is to lay the foundation for data assimilation for estimating short-term climate variability in the geological past from skeletal carbonate archives and comparing model and reconstruction outcomes.

 

References

  • Hakim, G. J. et al. The last millennium climate reanalysis project: Framework and first results. Journal of Geophysical Research: Atmospheres 121, 6745–6764 (2016).
  • Tierney, J. E. et al. Past climates inform our future. Science 370, (2020).
  • Dirren, S. & Hakim, G. J. Toward the assimilation of time-averaged observations. Geophysical Research Letters 32, (2005).
  • de Winter, N. J. et al. Amplified seasonality in western Europe in a warmer world. Science Advances 10, eadl6717 (2024).
  • Caldarescu, D. E. et al. Clumped isotope thermometry in bivalve shells: A tool for reconstructing seasonal upwelling. Geochimica et Cosmochimica Acta 294, 174–191 (2021).
  • de Winter, N. J. et al. Absolute seasonal temperature estimates from clumped isotopes in bivalve shells suggest warm and variable greenhouse climate. Commun Earth Environ 2, 1–8 (2021).

How to cite: de Winter, N., Goudsmit-Harzevoort, B., Oerlemans, B., Witbaard, R., Bakker, P., Tindall, J., Farnsworth, A., and Ziegler, M.: Using data assimilation to combine model outcomes and reconstructions of seasonality during past warm periods, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-4520, https://doi.org/10.5194/egusphere-egu25-4520, 2025.