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Mulitza, Stefan; Chiessi, Cristiano Mazur; Schefuß, Enno; Lippold, Jörg; Wichmann, David; Antz, Benny; Mackensen, Andreas; Paul, André; Prange, Matthias; Rehfeld, Kira; Werner, Martin; Bickert, Torsten; Frank, Norbert; Kuhnert, Henning; Lynch-Stieglitz, Jean; Portilho-Ramos, Rodrigo Costa; Sawakuchi, André O; Schulz, Michael; Schwenk, Tilmann; Tiedemann, Ralf; Vahlenkamp, Maximilian; Zhang, Yancheng (2017): Investigations of sediment core GeoB16202-2 to elucidate the coevolution of continental precipitation, terrestrial matter erosion, and AMOC during the last deglaciation. PANGAEA, https://doi.org/10.1594/PANGAEA.877731, Supplement to: Mulitza, Stefan; Schefuß, Enno; Chiessi, Cristiano Mazur; Lippold, Jörg; Wichmann, David; Antz, Benny; Mackensen, Andreas; Paul, André; Prange, Matthias; Rehfeld, Kira; Werner, Martin; Bickert, Torsten; Frank, Norbert; Kuhnert, Henning; Lynch-Stieglitz, Jean; Portilho-Ramos, Rodrigo Costa; Sawakuchi, André O; Schulz, Michael; Schwenk, Tilmann; Tiedemann, Ralf; Vahlenkamp, Maximilian; Zhang, Yancheng (2017): Synchronous and proportional deglacial changes in Atlantic meridional overturning and northeast Brazilian precipitation. Paleoceanography, https://doi.org/10.1002/2017PA003084

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Abstract:
Changes in heat transport associated with fluctuations in the strength of the Atlantic meridional overturning circulation (AMOC) are widely considered to affect the position of the Intertropical Convergence Zone (ITCZ), but the temporal immediacy of this teleconnection has to date not been resolved. Based on a high-resolution marine sediment sequence over the last deglaciation, we provide evidence for a synchronous and near-linear link between changes in the Atlantic interhemispheric sea surface temperature difference and continental precipitation over northeast Brazil. The tight coupling between AMOC strength, sea surface temperature difference, and precipitation changes over northeast Brazil unambiguously points to a rapid and proportional adjustment of the ITCZ location to past changes in the Atlantic meridional heat transport.
Coverage:
Latitude: -1.908333 * Longitude: -41.591667
Date/Time Start: 2012-02-22T15:41:00 * Date/Time End: 2012-02-22T15:41:00
Size:
11 datasets

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Datasets listed in this publication series

  1. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Age model of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877639
  2. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Iron/Calcium ratio of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877685
  3. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Opal contents of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877698
  4. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Protactinium/Thorium ratios of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877699
  5. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Radiocarbon age of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877727
  6. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Radionuclides of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877728
  7. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Sedimentation rates of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877729
  8. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Stable isotopes on benthic foraminifera of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877641
  9. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): Temperature difference vs. dD of sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877730
  10. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): d13C of C29 and C31 plant wax n-alkanes from sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877712
  11. Mulitza, S; Chiessi, CM; Schefuß, E et al. (2017): dD of C29 and C31 plant wax n-alkanes from sediment core GeoB16202-2. https://doi.org/10.1594/PANGAEA.877724