Modelled atmospheric temperatures and global sea levels over the past million years

By R. Bintanja, Roderik S. W. van de Wal, J. Oerlemans. Nature, 2005

757 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Environmental Chemistry

View Paper: https://www.semanticscholar.org/paper/b843063f7422a2bfe5174f0890d74179edf3a00d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. J. Ali
2. Jonathan Aitchison
3. F. Joos
4. Gerrit Lohmann
5. A. Townsend Peterson
6. Reto Knutti
7. R. Bintanja
8. H. Fischer

In Ecology

1. W. Ludt
2. Jonathan Aitchison
3. J. Ali
4. Luiz A. Rocha
5. A. Townsend Peterson
6. Rafe M. Brown
7. Jorge Soberón
8. R. P. Anderson

In Environmental Chemistry

1. Jonathan Aitchison
2. J. Ali
3. F. Joos
4. Gerrit Lohmann

Citations in the corpus

• Probabilistic assessment of sea level during the last interglacial stage (2009, neutral): “[16] Kendall, R.”
• What caused Earths temperature variations during the last 800,000 years? Data-based evidences on radiative forcing and constraints on climate sensitivity (2009, methodology): “The model of Bintanja et al. (2005) furthermore calculates, based on monthly snow cover simulations (Bintanja et al., 2002), that the surface albedo on the ice sheets was about 0.6 larger than on the ice-free continents (Fig.”
• Integrating phylogenetic and taxonomic evidence illuminates complex biogeographic patterns along Huxley’s modification of Wallace’s Line (2010, background): “…estimates for the penultimate glacial period suggest that Palawan and Borneo were not united at that time, with reconstructed sea-level minima nearer the )120 m typically inferred for the most recent glacial maximum (e.g. Siddall et al., 2003, 2006; Bintanja et al., 2005; Thomas et al., 2009).”
• Shifting seas: the impacts of Pleistocene sea‐level fluctuations on the evolution of tropical marine taxa (2015, background): “Low sea levels culminated in coastlines 115–130 m below current level, reaching a minimum during the Last Glacial Maximum (LGM) c. 17–19 ka (Fairbanks, 1989; Hanebuth et al., 2000; Voris, 2000; Bintanja et al., 2005; Bintanja & van de Wal, 2008; Clark et al., 2009).”
• Exploring the combined role of eustasy and oceanic island thermal subsidence in shaping biodiversity on the Galápagos (2014, methodology): “100 kyr fallen to between about 90 and 130 m below the present datum (Bintanja et al., 2005; Rohling et al., 2009; Elderfield et al., 2012).”