1. Glacial/Interglacial Paleoclimate

2. N. American cold winds affected N. Atlantic SST

3. Size of ice sheets controlled climate in mid- and high-latitude regions

9. Paleoclimate of the Last Glacial Maximum

10. Climap reconstruction of SST

12. Climap reconstructions of ice thickness do not match recent glacial reconstructions

15. Today precipitation and temperature control the distribution of vegetation in the Midwest.

17. Model simulations verified that colder conditions forced a change in vegetation, although these simulations do not fully capture proxy data.

20. Melting of southward- floating icebergs.

23. Tropical cooling during the LGM

24. Climap’s SST reconstructions for low latitudes is based on small differences