Glacial Ocean Atlas

Table S3: Diatoms-based LGM SST anomalies. The file header contains a description of the content of each column. All SST proxies in the MARGO compilation have been calibrated to pre-1998 long-term average SST and the LGM SST anomalies are here calculated as the differences between WOA98 climatology and the reconstructed values.

Table S4: Radiolarians-based LGM SST anomalies. As in Table S3.

Table S5: Dinocysts-based LGM SST anomalies. As in Table S3.

Table S6: Foraminifera-based LGM SST anomalies. As in Table S3.

Table S7: Alkenone-based LGM SST anomalies. As in Table S3.

Table S8: Mg/Ca-based LGM SST anomalies. As in Table S3.

Table S9: 5°x5° block weighted mean values. The file header contains a description of the content of each column. By convention (International Hydrographic Bureau 1953), the meridian of Cape Agulhas (20°E) was taken as the boundary between the Atlantic and Indian Oceans, the meridian of the southern cape of Tasmania (147°E) was taken as the boundary between the Indian and Pacific Oceans and the meridian of Cape Horn (68°W) was taken as the boundary between the Pacific and Indian Oceans. The Nordic Seas and Arctic Ocean were included in the Atlantic Ocean.

The same data in other formats:

NetCDF

ODV Generic Spreadsheet