-
CLIMAP_OSU LGM sea surface temperature
Created by taking the annual-average version of CLIMAP 1981 reconstruction, and replacing the data in the region 140W-20E, 20N-20S with OSU estimates and new codes for 0=ocean,... -
CLIMAP_OSU sea surface temperature anomaly
Created by taking the annual-average version of CLIMAP 1981 reconstruction, and replacing the data in the region 140W-20E, 20N-20S with OSU estimates and new codes for 0=ocean,... -
Stable carbon and oxygen isotope ratios of planktonic foraminifera from the e...
Carbon isotopic records of nutrient-depleted surface water place constraints on the past fertility of the oceans and on past atmospheric pCO2 levels. The best records of... -
LGM CLIMAP sea surface temperature
Created by averaging the CLIMAP 1981 seasonal files with new codes for 0=ocean, -222=seasonal sea ice, -444=sea ice, -555=land ice, -999=land. See Hostetler & Mix, 1999. -
CLIMAP sea surface temperature anomaly (LGM-modern)
Created by averaging the CLIMAP 1981 seasonal files with new codes for 0=ocean, -222=seasonal sea ice, -444=sea ice, -555=land ice, -999=land. See Hostetler & Mix, 1999. -
Modern CLIMAP sea surface temperature
Created by averaging the CLIMAP 1981 seasonal files with new codes for 0=ocean, -222=seasonal sea ice, -444=sea ice, -555=land ice, -999=land. See Hostetler & Mix, 1999. -
Monthly Southern Oscillation Index from 1866 to 1997
The SOI is defined as the normalized pressure difference between Tahiti and Darwin. There are several slight variations in the SOI values calculated at various centres. Here we... -
Monthly values of the North Atlantic Oscillation Index from 1821 to 2000
Early instrumental pressure measurements from Gibraltar and the Reykjavik area of Iceland have been used to extend to 1821 the homogeneous pressure series at the two locations.... -
Various flux data of organic material modeled for the North Atlantic
Gridded data set (2 x 2 degree) of modeled flux rates -
Rock magnetics and age models of three sediment cores from Makarov Basin
Three long sediment cores from the Makarov Basin have been subjected to detailed paleomagnetic and rock magnetic analyses. Investigated sediments are dominated by normal... -
Paleointensity stacked from three sediment cores, named as MakarovStack
Depth is composite depth, compiled from sediment cores PS2178-3, PS2178-5 and PS2180-2 -
(Table 5) Stacked records of stable carbon and oxygen isotopes for Equatorial...
Stacked record for Equatorial Atlantic, presented as diff from avg Late Holocene (0 to 8 kyr) isotopic composition. The record has been linearly interpolated to 1000-year sample... -
Input-output parameters for the steady-state model of Independencia Bay in 19...
This dataset has no description
-
Input-output parameters for the steady-state model of Independencia Bay in 19...
This dataset has no description
