-
Maximum annual SST estimates during the early LIG (129-124 ka; 189 sites)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
Annual SST estimates for the Last Interglacial (129-116 ka BP)
Drift correction has not been applied to the two coral sites!Drift correction could not be applied to four sites in a land box when located using OFES. -
(Table S1) Planktonic foraminifera abundances for the 1223 surface sediment s...
Our training set (SH0911C2, available from http://www.ncdc.noaa.gov/paleo/paleo.html) augments that used by Crundwell el al . [2008, Figure 2] with additional data from Mohtadi... -
Compilation of planktonic foraminiferal census counts from the Southern Hemis...
We present an improved database of planktonic foraminiferal census counts from the Southern Hemisphere Oceans (SHO) from 15°S to 64°S. The SHO database combines 3 existing... -
Compilation of delta 18O data from planktonic foraminifera in surface sediment
Note that the exact depth in sediment is not given in this compilation. -
Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Compilation of 220 sediment core δ¹³C data from the glacial Atlantic Ocean
We compare a compilation of 220 sediment core d13C data from the glacial Atlantic Ocean with three-dimensional ocean circulation simulations including a marine carbon cycle... -
Master tracks in different resolutions of POLARSTERN cruise PS18/4, Cape Town...
Raw data acquired by position sensors on board RV Polarstern during expedition ANT-IX/4 was processed to receive a validated master track which can be used as reference of... -
Master track of POLARSTERN cruise PS18/4 in 1 sec resolution (zipped, 169 MB)
Raw data acquired by position sensors on board RV Polarstern during expedition ANT-IX/4 was processed to receive a validated master track which can be used as reference of... -
δ18O and δ13C of Cibicidoides wuellerstorfi and related species and carbonate...
The δ13C composition of Cibicidoides wuellerstorfi and other Cibicidoides spp is an important tool to reconstruct past changes in the deep ocean carbon cycle. The species are... -
Station list and links to master tracks in different resolutions of POLARSTER...
This dataset has no description
-
(Table 6) Stable carbon and oxygen isotope composition of live and dead benth...
-0.05 m depth is mean of MUC bottom water sample. -
Radiosonde PS18/06414 during POLARSTERN cruise ANT-IX/4 on 1991-05-11 10:43h
Height of tropopause 12071 m, precipitable water content 2.0636 cm -
Radiosonde PS18/06413 during POLARSTERN cruise ANT-IX/4 on 1991-05-10 09:25h
Height of tropopause 10096 m, precipitable water content 1.0509 cm -
Radiosonde PS18/06412 during POLARSTERN cruise ANT-IX/4 on 1991-05-09 10:33h
Height of tropopause 11085 m, precipitable water content 1.1393 cm -
Radiosonde PS18/06411 during POLARSTERN cruise ANT-IX/4 on 1991-05-08 10:32h
Height of tropopause 11366 m, precipitable water content 1.997 cm -
Radiosonde PS18/06410 during POLARSTERN cruise ANT-IX/4 on 1991-05-07 14:32h
Height of tropopause 16223 m, precipitable water content 1.0228 cm -
Radiosonde PS18/06409 during POLARSTERN cruise ANT-IX/4 on 1991-05-06 10:31h
Height of tropopause 12222 m, precipitable water content 1.0773 cm -
Radiosonde PS18/06408 during POLARSTERN cruise ANT-IX/4 on 1991-05-05 10:21h
Height of tropopause 11566 m, precipitable water content 1.4221 cm -
Radiosonde PS18/06407 during POLARSTERN cruise ANT-IX/4 on 1991-05-04 10:11h
Height of tropopause 16260 m, precipitable water content 1.2394 cm