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Last Interglacial synthesis of high-latitude temperature: temperature anomali...
The Last Interglacial (LIG, 129-116 thousand of years BP, ka) represents a test bed for climate model feedbacks in warmer-than-present high latitude regions. However, mainly... -
Data for the manuscript "Interactive effects of management and temperature an...
Datasets related to the results presented in the manuscript "Interactive effects of management and temperature anomalies on CO2 fluxes recorded over 18 years in a temperate... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
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. -
LOVECLIM model data time series during MIS3
This dataset has no description
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Reconstructed temperature anomilies for ice core Colle_Gnifetti_KCC
Dataset corresponds to Figure 11 in the final manuscript. Please note that the period 1000-800 AD is given as a tentative extension only, with likely larger dating uncertainty. -
Relative abundance of planktic foraminifera and calculated SSTs and SST anoma...
This dataset has no description
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Global mean CO2, temperature and sea level data from transient model simulati...
Variations in Earth's orbit pace the glacial-interglacial cycles of the Quaternary, but the mechanisms that transform regional and seasonal variations in solar insolation into... -
Biomarker composition of Mediterranean Sapropels
This dataset has no description
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Alkenone temperature data of Holocene lake sediment sequence GJP0114 from Sva...
This dataset has no description
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Alkenone temperature data of Holocene lake sediment sequence HAP0212 from Sva...
This dataset has no description
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Alkenone temperature data of Holocene lake sediment sequence AMP112 from Sval...
This dataset has no description
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A: GISP2 temperature anomalies from δ15N fitting using Schwander et al. (1997...
Uncertainty is 2sigma = 0.80...0.88 K for the Schwander et al. (1997) firn model reconstruction and 2sigma = 0.86...0.94 K for the Goujon et al. (2003) firn model... -
D: GISP2 temperature anomalies from δ15N fitting using Schwander et al. (1997...
GISP2 temperature anomalies from d15N fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to... -
G: GISP2 temperature anomalies from δ40Ar fitting using Schwander et al. (199...
GISP2 temperature anomalies from δ40Ar fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model reconstructed using stabilized temperature from 70 to... -
J: GISP2 temperature anomalies from δ15Nexcess fitting using Schwander et al....
GISP2 temperature anomalies from δ15Nexcess fitting using Schwander et al. (1997) firn model and Goujon et al. (2003) firn model (Figure 4 and Supplement p. 6 in Döring and... -
N: GISP2 temperature anomalies from hybrid approach using Schwander et al. (1...
This dataset has no description
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MAAT reconstruction of sediment core Colonia_CO14
This dataset has no description
