To get a view on global temperatures that long ago, the researchers studied 73 sediment and
polar ice samples, taken from all over the globe.
Not exact matches
Following an expected soft landing in the northern
polar region, Phoenix will study the planet's
ice cap and use a robotic arm to dig into the Martian subsurface, collecting
ice and soil
samples.
Keeling's record of data from Mauna Loa is considered one of the best and most consistent climate records anywhere, though scientists also use other sources for atmospheric data, including
samples of air trapped in
polar ice, to analyze CO2 levels in past millennia.
By far the best match was to the record of atmospheric carbon dioxide, measured from atmospheric
samples and air trapped in
polar ice.
The following are more of interest: — «Winter
Sampling of Shallow Firn Air at the South Pole to Understand Processes Affecting Firn Atmospheric Histories and
Ice Core Gas Records» by Severinghaus (2000), — «Thermal fractionation of air in polar firn by seasonal temperature gradients» by Severinghaus, Grachev & Battle (2001), — «Severinghaus et al. «Fractionation of gases in polar ice during bubble close - off: New constraints from firn air Ne, Kr and Xe observations» by Severinghaus & Battle (2006), but all follow the same line of reasoni
Ice Core Gas Records» by Severinghaus (2000), — «Thermal fractionation of air in
polar firn by seasonal temperature gradients» by Severinghaus, Grachev & Battle (2001), — «Severinghaus et al. «Fractionation of gases in
polar ice during bubble close - off: New constraints from firn air Ne, Kr and Xe observations» by Severinghaus & Battle (2006), but all follow the same line of reasoni
ice during bubble close - off: New constraints from firn air Ne, Kr and Xe observations» by Severinghaus & Battle (2006), but all follow the same line of reasoning.
Uncertainties should decrease closer to near - current dates (e.g. from denser and more accurate
sampling)-- but note that these products also employ different QC and analysis methods, rely to varying degrees on satellite data, on sea -
ice data to constrain
polar SST, and on bias adjustments for historical changes in measurement methods.
The gradual but systematic rise of 1.5 degrees C is best explained by the record of atmospheric carbon dioxide, measured from atmospheric
samples and air trapped in
polar ice.
A geologist can take soil
samples,
sample cores taken from a tropical ocean or
sample cores from beneath the
polar ice caps.