They looked at global temperature anomalies — deviations from an average or standard temperature — for 73 sites distributed across the planet, using fossils in
sediments as a proxy for temperature.
Not exact matches
As there is no explanation as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that proxy sea floor sediment data should be adjusted («corrected») for sea water temperatur
As there is no explanation
as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that proxy sea floor sediment data should be adjusted («corrected») for sea water temperatur
as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that
proxy sea floor
sediment data should be adjusted («corrected»)
for sea water
temperature.
If there is a separate paper discussing the scientific merits of using post-1720
sediments from this region
as a
temperature proxy, then it meets Mann's criteria
for inclusion.
The earlier data comes from some sort of
proxy analysis (ice cores, tree rings,
sediments, etc.) While we know these
proxies generally change with
temperature, there are still a lot of questions
as to their accuracy and, perhaps more importantly
for us here, whether they vary linearly or have any sort of attenuation of the peaks.
As there is no explanation as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that proxy sea floor sediment data should be adjusted («corrected») for sea water temperatur
As there is no explanation
as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that proxy sea floor sediment data should be adjusted («corrected») for sea water temperatur
as to how climate changes could possibly affect the intensity of the earth's magnetic field, it was decided that it would be easier to believe that
proxy sea floor
sediment data should be adjusted («corrected»)
for sea water
temperature.