R S Sternberg
Biographic Data
| ID | 5598267 |
|---|---|
| NAME | R S Sternberg |
| GIVEN NAMES | R S |
| FAMILY NAME | Sternberg |
| SIGNATURE | STERNBERG R S |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 10 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1983 |
| LATEST PUBLICATION YEAR | 1992 |
| H-INDEX | 2 |
Implications of Dipole Moment Secular Variation from 50,000–10,000 Years for the Radiocarbon Record
Sparse paleointensity data from 10–50 ka suggest that the average dipole moment (DM) was 50–75% of the average of 8.67 μ 10 22 A m 2 for the past 5 Ma, and 8.75 μ 10 22 for the past 12 ka. A linear ramp function, increasing the DM from 4 to 8.75 μ 10 22 A m 2 between 50–10 ka BP, generates a total 14 C inventory of 126 dpm/cm e 2 , agreeing very well with an inventory assay of 128 dpm/cm e 2 , which includes 14 C in sediments. With the Lingenfelt…
Atmospheric Radiocarbon
The geomagnetic field is one of the major physical fields of the earth. Because its source is fluid motion in the outer core, it exhibits temporal changes, called secular variation, which are quite rapid compared to most geologic phenomena. The prehistoric secular variation is usually inferred from paleomagnetic data. We will discuss here how changes in the atmospheric 14 C content can be used to gain additional insight into the behavior of the d…
Modeling of Atmospheric Radiocarbon Fluctuations for the Past Three Centuries
Relatively precise quantitative observations of geophysical parameters are available to evaluate the fluctuations of atmospheric 14 C activity during the past three centuries. As reviewed by Damon, Lerman, and Long (1978), these fluctuations seem to result from three factors: 1) changes in the earth's dipole magnetic field intensity, which has been decreasing since the first measurements by Gauss (McDonald and Gunst, 1968); 2) solar modulation of…
Modeling of Atmospheric Radiocarbon Fluctuations for the Past Three Centuries
Relatively precise quantitative observations of geophysical parameters are available to evaluate the fluctuations of atmospheric 14 C activity during the past three centuries. As reviewed by Damon, Lerman, and Long (1978), these fluctuations seem to result from three factors: 1) changes in the earth's dipole magnetic field intensity, which has been decreasing since the first measurements by Gauss (McDonald and Gunst, 1968); 2) solar modulation of…
Implications of Dipole Moment Secular Variation from 50,000–10,000 Years for the Radiocarbon Record
Sparse paleointensity data from 10–50 ka suggest that the average dipole moment (DM) was 50–75% of the average of 8.67 μ 10 22 A m 2 for the past 5 Ma, and 8.75 μ 10 22 for the past 12 ka. A linear ramp function, increasing the DM from 4 to 8.75 μ 10 22 A m 2 between 50–10 ka BP, generates a total 14 C inventory of 126 dpm/cm e 2 , agreeing very well with an inventory assay of 128 dpm/cm e 2 , which includes 14 C in sediments. With the Lingenfelt…
Atmospheric Radiocarbon
The geomagnetic field is one of the major physical fields of the earth. Because its source is fluid motion in the outer core, it exhibits temporal changes, called secular variation, which are quite rapid compared to most geologic phenomena. The prehistoric secular variation is usually inferred from paleomagnetic data. We will discuss here how changes in the atmospheric 14 C content can be used to gain additional insight into the behavior of the d…
Modeling of Atmospheric Radiocarbon Fluctuations for the Past Three Centuries
Relatively precise quantitative observations of geophysical parameters are available to evaluate the fluctuations of atmospheric 14 C activity during the past three centuries. As reviewed by Damon, Lerman, and Long (1978), these fluctuations seem to result from three factors: 1) changes in the earth's dipole magnetic field intensity, which has been decreasing since the first measurements by Gauss (McDonald and Gunst, 1968); 2) solar modulation of…
Implications of Dipole Moment Secular Variation from 50,000–10,000 Years for the Radiocarbon Record
Sparse paleointensity data from 10–50 ka suggest that the average dipole moment (DM) was 50–75% of the average of 8.67 μ 10 22 A m 2 for the past 5 Ma, and 8.75 μ 10 22 for the past 12 ka. A linear ramp function, increasing the DM from 4 to 8.75 μ 10 22 A m 2 between 50–10 ka BP, generates a total 14 C inventory of 126 dpm/cm e 2 , agreeing very well with an inventory assay of 128 dpm/cm e 2 , which includes 14 C in sediments. With the Lingenfelt…
Earth's magnetic field (3 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Geomagnetism and Paleomagnetism Studies (3 works) · Magnetic field (3 works) · Paleontology (3 works) · Physics (3 works) · Radiocarbon dating (3 works) · Archaeology and ancient environmental studies (2 works) · Astrophysics (2 works)