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in previous experiments. The present results demonstrate the validity of the retrieval algorithm for moderately to extremely dry soils. The ESTAR measurements along with ancillary data were used to create soil moisture maps of the entire region.
variation may thus be expected in more realistic, numerical simulations of the geodynamo and may provide an important constraint on those models 12–14. A The last two geomagnetic polarity reversals recorded in high-deposition-rate sediment drifts. dependency of geomagnetic polarity transition durations. A statistical analysis of magnetic fields from some(More)
variation may thus be expected in more realistic, numerical simulations of the geodynamo and may provide an important constraint on those models 12–14. A The last two geomagnetic polarity reversals recorded in high-deposition-rate sediment drifts. dependency of geomagnetic polarity transition durations. A statistical analysis of magnetic fields from some(More)
> BLOCKIN?6?6:67 ≅ may result from straightforward geometrical constraints. This variation may thus be expected in more realistic, numerical simulations of the geodynamo and may provide an important constraint on those models 12–14. A 40 Ar/ 39 Ar incremental heating analyses of lavas. The last two geomagnetic polarity reversals recorded in(More)
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