1.4 Fundamentals of Geomagnetism
Case Study 1: South Atlantic Anomaly and Magnetic Field Weakening
- Models/Theories:
- Dynamo Theory (explains Earth's magnetic field generation in the outer core)
- Magnetic Reversal Theory
- Recent Data (2023):
- The South Atlantic Anomaly (SAA), an area of weakening magnetic field intensity, has expanded over the past decade. ESA’s Swarm satellites recorded a field strength drop of ~8% between 1970 and 2023.
- Magnetic north is drifting ~55–60 km per year toward Siberia.
- Spatial Variation:
- The SAA spans parts of South America to southern Africa, showing greatest magnetic field weakness over Brazil and the South Atlantic.
- Temporal Variation:
- The Earth’s magnetic field strength has decreased by nearly 9% over the past 200 years, with localized weakening accelerating recently.
- Source:
- ESA (2023), Nature Geoscience, and DownToEarth ("Geomagnetic Changes and Their Risks", Sept 2023)
- Insight:
- The SAA illustrates a real-time weakening of Earth’s geomagnetic field, potentially linked to pole reversals. It supports the Dynamo Theory and indicates active changes in the outer core dynamics.
Case Study 2: Magnetic Striping at Mid-Ocean Ridges
- Models/Theories:
- Sea-Floor Spreading Model (Vine-Matthews Hypothesis)
- Dynamo Theory
- Recent Data (2023):
- Magnetic surveys in the Mid-Atlantic Ridge show symmetrical striping of normal and reversed magnetic polarity on both sides of the ridge, correlating with known geomagnetic reversals.
- Spatial Variation:
- Patterns of striping are found along all active mid-ocean ridges—Mid-Atlantic Ridge, East Pacific Rise, Carlsberg Ridge in the Indian Ocean.
- Temporal Variation:
- These magnetic anomalies represent over 170 magnetic reversals over the last 180 million years, with a frequency of ~1 reversal every 200,000–300,000 years.
- Source:
- Science Journal, USGS (2023); National Geographic coverage on seafloor spreading and magnetic field behavior.
- Insight:
- Magnetic striping validates the Dynamo Theory and Plate Tectonics, revealing Earth’s internal magnetism imprinted on the ocean floor.
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