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Article
Open AccessIntradecadal variations in length of day and their correspondence with geomagnetic jerks
Earth’s core oscillations and magnetic field inside the liquid outer core cannot be observed directly from the surface, we can infer these information from the intradecadal variations in Earth’s rotation rate ...
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Article
Detection of Antarctic oscillation signals in Earth’s oblateness variations
Variations of Earth’s oblateness (J 2) reflect a large scale mass redistribution within the Earth system. The climate effect causing J 2 interannual variations is s...
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Article
Open AccessRecovery of the 6-year signal in length of day and its long-term decreasing trend
There is a significant 6-year oscillation signal (called 6-year signal in this paper) existing in the interannual variations of length of day (LOD). It is unclear to understand its nature variation features. T...