Very Slow Rotation of Earth's Inner Core From 1971 to 1974

Abstract The rate that Earth's inner core rotates relative to the mantle and crust has been debated for decades. Nonrotational processes, including internal deformation and flow in the outer core, have also been proposed to explain observed seismic changes. The observed changes thus far have be...

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Main Author: John E. Vidale
Format: Article
Language:English
Published: Wiley 2019-08-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2019GL083774
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author John E. Vidale
author_facet John E. Vidale
author_sort John E. Vidale
collection DOAJ
description Abstract The rate that Earth's inner core rotates relative to the mantle and crust has been debated for decades. Nonrotational processes, including internal deformation and flow in the outer core, have also been proposed to explain observed seismic changes. The observed changes thus far have been so inconsistent and weak as to hamper convincing interpretation. Here, we examine waves backscattered from within the inner core, which can more robustly evaluate rotation, from two nuclear tests 3 years apart in Novaya Zemlya, Russia. We have extended our previous analysis of these explosions using precise station corrections and the full Large Aperture Seismic Array, thus revealing how the time shifts depend on slowness and lag time and halving our rotation rate estimate. Our derived 0.07°/year inner core superrotation rate from 1971 to 1974 is more robust and slower than most previous estimates and may require interesting reinterpretations of localized signals previously interpreted as inner core rotation.
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spelling doaj-art-6bf2e5a68e0b4c44a51cf01c33cfa88f2025-08-20T02:12:20ZengWileyGeophysical Research Letters0094-82761944-80072019-08-0146169483948810.1029/2019GL083774Very Slow Rotation of Earth's Inner Core From 1971 to 1974John E. Vidale0Department of Earth Sciences University of Southern California Los Angeles CA USAAbstract The rate that Earth's inner core rotates relative to the mantle and crust has been debated for decades. Nonrotational processes, including internal deformation and flow in the outer core, have also been proposed to explain observed seismic changes. The observed changes thus far have been so inconsistent and weak as to hamper convincing interpretation. Here, we examine waves backscattered from within the inner core, which can more robustly evaluate rotation, from two nuclear tests 3 years apart in Novaya Zemlya, Russia. We have extended our previous analysis of these explosions using precise station corrections and the full Large Aperture Seismic Array, thus revealing how the time shifts depend on slowness and lag time and halving our rotation rate estimate. Our derived 0.07°/year inner core superrotation rate from 1971 to 1974 is more robust and slower than most previous estimates and may require interesting reinterpretations of localized signals previously interpreted as inner core rotation.https://doi.org/10.1029/2019GL083774core rotationarray seismologybeam formingtime‐dependent seismologyinner corenuclear tests
spellingShingle John E. Vidale
Very Slow Rotation of Earth's Inner Core From 1971 to 1974
Geophysical Research Letters
core rotation
array seismology
beam forming
time‐dependent seismology
inner core
nuclear tests
title Very Slow Rotation of Earth's Inner Core From 1971 to 1974
title_full Very Slow Rotation of Earth's Inner Core From 1971 to 1974
title_fullStr Very Slow Rotation of Earth's Inner Core From 1971 to 1974
title_full_unstemmed Very Slow Rotation of Earth's Inner Core From 1971 to 1974
title_short Very Slow Rotation of Earth's Inner Core From 1971 to 1974
title_sort very slow rotation of earth s inner core from 1971 to 1974
topic core rotation
array seismology
beam forming
time‐dependent seismology
inner core
nuclear tests
url https://doi.org/10.1029/2019GL083774
work_keys_str_mv AT johnevidale veryslowrotationofearthsinnercorefrom1971to1974