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#geodynamo — Public Fediverse posts

Live and recent posts from across the Fediverse tagged #geodynamo, aggregated by home.social.

  1. @coreyspowell
    10/
    In short: It’s not an apocalypse; it’s a data corrective. It proves that the engine room of our planet is a highly active, rapidly changing environment, and it took a constellation of advanced satellites sixteen years of data-crunching to finally reveal what happened right under our feet.

    #Geophysics
    #Geomagnetism
    #EarthsCore
    #Geodynamics
    #OuterCore
    #Geodynamo
    #ESASwarm
    #CryoSat
    #SatelliteData
    #EarthObservation
    #GeomagneticField
    #WorldMagneticModel
    #WMM

  2. @coreyspowell
    10/
    In short: It’s not an apocalypse; it’s a data corrective. It proves that the engine room of our planet is a highly active, rapidly changing environment, and it took a constellation of advanced satellites sixteen years of data-crunching to finally reveal what happened right under our feet.

    #Geophysics
    #Geomagnetism
    #EarthsCore
    #Geodynamics
    #OuterCore
    #Geodynamo
    #ESASwarm
    #CryoSat
    #SatelliteData
    #EarthObservation
    #GeomagneticField
    #WorldMagneticModel
    #WMM

  3. @coreyspowell
    10/
    In short: It’s not an apocalypse; it’s a data corrective. It proves that the engine room of our planet is a highly active, rapidly changing environment, and it took a constellation of advanced satellites sixteen years of data-crunching to finally reveal what happened right under our feet.

    #Geophysics
    #Geomagnetism
    #EarthsCore
    #Geodynamics
    #OuterCore
    #Geodynamo
    #ESASwarm
    #CryoSat
    #SatelliteData
    #EarthObservation
    #GeomagneticField
    #WorldMagneticModel
    #WMM

  4. @coreyspowell
    10/
    In short: It’s not an apocalypse; it’s a data corrective. It proves that the engine room of our planet is a highly active, rapidly changing environment, and it took a constellation of advanced satellites sixteen years of data-crunching to finally reveal what happened right under our feet.

    #Geophysics
    #Geomagnetism
    #EarthsCore
    #Geodynamics
    #OuterCore
    #Geodynamo
    #ESASwarm
    #CryoSat
    #SatelliteData
    #EarthObservation
    #GeomagneticField
    #WorldMagneticModel
    #WMM

  5. @coreyspowell
    10/
    In short: It’s not an apocalypse; it’s a data corrective. It proves that the engine room of our planet is a highly active, rapidly changing environment, and it took a constellation of advanced satellites sixteen years of data-crunching to finally reveal what happened right under our feet.

    #Geophysics
    #Geomagnetism
    #EarthsCore
    #Geodynamics
    #OuterCore
    #Geodynamo
    #ESASwarm
    #CryoSat
    #SatelliteData
    #EarthObservation
    #GeomagneticField
    #WorldMagneticModel
    #WMM

  6. Earth’s #geodynamo has operated for over 3.5 billion years.

    The #magnetic field is currently powered by thermocompositional convection in the outer core, which involves the release of light elements and latent heat as the inner core solidifies.

    However, since the inner core nucleated no more than 1.5 billion years ago, the early dynamo could not rely on these buoyancy sources and an alternative mechanism was required to sustain the geodynamo.

    #Earth #planets
    astrobiology.com/2024/09/therm

  7. Wann entstand das schützende Magnetfeld unseres Planeten – und wie stark war es? Eine überraschende Antwort liefern nun 3,7 Milliarden Jahre alte Gesteine aus Grönland. #Erdmagnetfeld #Magnetfeld #Erdgeschichte #Geologie #Geodynamo
    scinexx.de/news/geowissen/ur-m

  8. Earth’s innermost region is separated into two major components: a solid #inner #core that measures about 750 miles in radius and sits within the #outer #core, which is a 1,300-mile-thick layer of liquid metal.
    Due to its remote location 1,800 miles under our feet, the core has long evaded easy observation, though scientists can peer at some of its hidden features by recording seismic waves from earthquakes that pass through this enigmatic area.
    Past studies with seismic waves have offered tantalizing hints that the inner core might itself contain a distinct core, though the size and nature of this potential “fifth layer” of Earth has remained a matter of debate. 
    Now, Thanh-Son Phạm and Hrvoje Tkalčić, a pair of researchers at The Australian National University, have used “a previously unobserved and unutilized class of seismological observations” to expose the #IMIC, which they say “could be a fossilized record of a significant global event from the past,” according to a study published on Tuesday in Nature Communications.
    “Earth’s #inner #core ( #IC ), which accounts for less than 1% of the Earth’s volume, is a time capsule of our planet’s history,” said Phạm and Tkalčić in the study.
    “As the IC grows, the latent heat and light elements released by the solidification process drive the convection of the liquid #outer core, which, in turn, maintains the #geodynamo,” referring to the mechanism that generates Earth’s #magnetic field.  

    vice.com/en/article/4axkwj/ear

  9. Earth’s innermost region is separated into two major components: a solid #inner #core that measures about 750 miles in radius and sits within the #outer #core, which is a 1,300-mile-thick layer of liquid metal.
    Due to its remote location 1,800 miles under our feet, the core has long evaded easy observation, though scientists can peer at some of its hidden features by recording seismic waves from earthquakes that pass through this enigmatic area.
    Past studies with seismic waves have offered tantalizing hints that the inner core might itself contain a distinct core, though the size and nature of this potential “fifth layer” of Earth has remained a matter of debate. 
    Now, Thanh-Son Phạm and Hrvoje Tkalčić, a pair of researchers at The Australian National University, have used “a previously unobserved and unutilized class of seismological observations” to expose the #IMIC, which they say “could be a fossilized record of a significant global event from the past,” according to a study published on Tuesday in Nature Communications.
    “Earth’s #inner #core ( #IC ), which accounts for less than 1% of the Earth’s volume, is a time capsule of our planet’s history,” said Phạm and Tkalčić in the study.
    “As the IC grows, the latent heat and light elements released by the solidification process drive the convection of the liquid #outer core, which, in turn, maintains the #geodynamo,” referring to the mechanism that generates Earth’s #magnetic field.  

    vice.com/en/article/4axkwj/ear

  10. Earth’s innermost region is separated into two major components: a solid #inner #core that measures about 750 miles in radius and sits within the #outer #core, which is a 1,300-mile-thick layer of liquid metal.
    Due to its remote location 1,800 miles under our feet, the core has long evaded easy observation, though scientists can peer at some of its hidden features by recording seismic waves from earthquakes that pass through this enigmatic area.
    Past studies with seismic waves have offered tantalizing hints that the inner core might itself contain a distinct core, though the size and nature of this potential “fifth layer” of Earth has remained a matter of debate. 
    Now, Thanh-Son Phạm and Hrvoje Tkalčić, a pair of researchers at The Australian National University, have used “a previously unobserved and unutilized class of seismological observations” to expose the #IMIC, which they say “could be a fossilized record of a significant global event from the past,” according to a study published on Tuesday in Nature Communications.
    “Earth’s #inner #core ( #IC ), which accounts for less than 1% of the Earth’s volume, is a time capsule of our planet’s history,” said Phạm and Tkalčić in the study.
    “As the IC grows, the latent heat and light elements released by the solidification process drive the convection of the liquid #outer core, which, in turn, maintains the #geodynamo,” referring to the mechanism that generates Earth’s #magnetic field.  

    vice.com/en/article/4axkwj/ear

  11. Earth’s innermost region is separated into two major components: a solid #inner #core that measures about 750 miles in radius and sits within the #outer #core, which is a 1,300-mile-thick layer of liquid metal.
    Due to its remote location 1,800 miles under our feet, the core has long evaded easy observation, though scientists can peer at some of its hidden features by recording seismic waves from earthquakes that pass through this enigmatic area.
    Past studies with seismic waves have offered tantalizing hints that the inner core might itself contain a distinct core, though the size and nature of this potential “fifth layer” of Earth has remained a matter of debate. 
    Now, Thanh-Son Phạm and Hrvoje Tkalčić, a pair of researchers at The Australian National University, have used “a previously unobserved and unutilized class of seismological observations” to expose the #IMIC, which they say “could be a fossilized record of a significant global event from the past,” according to a study published on Tuesday in Nature Communications.
    “Earth’s #inner #core ( #IC ), which accounts for less than 1% of the Earth’s volume, is a time capsule of our planet’s history,” said Phạm and Tkalčić in the study.
    “As the IC grows, the latent heat and light elements released by the solidification process drive the convection of the liquid #outer core, which, in turn, maintains the #geodynamo,” referring to the mechanism that generates Earth’s #magnetic field.  

    vice.com/en/article/4axkwj/ear

  12. Earth’s innermost region is separated into two major components: a solid #inner #core that measures about 750 miles in radius and sits within the #outer #core, which is a 1,300-mile-thick layer of liquid metal.
    Due to its remote location 1,800 miles under our feet, the core has long evaded easy observation, though scientists can peer at some of its hidden features by recording seismic waves from earthquakes that pass through this enigmatic area.
    Past studies with seismic waves have offered tantalizing hints that the inner core might itself contain a distinct core, though the size and nature of this potential “fifth layer” of Earth has remained a matter of debate. 
    Now, Thanh-Son Phạm and Hrvoje Tkalčić, a pair of researchers at The Australian National University, have used “a previously unobserved and unutilized class of seismological observations” to expose the #IMIC, which they say “could be a fossilized record of a significant global event from the past,” according to a study published on Tuesday in Nature Communications.
    “Earth’s #inner #core ( #IC ), which accounts for less than 1% of the Earth’s volume, is a time capsule of our planet’s history,” said Phạm and Tkalčić in the study.
    “As the IC grows, the latent heat and light elements released by the solidification process drive the convection of the liquid #outer core, which, in turn, maintains the #geodynamo,” referring to the mechanism that generates Earth’s #magnetic field.  

    vice.com/en/article/4axkwj/ear

  13. The paper is still not ready, but some may find interest in the #scientific #poster about #geodynamo #reversals simulated with a rare event method.
    doi.org/10.6084/m9.figshare.21

  14. The paper "The inherent instability of axisymmetric magnetostrophic dynamo models", written by Colin Hardy, Phil Livermore and myself, is now published online in the journal Geophysical & Astrophysical Fluid Dynamics.

    Link (open access): tandfonline.com/doi/full/10.10

    Below I will give a (relatively) non-technical explanation of some background of our paper.

    #geomagnetism #geodynamo #EarthsCore #magnetohydrodynamics #magnetostrophic

  15. The paper "The inherent instability of axisymmetric magnetostrophic dynamo models", written by Colin Hardy, Phil Livermore and myself, is now published online in the journal Geophysical & Astrophysical Fluid Dynamics.

    Link (open access): tandfonline.com/doi/full/10.10

    Below I will give a (relatively) non-technical explanation of some background of our paper.

    #geomagnetism #geodynamo #EarthsCore #magnetohydrodynamics #magnetostrophic

  16. The paper "The inherent instability of axisymmetric magnetostrophic dynamo models", written by Colin Hardy, Phil Livermore and myself, is now published online in the journal Geophysical & Astrophysical Fluid Dynamics.

    Link (open access): tandfonline.com/doi/full/10.10

    Below I will give a (relatively) non-technical explanation of some background of our paper.

    #geomagnetism #geodynamo #EarthsCore #magnetohydrodynamics #magnetostrophic

  17. The paper "The inherent instability of axisymmetric magnetostrophic dynamo models", written by Colin Hardy, Phil Livermore and myself, is now published online in the journal Geophysical & Astrophysical Fluid Dynamics.

    Link (open access): tandfonline.com/doi/full/10.10

    Below I will give a (relatively) non-technical explanation of some background of our paper.

    #geomagnetism #geodynamo #EarthsCore #magnetohydrodynamics #magnetostrophic

  18. The paper "The inherent instability of axisymmetric magnetostrophic dynamo models", written by Colin Hardy, Phil Livermore and myself, is now published online in the journal Geophysical & Astrophysical Fluid Dynamics.

    Link (open access): tandfonline.com/doi/full/10.10

    Below I will give a (relatively) non-technical explanation of some background of our paper.

    #geomagnetism #geodynamo #EarthsCore #magnetohydrodynamics #magnetostrophic

  19. First paper of a PhD student in our team.
    It is a preprint #OpenAccess and #OpenReview paper, so you can comment online.

    It is about correcting for alignement with rotation axis of the main inertial axis of the Earth in a #simulation of Mantle #convection. We need this to get plausible heat flux maps for later #geodynamo simulations.

    egusphere.copernicus.org/prepr