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National Oceanic and Atmospheric Administration

Monday, March 18, 2024 19:50:20

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NOAA Scales mini

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Space Weather Conditions
24-Hour Observed Maximums
R
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S
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G
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Latest Observed
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S
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R1-R2 --
R3-R5 --
S1 or greater --
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R1-R2 --
R3-R5 --
S1 or greater --
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R1-R2 --
R3-R5 --
S1 or greater --
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R
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Current Space Weather Conditions
R1 (Minor) Radio Blackout Impacts
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HF Radio: Weak or minor degradation of HF radio communication on sunlit side, occasional loss of radio contact.
Navigation: Low-frequency navigation signals degraded for brief intervals.
More about the NOAA Space Weather Scales

Geospace Magnetosphere Movies

Velocity

Geospace 2d Cut Planes - Velocity

Density

Geospace 2d Cut Planes - Density

Pressure

Geospace 2d Cut Planes - Pressure

The Geospace Magnetosphere Movies display 2d cut planes of Earth's magnetosphere from the Geospace model output for three different plasma parameters (velocity, density, and pressure). For each plasma parameter, equatorial (x-y plane) and noon-midnight magnetic meridian (x-z plane) cut planes are plotted in GSM coordinates. The animations show the model forecast, where the lead time depends on the solar wind speed, as well as the previous two hours for context.

2D cut planes of the magnetosphere are useful for providing a large-scale, global context of activity in the near-Earth environment. These plots assist forecasters in developing situational awareness and are useful for assessing the validity of the Geospace model. 

For additional space weather products generated using output from the Geospace model, see the following pages:

This product uses output generated by the University of Michigan’s Geospace model that consists of several components in their Space Weather Modeling Framework (SWMF). The Geospace model is a first-principles physics based model which includes three components:

  • The University of Michigan’s BATS-R-US magnetohydrodynamic (MHD) model of the magnetosphere
  • The Ridley Ionosphere electrodynamics Model (RIM) developed at Michigan
  • The Rice Convection Model (RCM), an inner magnetosphere ring-current model developed at Rice University

The Geospace Magnetosphere Movies represent the first generation of operational space weather products derived from the Geospace model, a model which includes both global and regional short-term predictions of geomagnetic activity. Other operational space weather products generated using output from the Geospace model include the Geospace Geomagnetic Activity Plot and the Geospace Ground Magnetic Perturbation Maps.

The Geospace model (v1.0) first went operational in October 2016, and during its first year in operations the model achieved initial success in providing forecaster guidance on levels of regional geomagnetic activity, short-term predictions of geomagnetic indices, and making data available to customers over the web.

As of November 8, 2017, the operational product was driven by the Geospace model (v 1.5). This first upgrade to the Geospace model included some minor physics improvements, new output parameters, increased model robustness, and a switch to a different operational high-performance computer (Cray). In addition, this version of the model allowed for the model to perform a warm restart from a previous output file during times when there was a solar wind data gap of greater than 15 minutes and less than 2 hours. Solar wind data gaps of greater than 2 hours continue to trigger the model to perform a cold restart, which can require 2-3 hours for the model to return to equilibrium. 

As of January 25, 2021, the operational products are now being driven by the Geospace model (v2.0). In this upgrade to the Geospace model, the most significant changes are: increased resolution for solving the MHD equations in targeted regions of the grid, moving from ~ 1 million to 1.9 million grid cells; improved auroral oval specification and more realistic representation of magnetospheric current systems; new tail composition settings to better represent current systems responsible for the Disturbance Storm Time index – Dst; a new method for calculating a predicted estimated Kp (global geomagnetic activity index) based on magnetic variations from the Geospace model processed by a Kp algorithm that is the same as SWPC uses for calculating Kp from ground-based magnetometer stations.

The model output files for the last 48 hours can be accessed here