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This anomaly reached a critical point during a 2011 game between Romania and Hungary in Miercurea Ciuc.
The values were lower in the center, and the maximum difference of the gravity anomaly reached approximately 0.3 mGal.
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To the west, the positive thermal anomaly reaches temperatures to up to 170 °C.
However, with the presence of significant groundwater recharge, a temperature anomaly of 4 °C reaches a 25-m depth, and a 2 °C anomaly reaches a depth of only 22 m after 100 years.
The anomaly reaches its peak strength during the postnoon period (1300 1600 LT) after a time lag of around 2 3 h from the time of the maximum electrojet strength (Rush and Richmond 1973).
The impulsive anomalies reach ~24 cm at 5 min after the onset and then decreased gradually for more than 30 min.
When these anomalies reach sufficient magnitude, the scientific discipline falls into a state of crisis that cannot be worked out with current instruments and means (Kuhn 1962).
If the anomalies reach a width of Ψ= 90°, the magnetic field drastically enhances the EAA symmetry relative to the hydrodynamic runs.
The magnetic field prevents narrow heat flux anomalies from affecting the core convection but drastically increases their respective effects when the anomalies reach horizontal extents on the same order as the core radius.
Higher-pressure-gradient anomalies occupy the southeastern, central, northeastern, and western parts attaining a maximum value of 13.8 ppg (0.72 psi/ft), while the southwestern and northwestern corners represent the lower-pressure-gradient anomalies reach 10 ppg (0.52 psi/ft).
Once temperature anomalies reach 2 SDs (∼5 6°C), the melt amplifies almost exponentially.
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