Electron heat flux in the magnetosheath is shaped by magnetic field draping, increases with field strength, and is limited by whistler instability thresholds.
However, we find that there is no increase in whistler wave activity when the heat flux is close to the instability thresholds
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Electron Heat Flux and Whistler Instability in the Earth's Magnetosheath
Electron heat flux in the magnetosheath is shaped by magnetic field draping, increases with field strength, and is limited by whistler instability thresholds.