Oxygen falls as water warms
The oxygen readout uses a standard curve fit for fresh water at sea level: DO = 14.652 minus 0.41022 T plus 0.007991 T squared minus 0.000077774 T cubed, with T in degrees Celsius. It gives about 9 mg/L at 20 °C and about 7.4 mg/L at 30 °C.
That is the most the water can hold when fully mixed with air. Real tanks run a little below it, which is why bubbling never stops.
Demand rises too
Root respiration speeds up with temperature. Biologists often use a Q10 of about 2, meaning the rate doubles for every 10 °C rise. The demand readout uses that rule of thumb relative to 20 °C, so it is a simplified teaching model rather than a measurement.