Why Sporadic-E clouds of intensely ionized patches in the E layer (about 60-70 miles up) form most often in a broad season centered on the summer solstice, with a weaker secondary peak near the winter solstice. In the northern hemisphere that means a strong May-through-August season for 10, 6 and sometimes 2 meters. The mechanism is tied to wind shear and meteoric ionization rather than to solar flux, so Es appears even at sunspot minimum.
Watch out The equinox answers describe the pattern for F2-layer DX and transequatorial propagation, which favor spring and fall, not Es. The winter-solstice choice names the real but much weaker secondary Es peak.
Sporadic-E = summer sizzle: the big 6 meter season peaks around the June solstice.