Seasonal variations in Canadian Lakes
Winter - lakes covered by ice, blocks oxygen from entering, acts as insulator
Layers: Epilimnion (zero degrees), Thermocline, Hypolimnion (four degrees)
Spring - Ice melts, oxygen unblocked
Wind makes waves, increasing surface area and oxygen dissolving rate
Spring turnover: Surface water sinks, holding lots of oxygen
Summer - Upper layers warm, lower layers cold
Little oxygen transfer, hypolimnion still has most oxygen
Warm epilimnion means less dissolved oxygen
Fall - Surface water cools
Fall turnover: Renews oxygen in lower levels