The solar radiation reaching the top of the atmosphere (in unit area and unit time)
Laminar flow
Smooth, even flow, where the fluid moves in parallel layers and there is a minimal amount of mixing between layers
Turbulent flow
Chaotic movement, where the fluid contains swirling regions called EDDIES and there is significant mixing of the fluid
Holomictic lakes
Lakes that undergo complete mixing from top to bottom at least once a year, typically during the spring and fall turnovers
Types of holomictic lakes
Polymictic (mixing many times annually)
Cold monomictic (mixing once annually; exhibiting negative stratification)
Warm monomictic (mixing once annually; exhibiting positive stratification)
Dimictic (mixing twice annually)
Oligomictic (mixing less than once annually)
Meromictic lakes
Lakes that do not undergo complete mixing of their water column annually
Amictic lakes
The coldest lakes, are covered in ice permanently, and as such do not experience any circulation
Destratification
The process of disrupting thermal layers or chemical layers in a body of water, particularly in lakes and reservoirs
Types of destratifiers
Air injection
Mechanical axial flow pumps
Thermal stratification
Temperature layering
Seasonal variations
Ecological impact
Nutrient cycling
Destratification
Mixing of layers
Nutrient redistribution
Temperature equalization
Cold monomictic lakes
Lakes with ice covering the surface most of the year, without ice during the summer, but with temperatures that never exceed 4ºC
Cold polymictic lakes
Lakes covered with ice for part of the year, without ice during the summer, with temperatures above 4ºC and stratified at least during the day
Discontinuous cold polymictic lakes
Lakes covered with ice for part of the year, free of ice above 4ºC, stratified during the summer, but with interruption of stratification and total circulation at irregular intervals
Dimictic lakes
Lakes covered with ice for part of year, stratified during the summer, with circulation during periods of transition between these two states of vertical organization
Warm monomictic lakes
No ice cover at any time of the year, stable stratification during part of the year and vertical mixing during one period of the year