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Early Limnology: Temperature Profiles
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Lake Zones Zones are dynamic! Input of heat Mixing forces
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The stratification and mixing cycle of an average-sized, temperate lake
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Stratification and Mixing
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The Whole Cycle in One Confusing Figure!
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Factors that influence stratification pattern Heating / Density Wind / Waves Depth Surface Area Topography / Location / Exposure
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The Family of Lake Cycles Temperature Incident Solar Radiation
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The Family of Lake Cycles
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Amictic Perennially ice-covered Inversely stratified
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The Family of Lake Cycles
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Cold Monomictic Water temperature never exceeds 4 C Ice-covered for most of the year = inversely stratified One period of free circulation in summer at or below 4 C
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The Family of Lake Cycles
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Dimictic
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The Family of Lake Cycles
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Warm Monomictic Circulates once in winter at or above 4 C Directly stratified for the rest of the year Not ice covered
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The Family of Lake Cycles
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Oligomictic Stable, direct stratification most of the year Circulation at irregular intervals (scale of years) during cool periods
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The Family of Lake Cycles
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Polymictic Frequent periods of mixing per year Not ice-covered
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Cold Polymictic Equatorial, high elevation Hovering around 4 C Intense heat during day (stratification) Intense cooling at night (mixing)
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Warm Polymictic Warm throughout (i.e., well above 4 C) Sometimes get intense heating of epilimnion = development of weak stratification.
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4 C is IMPORTANT
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Holomixis: Circulation occurs throughout the entire water column. Meromixis: Primary water mass never mixes with the lower portion.
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Stratification in meromictic lakes Monimolimnion: deep stratum, high salinity Chemolimnion: strong salinity gradient Mixolimnion: upper stratum (i.e., epi-, meta-, and hypolimnion)
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How does the salt get there? Ectogenic meromixis Crenogenic meromixis Biogenic meromixis
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Consequences of meromixis Monimolimnion = Dead Zone Chemolimnion = Heat Trap
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More Blue More Red Frequency Wavelength
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Consequences of meromixis Hot Lake, north-central WA On top of epsom salt excavation High MgSO 4 in monimolimnion Temperature in monimolimnion can get to 50 C!
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Why Lake Circulation Matters: Lake Nyos Gas Disaster
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Lake Nyos Degassing Project Pipe is 203 m long and 14.5 cm in diameter. Upper end attached to raft and supported by lines to shore.
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Oxygen Light Temperature
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Patterns along the “river continuum” Oxygen Light Temperature
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Temperature along streams
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Temperature fluctuations along the streams
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Effect of Groundwater on Stream Temperature: Nyack Floodplain, MT
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Oxygen along streams DO in unpolluted, flowing water usually at or near saturation, and concentrations are of little biological significance.
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