hypolimnion

listen to the pronunciation of hypolimnion
İngilizce - Türkçe
hipolimniyon
İngilizce - İngilizce
The perpetually cold layer of water that lies beneath the thermocline of a thermally stratified lake
The lowest layer in a thermally stratified lake or reservoir This layer consists of colder, more dense water, has a constant temperature and no mixing occurs
Bottom waters of a thermally stratified lake , The hypolimnion of a eutrophic lake is usually low or lacking in oxygen
The layer of water below the thermocline in a fresh water lake, as opposed to the epilimnion
The cooler, lower most layer of water in a thermally stratified lake
The deep layer of a lake below the thermocline and removed from surface influences such as direct heating by sunlight and aeration by vertical circulation
The lowest layer in a thermally stratified lake or reservoir This layer consists of colder, more dense water, and has a constant temperature where no mixing occurs
The lowermost layer of lake water that is colder and more stagnant than overlying layers
The cold dense lower layer of water that occurs in a lake during summer stratification
The colder, deep layer of a lake lying below the metalimnion and removed from surface influences
The lowermost, non-circulating layer of cold water in a thermally stratified lake; usually deficient of oxygen
Bottom waters of a thermally stratified lake The hypolimnion of a eutrophic lake is usually low or lacking in oxygen
the cold, dense lower waters of a summer stratified lake Oxygen depletion is a common problem in the hypolimnion of eutrophic lakes
The colder, lower, denser zone of water in a lake, separated by the fairly thin thermocline zone, from the upper, warmer, less dense zone, the epilimnion
The lower layer of a lake
The layer of water in a thermally stratified lake that lies below the thermocline, is noncirculating, and remains perpetually cold
lower later of water in a lake or pond (below thermocline), which maintains constant temperature (Henry and Heinke, 1996)
The hypolimnion is the lowers layer of a lentic (standing water) ecosystem
{i} (in thermally stratified lakes) non-circulating layer of water located below the thermocline and characterized by uniformly cold temperatures and low oxygen levels
The region of a body of water that extends from the thermocline to the bottom and is essentially removed from major surface influences during periods of thermal stratification