Définition : The top-most layer in a thermally stratified lake, occurring above the deeper hypolimnion. It is warmer and typically has a higher pH and dissolved oxygen concentration than the hypolimnion
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : The top-most layer in a thermally stratified lake, occurring above the deeper hypolimnion. It is warmer and typically has a higher pH and dissolved oxygen concentration than the hypolimnion
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : The top-most layer in a thermally stratified lake, occurring above the deeper hypolimnion. It is warmer and typically has a higher pH and dissolved oxygen concentration than the hypolimnion
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
Définition : The top-most layer in a thermally stratified lake, occurring above the deeper hypolimnion. It is warmer and typically has a higher pH and dissolved oxygen concentration than the hypolimnion
Définition : A lake from which there is no outflow of water, either on the surface as rivers, or underground by flow or diffusion through rock or permeable material.
