Methane (CH4) produced in anoxic sediments plays a significant role in the carbon economy of many lakes and reservoirs. CH4 released from sediments first crosses the …
Field data and numerical modeling were used to investigate the effects of the riverine inflows on the seasonality of the lake mean temperature, thermal structure, and basin‐scale internal …
In eutrophic lakes and reservoirs, reduced mixing during stratified conditions limits oxygen (O 2) supply to the hypolimnion (that is, bottom waters). In the absence of an O 2 supply …
Lateral intrusions flowing from the boundaries of lakes and oceans might influence basin‐ scale distributions of heat, chemical solutes, sediments, and organisms. Here, observations …
SM Henderson - Journal of Geophysical Research: Oceans, 2016 - Wiley Online Library
Internal seiches, which supply the energy responsible for mixing many lakes, are often modeled as vertically standing waves. However, recent observations of vertical seiche …
In lakes and reservoirs, the bottom boundary layer (BBL) mediates chemical fluxes between sediments and the overlying water column. At the internal shoreline, where the thermocline …
Periodic winds acting on a stratified waterbody can amplify normal modes of motion and enhance the basin-scale circulation via resonance. Here, we use idealized large-eddy …
In a stratified lake, where an internal seiche maintained an oscillating bottom boundary layer (BBL), processes including strain‐induced periodic stratification (SIPS), a downslope mean …