The seasonal succession of plankton is an annually repeated process of community assembly
during which all major external factors and internal interactions shaping communities can …

… the value for clear water (0.02 m −1 ), while it can reach values >1 m −1 in brown-water lakes
… “optical winter”. The same applies to suspended solids transported by floods of tributaries. …

… We quantify mass fluxes (F) and the mass of reservoirs (M) related to mountain hydrology
at the global scale based on published literature. All fluxes are estimates that are subject to …

While there is a general sense that lakes can act as sentinels of climate change, their efficacy
has not been thoroughly analyzed. We identified the key response variables within a lake …

This synthesis examines 35 long‐term (5–35 years, mean: 16 years) lake re‐oligotrophication
studies. It covers lakes ranging from shallow (mean depth <5 m and/or polymictic) to deep (…

… the winter but develops thermal stratification from April to November when a warm water layer
(∼10 m) … Water temperature was recorded in 1-m intervals above the thermocline and 5-m …

… W; 4 m asl) with a mean depth of 32.9 m and maximum depth of 65.2 m. Lake Washington
is stratified from early spring until late fall and is mixed entirely during the winter months. The …

… there is a strong climatic gradient including the northern areas having winter sea ice cover.
Offshore is a semipermanent halocline at ~70 m depth and persistent anoxia in deep areas. (c…

… The lake has a surface area of 500 km 2 , a maximum depth of 501 m, a mean depth of
333 m and is free of ice the entire year. The lake starts to stratify in April and by October …

Coastal global oceans are expected to undergo drastic changes driven by climate change
and increasing anthropogenic pressures in coming decades. Predicting specific future …