Inland water carbon (C) sequestration rates play a potentially important role in the balance
between C supplies from the atmosphere and associated watersheds and the net demand of …

Recent advances in high‐frequency environmental sensing and statistical approaches have
greatly expanded the breadth of knowledge regarding aquatic ecosystem metabolism—the …

Shallow lakes, the most prevalent type of freshwater ecosystems, can shift between clear
states with macrophyte dominance and turbid, phytoplankton-dominated states. Such …

Small water systems are important hotspots of greenhouse gas (GHG) emission, but
estimates are poorly constrained as data are scarce. Small ponds are often constructed in …

Ponds, wetlands, and shallow lakes (collectively “shallow waterbodies”) are among the most
biogeochemically active freshwater ecosystems. Measurements of gross primary production …

Winter is a long period of the annual cycle of many lakes in the northern hemisphere. Low
irradiance, ice, and snow cover cause poor light penetration into the water column of these …

Metabolism is one of the most fundamental ecosystem processes, but the drivers of variation
in metabolic rates among lakes dominated by benthic primary producers remain poorly …

Carbon dioxide (CO 2) emissions from lakes have been proven to be an important
component of the continental carbon balance, but most CO 2 evasion estimates ignore daily …

Cooling the surface of freshwater bodies, whose temperatures are above the temperature of
maximum density, can generate differential cooling between shallow and deep regions …

Reservoirs represent a key component of the global carbon cycle. However, estimates of
carbon dioxide (CO 2) emissions from reservoirs remain poorly constrained due to the …