Permafrost regions at high latitudes and altitudes store about half of the Earth's soil organic
carbon (SOC). These areas are also some of the most intensely affected by anthropogenic …

Permafrost covers a quarter of the northern hemisphere land surface and contains twice the
amount of carbon that is currently present in the atmosphere. Future climate change is …

Understanding methane (CH4) emission from thermokarst lakes is crucial for predicting the
impacts of abrupt thaw on the permafrost carbon-climate feedback. However, observational …

Thermokarst lakes are potentially important sources of methane (CH4) and carbon dioxide
(CO2). However, considerable uncertainty exists regarding carbon emissions from …

Our knowledge on permafrost carbon (C) cycle is crucial for understanding its feedback to
climate warming and develo** nature-based solutions for mitigating climate change. To …

Carbon dioxide (CO 2) and methane (CH 4) emissions from freshwater ecosystems are
predicted to increase under climate warming. However, freshwater ecosystems in …

Ebullition has been shown to be an important pathway for methane (CH 4) emissions from
inland waters. However, the CH 4 fluxes and their magnitudes in thermokarst lakes remain …

There are several publications related to the soil organic carbon (SOC) on the Qinghai-
Tibetan Plateau (QTP). However, most of these reports were from different parts of the …

Inland waters play an important role in the global carbon cycle and are potential hotspots of
greenhouse gas (GHG) production and emission. However, considerable uncertainty exists …

Small lentic freshwater ecosystems play a disproportionate role in global biogeochemical
cycles by processing large amounts of carbon (C), nitrogen (N), and phosphorus (P), but it is …