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 …

Permafrost degradation alters the flow rate, direction, and storage capacity of soil moisture,
affecting ecohydrological effects and climate systems, and posing a potential threat to …

Climate change exacerbates permafrost thawing, resulting exceptionally intense
retrogressive thaw slump (RTS) activity in the Arctic and Third Pole. However, comparative …

The status of plant and microbial nutrient limitation have profound impacts on ecosystem
carbon cycle in permafrost areas, which store large amounts of carbon and experience …

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

Vegetation changes are expected to alter soil thermal regimes, consequently modifying
climate feedbacks related to frozen ground thawing and carbon cycling in cold regions. The …

Quantifying uncertainty in runoff changes has profound implications for future runoff
investigations and will support global climate model improvement. We analyze the runoff …

In the context of global warming, increasing frequency of climate extremes poses a great
challenge to natural systems and humankind. However, the spatial and temporal …

Climate warming leads to widespread permafrost thaw with a fraction of the thawed
permafrost carbon (C) being released as carbon dioxide (CO2), thus triggering a positive …

Both gradual and abrupt changes in lake surface area in permafrost regions are crucial for
understanding the water cycles in cold regions under climate change. However, seasonal …