Abstract Terrestrial ecosystems release~ 106–130 PgC yr–1 into the atmosphere through
respiration, counterbalancing photosynthetic carbon uptake and determining the strength of …

Soil respiration (Rs), the soil‐to‐atmosphere flux of CO2, is a dominant but uncertain part of
the carbon cycle, even after decades of study. This review focuses on progress in …

The scientific and wider interest in the relationship between atmospheric temperature (T)
and concentration of carbon dioxide ([CO 2]) has been enormous. According to the …

Reservoir routing has been a routine procedure in hydrology, hydraulics and water
management. It is typically based on the mass balance (continuity equation) and a …

The coastal terrestrial-aquatic interface (TAI) is a highly dynamic system characterized by
strong physical, chemical, and biological gradients. In particular, shifting soil redox …

Soils both produce and consume methane (CH 4), a potent greenhouse gas that contributes
to climate change. In coastal forests, upland soils are shifting from being CH 4 sinks to …

The temperature sensitivity (Q 10) of C mineralization was studied in soils of two types: gray
forest (Phaeozem, forest glade ecosystem) and soddy-podzolic (Retisol), dead soil cover …

Microbial processing of soil organic matter is a significant driver of C cycling, yet we lack an
understanding of what shapes the turnover of this large terrestrial pool. In part, this is due to …

Reservoir routing has been a routine procedure in hydrology, hydraulics and water
management. It is typically based on the mass balance (continuity equation) and a …

Why do (mainstream)“sceptics” accept the debating space (the penthouse) that was defined
by the climate establishment? 1. Is the underlying science correct and only details need to …