Altered precipitation patterns resulting from climate change will have particularly significant
consequences in water‐limited ecosystems, such as arid to semi‐arid ecosystems, where …

As the second largest carbon (C) flux between the atmosphere and terrestrial ecosystems,
soil respiration (Rs) plays vital roles in regulating atmospheric CO 2 concentration ([CO2]) …

Aim Climate change intensifies the hydrological cycle and consequently alters precipitation
regimes. Accurately assessing future carbon (C) budgets depends on understanding the …

Global climate models predict that future precipitation regimes will largely change across the
globe due to the intensification of the global water cycle under climate warming, which may …

Nitrogen (N) deposition to semiarid ecosystems is increasing globally, yet few studies have
investigated the ecological consequences of N enrichment in these ecosystems …

Aim Root production and turnover play a key role in regulating carbon (C) flow in terrestrial
ecosystems. However, a general pattern reflecting the responses of roots to increasing …

Anthropogenic eutrophication is known to impair the stability of aboveground net primary
productivity (ANPP), but its effects on the stability of belowground (BNPP) and total (TNPP) …

Terrestrial ecosystems have experienced rising nitrogen (N) inputs during the last decades
with consequences for belowground carbon (C) and N dynamics. This study investigates …

Despite the increasing impact of atmospheric nitrogen (N) deposition on terrestrial
greenhouse gas (GHG) budget, through driving both the net atmospheric CO2 exchange …

Semi‐arid ecosystems play an important role in regulating the dynamics of the global
terrestrial CO 2 sink. These dynamics are mainly driven by increasing inter‐annual …