Many regions on Earth are expected to become drier with climate change, which may impact
nitrogen (N) cycling rates and availability. We used a meta‐analytical approach on the …

Nitric oxide (NO) is essential for plant growth and development, as well as interactions with
abiotic and biotic environments. Its importance for multiple functions in plants means that …

Soil drying and wetting cycles can produce pulses of nitric oxide (NO) and nitrous oxide
(N2O) emissions with substantial effects on both regional air quality and Earth's climate …

The global inventory of NO x (NO x= NO+ NO2) emissions is poorly constrained, with a large
portion of the uncertainty attributed to soil NO emissions that result from soil abiotic and …

Nitrogen (N) trace gas emission pulses produced after wetting dry soils may be important
pathways of ecosystem N loss. However, the rates and mechanisms controlling these …

Soils are an important source of NO, particularly in dry lands because of trade‐offs that
develop between biotic and abiotic NO‐producing processes when soils dry out …

Determination of tipping points in nitrogen (N) isotope (δ15N) natural abundance, especially
soil δ15N, with increasing aridity, is critical for estimating N‐cycling dynamics and N …

The invasion of drylands by leguminous mesquite (Prosopis spp.) is frequently associated
with increases in the soil organic carbon (C) and nitrogen (N) pools. These increases …

In dryland soils, spatiotemporal variation in surface soils (0–10 cm) plays an important role
in the function of the “critical zone” that extends from canopy to groundwater. Understanding …

Climate change is increasing the variability of precipitation, altering the frequency of soil
drying‐wetting events and the distribution of seasonal precipitation. These changes in …