핵심 개념
Anthropogenic reactive nitrogen has a net cooling effect on the global climate, but this effect may weaken in the future due to reduced aerosol loading and increased methane lifetime, while nitrous oxide-induced warming is likely to continue increasing.
초록
The content discusses the net climate effects of anthropogenic reactive nitrogen (Nr) since the pre-industrial era. Key points:
- Anthropogenic activities have substantially increased Nr loadings in the Earth system since pre-industrial times, contributing to eutrophication and air pollution.
- Increased Nr can influence global climate through various effects on atmospheric and land processes.
- The authors show that anthropogenic Nr causes a net negative direct radiative forcing of -0.34 W/m^2 in 2019 relative to 1850.
- This net cooling effect is due to increased aerosol loading, reduced methane lifetime, and increased terrestrial carbon sequestration, which outweigh the warming effects of enhanced atmospheric nitrous oxide and ozone.
- Future predictions using three representative scenarios suggest this cooling effect may be weakened, primarily due to reduced aerosol loading and increased methane lifetime, while N2O-induced warming is likely to continue increasing under all scenarios.
- The authors conclude that future reductions in anthropogenic Nr to achieve environmental protection goals need to be accompanied by enhanced efforts to reduce anthropogenic greenhouse gas emissions to mitigate climate change in line with the Paris Agreement.
통계
Anthropogenic Nr causes a net negative direct radiative forcing of -0.34 [−0.20, −0.50] W m−2 in 2019 relative to 1850.
인용구
"Anthropogenic activities have substantially enhanced the loadings of reactive nitrogen (Nr) in the Earth system since pre-industrial times1,2, contributing to widespread eutrophication and air pollution3,4,5,6."
"Here we show that anthropogenic Nr causes a net negative direct radiative forcing of −0.34 [−0.20, −0.50] W m−2 in the year 2019 relative to the year 1850."