2011
DOI: 10.1029/2011gl047612
|View full text |Cite
|
Sign up to set email alerts
|

Tropospheric distribution and variability of N2O: Evidence for strong tropical emissions

Abstract: [1] Measurements of atmospheric N 2 O spanning altitudes from the surface to 14 km, and latitudes from 67°S to 85°N, show high concentrations in the tropics and subtropics, with strong maxima in the middle and upper troposphere. The pattern varies significantly over time scales of a few weeks. Global simulations do not accurately capture observed distributions with latitude, altitude, or time. Inversion results indicate strong, episodic inputs of nitrous oxide from tropical regions (as large as 1 Tg N-N 2 O ov… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

8
86
0

Year Published

2013
2013
2018
2018

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 86 publications
(94 citation statements)
references
References 30 publications
8
86
0
Order By: Relevance
“…we are not simply considering the annual mean latitudinal gradients). For N 2 O, the latitudinal relative difference between 20 and 40 • N is smaller than 0.32 % (Huang et al, 2008;Kort et al, 2011) and the seasonal cycle is insignificant as can be seen in WDCGG (2014). This implies a mean N 2 O gradient smaller than 0.016 % per degree of latitude.…”
Section: Appendix B: Collocation Criteria Between Iasi and Ground-basmentioning
confidence: 95%
“…we are not simply considering the annual mean latitudinal gradients). For N 2 O, the latitudinal relative difference between 20 and 40 • N is smaller than 0.32 % (Huang et al, 2008;Kort et al, 2011) and the seasonal cycle is insignificant as can be seen in WDCGG (2014). This implies a mean N 2 O gradient smaller than 0.016 % per degree of latitude.…”
Section: Appendix B: Collocation Criteria Between Iasi and Ground-basmentioning
confidence: 95%
“…In most cases in Fig. 4 we see that the model-measurement difference trends negative with height in the troposphere, which may reflect a model underestimate of the convective transport of N 2 O emissions (Kort et al, 2011). Large biases above 400 hPa in HIPPO IV (30-90 • N) and HIPPO V (30-90 • S) are driven by high-latitude observations in which the aircraft is sampling below the model tropopause but above the actual tropopause and highlight the difficulty in modeling the N 2 O vertical profile at these altitudes.…”
Section: A Posteriori Evaluation Of N 2 O Emissionsmentioning
confidence: 98%
“…The aircraft payload included high-frequency N 2 O measurements by quantum cascade laser spectroscopy (Kort et al, 2011). To ensure calibration consistency we apply an offset adjustment to these data for each deployment based on concurrent flask-based air samples, which are anchored to the NOAA 2006A scale.…”
Section: Atmospheric N 2 O Observationsmentioning
confidence: 99%
“…Soils under natural vegetation in tropical and subtropical regions have been reported to be a major source of nitrous oxide (N 2 O), a potent greenhouse gas and decomposer of ozone in the stratosphere (Hirsch et al 2006;Kort et al 2011;IPCC 2007). N 2 O emission from tropical forest are high compared to temperate and boreal natural ecosystems (Dalal and Allen 2008), but the contribution of subtropical forest in densely populated SE Asia to global N 2 O emissions is unclear.…”
Section: Introductionmentioning
confidence: 99%