[PDF] Top 20 Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
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Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
... from the undisturbed free stream either by ram pressure from a partially plugged shroud at the inlet tip (Arctic Re- search of the Composition of the Troposphere from Air- ... See full document
11
Measurements of CH<sub>3</sub>O<sub>2</sub>NO<sub>2</sub> in the upper troposphere
... by the National Science Foundation Graduate Research Fellowship under Grant ...from the NASA Postdoctoral Pro- gram. We thank William H. Brune for use of the OH and HO 2 ... See full document
27
Does acetone react with HO<sub>2</sub> in the upper-troposphere?
... conducted in a 500 cm 3 jacketed quartz ...by the circulation of a cryogenic fluid through the outer jacket, and monitored with a J-type thermocouple to an esti- mated accuracy ... See full document
27
Comparisons of continuous atmospheric CH<sub>4</sub>, CO<sub>2</sub> and N<sub>2</sub>O measurements – results from a travelling instrument campaign at Mace Head
... to the dry G2301 instru- ment. The calibration suite of the CRDS systems consists of four cylinders filled with synthetic gas mixture by Deuste Steininger (Mühlhausen, ...by the ... See full document
16
A novel model to predict the physical state of atmospheric H<sub>2</sub>SO<sub>4</sub>/NH<sub>3</sub>/H<sub>2</sub>O aerosol particles
... for the month of ...quently. The 400-600 mbar bin corresponds to the free troposphere around 5 km, an altitude where H 2 SO 4 /NH 3 /H 2 O particles have also been ... See full document
39
Spatiotemporal variations of air pollutants (O<sub>3</sub>, NO<sub>2</sub>, SO<sub>2</sub>, CO, PM<sub>10</sub>, and VOCs) with land-use types
... averages of the O 3 (ppb) versus NO 2 (ppb) over South Korea during 2002–2013 under the MEK four land- use types of residence (R), commerce (C), industry (I), and greenbelt ...O ... See full document
29
A two-channel thermal dissociation cavity ring-down spectrometer for the detection of ambient NO<sub>2</sub>, RO<sub>2</sub>NO<sub>2</sub> and RONO<sub>2</sub>
... 10. Measurements of the difference signal (TD cavity sam- pling from the 473 (squares) or 723 K inlet (circles) – NO 2 ref- erence cavity) when adding various amounts of NO to ... See full document
24
Aircraft measurements of BrO, IO, glyoxal, NO<sub>2</sub>, H<sub>2</sub>O, O<sub>2</sub>–O<sub>2</sub> and aerosol extinction profiles in the tropics: comparison with aircraft-/ship-based in situ and lidar measurements
... comparison, the Mie calculations consistently find lower extinction. The extinction inside the boundary layer was lower than that due to Rayleigh scattering and a factor of ∼ ...AMAX-DOAS. ... See full document
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HO<sub>2</sub>NO<sub>2</sub> and HNO<sub>3</sub> in the coastal Antarctic winter night: a "lab-in-the-field" experiment
... clearly in Fig. 5. The three examples show periods when ambient air temperatures varied rapidly and considerably, but where they remained below the −25 ◦ C dewpoint threshold such that no chemical ... See full document
9
Decadal variability of soil CO<sub>2</sub> NO, N<sub>2</sub>O, and CH<sub>4</sub> fluxes at the Höglwald Forest, Germany
... fluxes. The data base obtained by short-term continuous measurements – even if per- formed at different season – may lead to a significant under- or overestimation of the trace gas source ... See full document
49
Simultaneous measurements of OClO, NO<sub>2</sub> and O<sub>3</sub> in the Arctic polar vortex by the GOMOS instrument
... line). The relative differences between these two profiles are mostly lower than 10% (in absolute values) and this result holds for the other latitudinal ...that the results of our DOAS ... See full document
24
Characterization of trace gases measured over Alberta oil sands mining operations: 76 speciated C<sub>2</sub>–C<sub>10</sub> volatile organic compounds (VOCs), CO<sub>2</sub>, CH<sub>4</sub>, CO, NO, NO<sub>2</sub>, NO<sub>y</sub>, O<sub>3</sub> and SO<su
... over the oil sands than at any other time during the summer phase of ...that the maxi- mum abundances were not ordered according to chain ...showed the highest maximum mix- ing ratio, ... See full document
24
Direct detection of OH formation in the reactions of HO<sub>2</sub> with CH<sub>3</sub> C(O)O<sub>2</sub> and other substituted peroxy radicals
... uncertainties in both (experimentally determined) reagent concentrations and the (literature) photochemical parameters used to simulate [OH] t ...conducted in which the probe laser was tuned ... See full document
38
Simultaneous measurements of OClO, NO<sub>2</sub> and O<sub>3</sub> in the Arctic polar vortex by the GOMOS instrument
... Petelina, S. V., Bourassa, A. E., Wiensz, J. T., Ivanov, E. V., McDade, I. C., Solheim, B. H., McConnell, J. C., Haley, C. S., von Savigny, C., Sioris, C. E., McLinden, C. A., Griffioen, E., Kaminski, J., Evans, W. F. ... See full document
10
Suitability of quantum cascade laser spectroscopy for CH<sub>4</sub> and N<sub>2</sub>O eddy covariance flux measurements
... used in pulsed mode. A sequence of laser light pulses, each with duration of about 10 ns, is divided by a beam splitter and sent through the multipass cell and along a ...with the ... See full document
14
Consistency and quality assessment of the Metop-A/IASI and Metop-B/IASI operational trace gas products (O<sub>3</sub>, CO, N<sub>2</sub>O, CH<sub>4</sub>, and CO<sub>2</sub>) in the subtropical North Atlantic
... spectra, the FTS systems can pro- vide TC amounts and volume mixing ratio (VMR) profiles of many different atmospheric trace gases with high ...Within the NDACC (Network for Detection of ... See full document
19
Direct N<sub>2</sub>O<sub>5</sub> reactivity measurements at a polluted coastal site
... light of these effects, we instituted a fairly rigorous data quality ...when the RH in the flow reactor measured at the end of a filter on/off/on cycle was more than 2 % ... See full document
10
Observations of total RONO<sub>2</sub> over the boreal forest: NO<sub>x</sub> sinks and HNO<sub>3</sub> sources
... thus the base calculation is biased low. For in- stance, only the monoterpenes α-pinene and β-pinene are ...measured. Measurements from the boreal forest in Finland indicate ... See full document
54
Latitude-time variations of atmospheric column-average dry air mole fractions of CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O
... simulations of CH 4 and related species: linking transport, surface flux and chemical loss with CH 4 variability in the troposphere and lower stratosphere, ... See full document
26
The CU mobile Solar Occultation Flux instrument: structure functions and emission rates of NH<sub>3</sub>, NO<sub>2</sub> and C<sub>2</sub>H<sub>6</sub>
... For measurements from the mobile laboratory the azimuth and elevation angles change rapidly over the course of an ...characterize the ILS (Hase et al., 1999) over a wide range ... See full document
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