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[PDF] Top 20 Measurements of N<sub>2</sub>O<sub>5</sub>, NO<sub>2</sub>, and O<sub>3</sub> east of the San Francisco Bay

Has 10000 "Measurements of N<sub>2</sub>O<sub>5</sub>, NO<sub>2</sub>, and O<sub>3</sub> east of the San Francisco Bay" found on our website. Below are the top 20 most common "Measurements of N<sub>2</sub>O<sub>5</sub>, NO<sub>2</sub>, and O<sub>3</sub> east of the San Francisco Bay".

Measurements of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt;, and O&lt;sub&gt;3&lt;/sub&gt; east of the San Francisco Bay

Measurements of N<sub>2</sub>O<sub>5</sub>, NO<sub>2</sub>, and O<sub>3</sub> east of the San Francisco Bay

... scatter and to exclude ambient light from the cell. The laser power exiting the cell was monitored by a ...photodiode. The electric field vector of the laser light was ... See full document

21

High concentrations of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; and NO&lt;sub&gt;3&lt;/sub&gt; observed in daytime with a TD-CIMS: chemical interference or a real atmospheric phenomenon?

High concentrations of N<sub>2</sub>O<sub>5</sub> and NO<sub>3</sub> observed in daytime with a TD-CIMS: chemical interference or a real atmospheric phenomenon?

... T., and Fehsenfeld, F.: Reactivity and loss mechanisms of NO 3 and N 2 O 5 in a pol- luted marine environment: results from in situ measurements during New ... See full document

32

An aircraft based three channel broadband cavity enhanced absorption spectrometer for simultaneous measurements of NO&lt;sub&gt;3&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; and NO&lt;sub&gt;2&lt;/sub&gt;

An aircraft based three channel broadband cavity enhanced absorption spectrometer for simultaneous measurements of NO<sub>3</sub>, N<sub>2</sub>O<sub>5</sub> and NO<sub>2</sub>

... technique and spectral analysis procedure has been widely reported in the literature and is only briefly described ...details the reader is directed to recent publications by Ball and ... See full document

46

Radical chemistry at night: comparisons between observed and modelled HO&lt;sub&gt;x&lt;/sub&gt;, NO&lt;sub&gt;3&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; during the RONOCO project

Radical chemistry at night: comparisons between observed and modelled HO<sub>x</sub>, NO<sub>3</sub> and N<sub>2</sub>O<sub>5</sub> during the RONOCO project

... concentrations of unmeasured VOCs dur- ing RONOCO may explain the model measurement discrep- ...isolated and classi- fied over 500 different VOCs not routinely measured, with significant impacts on ... See full document

23

Direct N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reactivity measurements at a polluted coastal site

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

Comparisons of continuous atmospheric CH&lt;sub&gt;4&lt;/sub&gt;, CO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O measurements &amp;ndash; results from a travelling instrument campaign at Mace Head

Comparisons of continuous atmospheric CH<sub>4</sub>, CO<sub>2</sub> and N<sub>2</sub>O measurements &ndash; 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

MIPAS reduced spectral resolution UTLS-1 mode measurements of temperature, O&lt;sub&gt;3&lt;/sub&gt;, HNO&lt;sub&gt;3&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O, H&lt;sub&gt;2&lt;/sub&gt;O and relative humidity over ice: retrievals and comparison to MLS

MIPAS reduced spectral resolution UTLS-1 mode measurements of temperature, O<sub>3</sub>, HNO<sub>3</sub>, N<sub>2</sub>O, H<sub>2</sub>O and relative humidity over ice: retrievals and comparison to MLS

... P., San- tee, M., Yudin, V., and Walker, K.: Global Observations of HNO3 from the High Resolution Dynamics Limb Sounder (HIRDLS) – First results, ... See full document

49

Coastal upwelling fluxes of O&lt;sub&gt;2&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O,  and CO&lt;sub&gt;2&lt;/sub&gt; assessed from continuous atmospheric observations at Trinidad,California

Coastal upwelling fluxes of O<sub>2</sub>, N<sub>2</sub>O, and CO<sub>2</sub> assessed from continuous atmospheric observations at Trinidad,California

... tions of many anthropogenic trace gases (Prinn et al., 2000). The CO 2 record displays variations resulting from local meteorology and fluxes from extensive conifer forests to the ... See full document

31

Characterization of trace gases measured over Alberta oil sands mining operations: 76 speciated C&lt;sub&gt;2&lt;/sub&gt;–C&lt;sub&gt;10&lt;/sub&gt; volatile organic compounds (VOCs), CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt;, CO, NO, NO&lt;sub&gt;2&lt;/sub&gt;, NO&lt;sub&gt;y&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt; and SO&lt;su

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

... LPG) and biomass burning (Blake et al., 1996; Watson et al., 2001; Buzcu and Fraser, ...2006). The i-butane (290 pptv) and n-butane (765 pptv) max- ima in the oil sands plumes ... See full document

24

Fluxes of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O from soil of burned grassland savannah of central Africa

Fluxes of CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O from soil of burned grassland savannah of central Africa

... to the lack of sufficient studies which also include the overall balance of GHG in unburned and burned ...variations of soil greenhouse gas (GHG) fluxes from savannahs are ... See full document

38

Observations of total RONO&lt;sub&gt;2&lt;/sub&gt; over the boreal forest: NO&lt;sub&gt;x&lt;/sub&gt; sinks and HNO&lt;sub&gt;3&lt;/sub&gt; sources

Observations of total RONO<sub>2</sub> over the boreal forest: NO<sub>x</sub> sinks and HNO<sub>3</sub> sources

... ARCTAS, and thus the base calculation is biased ...only the monoterpenes α-pinene and β-pinene are measured. Measurements from the boreal forest in Finland indicate substantial ... See full document

54

CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O fluxes from soil of a burned grassland in Central Africa

CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes from soil of a burned grassland in Central Africa

... in the top soil. Burning of grasslands often results in earlier growth of grass in the growing season, increasing the length of the biomass growth period (Ojima et ...On ... See full document

13

Decadal variability of soil CO&lt;sub&gt;2&lt;/sub&gt; NO, N&lt;sub&gt;2&lt;/sub&gt;O, and CH&lt;sub&gt;4&lt;/sub&gt; fluxes at the Höglwald Forest, Germany

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

The CU mobile Solar Occultation Flux instrument: structure functions and emission rates of NH&lt;sub&gt;3&lt;/sub&gt;, NO&lt;sub&gt;2&lt;/sub&gt; and C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;

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>

... over the planetary boundary layer height (PBLH) and hence are inde- pendent of its changing ...Column measurements can be used to quantify the emission flux/production rate from an area ... See full document

20

Aircraft measurements of BrO, IO, glyoxal, NO&lt;sub&gt;2&lt;/sub&gt;, H&lt;sub&gt;2&lt;/sub&gt;O, O&lt;sub&gt;2&lt;/sub&gt;–O&lt;sub&gt;2&lt;/sub&gt;   and aerosol extinction profiles in the tropics: comparison with aircraft-/ship-based in situ and lidar measurements

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 ∼ ...HSRL ... See full document

28

Atmospheric histories and growth trends of C&lt;sub&gt;4&lt;/sub&gt;F&lt;sub&gt;10&lt;/sub&gt;, C&lt;sub&gt;5&lt;/sub&gt;F&lt;sub&gt;12&lt;/sub&gt;, C&lt;sub&gt;6&lt;/sub&gt;F&lt;sub&gt;14&lt;/sub&gt;, C&lt;sub&gt;7&lt;/sub&gt;F&lt;sub&gt;16&lt;/sub&gt; and C&lt;sub&gt;8&lt;/sub&gt;F&lt;sub&gt;18&lt;/sub&gt;

Atmospheric histories and growth trends of C<sub>4</sub>F<sub>10</sub>, C<sub>5</sub>F<sub>12</sub>, C<sub>6</sub>F<sub>14</sub>, C<sub>7</sub>F<sub>16</sub> and C<sub>8</sub>F<sub>18</sub>

... measure the heavy PFC mole fractions in archived air samples at the Scripps Institution of Oceanography (SIO), University of California, San Diego (San Diego, CA) and at ... See full document

13

HO&lt;sub&gt;2&lt;/sub&gt;NO&lt;sub&gt;2&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt; in the coastal Antarctic winter night: a &quot;lab-in-the-field&quot; experiment

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

... 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 data ... See full document

9

Greenhouse gas emissions (CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O) from perialpine and alpine hydropower reservoirs

Greenhouse gas emissions (CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O) from perialpine and alpine hydropower reservoirs

... concentrations of the water flowing from the glacier into the reservoir reach 30 nM in August with values in June and July are lower (around 15 nM), possibly due to dilution by snow ... See full document

38

Exploring the atmospheric chemistry of O&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;minus;&lt;/sup&gt; and assessing the maximum turnover number of ion-catalysed H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; formation

Exploring the atmospheric chemistry of O<sub>2</sub>SO<sub>3</sub><sup>&minus;</sup> and assessing the maximum turnover number of ion-catalysed H<sub>2</sub>SO<sub>4</sub> formation

... Kirkby, J., Curtius, J., Almeida, J., Dunne, E., Duplissy, J., Ehrhart, S., Franchin, A., Gagn´e, S., Ickes, L., K¨urten, A., Kupc, A., Met- zger, A., Riccobono, F., Rondo, L., Schobesberger, S., Tsagkoge- orgas, G., ... See full document

9

Latitude-time variations of atmospheric column-average dry air mole fractions of CO&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;4&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O

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

... by the nearest northern site (Park Falls), which has stronger uptake due to denser vegetation and agricultural activities compared to the re- gions around the Lamont site ...1). The ... See full document

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