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[PDF] Top 20 Unpredictability of internal M<sub>2</sub>

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Unpredictability of internal M&lt;sub&gt;2&lt;/sub&gt;

Unpredictability of internal M<sub>2</sub>

... the above regions will be discussed, focusing on “internal” motions. This requires separation of internal signals from ubiquitous “barotropic” semidiurnal motions. The latter are defined as motions ... See full document

8

Global distributions of C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;, C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;2&lt;/sub&gt;, HCN, and PAN retrieved from MIPAS reduced spectral resolution measurements

Global distributions of C<sub>2</sub>H<sub>6</sub>, C<sub>2</sub>H<sub>2</sub>, HCN, and PAN retrieved from MIPAS reduced spectral resolution measurements

... Kiefer, M., Schieferdecker, T., Stiller, G. P., and Versick, S.: Retrieval of tem- perature, H 2 O, O 3 , HNO 3 , CH 4 , N 2 O, ClONO 2 and ClO from MIPAS reduced resolution nom- inal ... See full document

36

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

... 30% of total world oil reserves (Alboudwarej et ...mixture of sand, water, clay and crude bitumen – a thick, sticky extra-heavy crude oil that is “unconventional”, ...most of which occurs as oil ... See full document

24

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>

... Rothman, L. S., Gordon, I. E., Barbe, A., Benner, D. C., Bernath, P. F., Birk, M., Boudon, V., Brown, L. R., Campargue, A., Champion, J. P., Chance, K., Coudert, L. H., Dana, V., Devi, V. M., Fally, S., ... See full document

46

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

... CO 2 flux based on climatological surface ocean pCO 2 , and seasonal biological and temperature effects, Deep-Sea Research Part II-Topical Studies in Oceanography, 49, 1601– 1622, ... See full document

31

Enhancement of atmospheric H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; / H&lt;sub&gt;2&lt;/sub&gt;O nucleation: organic oxidation products versus amines

Enhancement of atmospheric H<sub>2</sub>SO<sub>4</sub> / H<sub>2</sub>O nucleation: organic oxidation products versus amines

... Leppa, J., Loukonen, V., Makhmutov, V., Mathot, S., McGrath, M. J., Nieminen, T., Olenius, T., Onnela, A., Petaja, T., Ric- cobono, F., Riipinen, I., Rissanen, M., Rondo, L., Ruuskanen, T., Santos, F. D., ... See full document

14

Investigation of the hygroscopic properties of Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt; and internally mixed Ca(NO&lt;sub&gt;3&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;/CaCO&lt;sub&gt;3&lt;/sub&gt; particles by micro-Raman spectrometry

Investigation of the hygroscopic properties of Ca(NO<sub>3</sub>)<sub>2</sub> and internally mixed Ca(NO<sub>3</sub>)<sub>2</sub>/CaCO<sub>3</sub> particles by micro-Raman spectrometry

... Seinfeld, J. H., Carmichael, G. R., Arimoto, R., Conant, W. C., Brechtel, F. J., Bates, T. S., Cahill, T. A., Clarke, A. D., Doherty, S. J., Flatau, P. J., Huebert, B. J., Kim, J., Markowicz, K. M., Quinn, P. K., ... See full document

29

Global CO&lt;sub&gt;2&lt;/sub&gt; fluxes estimated from GOSAT retrievals of total column CO&lt;sub&gt;2&lt;/sub&gt;

Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>

... tensen, J. H., Delage, F., Denning, A. S., Fan, S., Geels, C., Houweling, S., Imasu, R., Karstens, U., Kawa, S. R., Kleist, J., Krol, M. C., Lin, S.-J., Lokupitiya, R., Maki, T., Maksyu- tov, S., Niwa, Y., Onishi, ... See full document

66

Five years of CO, HCN, C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;6&lt;/sub&gt;, C&lt;sub&gt;2&lt;/sub&gt;H&lt;sub&gt;2&lt;/sub&gt;, CH&lt;sub&gt;3&lt;/sub&gt;OH, HCOOH and H&lt;sub&gt;2&lt;/sub&gt;CO total columns measured in the Canadian high Arctic

Five years of CO, HCN, C<sub>2</sub>H<sub>6</sub>, C<sub>2</sub>H<sub>2</sub>, CH<sub>3</sub>OH, HCOOH and H<sub>2</sub>CO total columns measured in the Canadian high Arctic

... Rothman, L. S., Gordon, I. E., Barbe, A., Benner, D. C., Bernath, P. F., Birk, M., Boudon, V., Brown, L. R., Campargue, A., Champion, J.-P., Chance, K., Coudert, L. H., Danaj, V., Devi, V. M., Fally, S., ... See full document

24

Chlorine activation by N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;: simultaneous, in situ detection of ClNO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; by chemical ionization mass spectrometry

Chlorine activation by N<sub>2</sub>O<sub>5</sub>: simultaneous, in situ detection of ClNO<sub>2</sub> and N<sub>2</sub>O<sub>5</sub> by chemical ionization mass spectrometry

... many of the analyte ions produced during the chemical ionization pro- ...formation of such complexes can enhance sensi- tivity by stabilizing reactive complexes, or, as is more often the case, such ... See full document

12

Global CO&lt;sub&gt;2&lt;/sub&gt; fluxes estimated from GOSAT retrievals of total column CO&lt;sub&gt;2&lt;/sub&gt;

Global CO<sub>2</sub> fluxes estimated from GOSAT retrievals of total column CO<sub>2</sub>

... fects of atmospheric light scattering on spectroscopic observa- tions of greenhouse gases from ...Part 2: Algorithm inter- comparison in the GOSAT data processing for CO 2 retrievals over ... See full document

23

On the mechanism of the post-midnight winter &lt;i&gt;N&lt;sub&gt;m&lt;/sub&gt;F&lt;sub&gt;2&lt;/sub&gt;&lt;/i&gt; enhancements: dependence on solar activity

On the mechanism of the post-midnight winter <i>N<sub>m</sub>F<sub>2</sub></i> enhancements: dependence on solar activity

... probability of the ...70±80% of all quiet days), while the summer probability is about ...regardless of the level of solar ...results of other authors who analyzed this e€ect in the ... See full document

13

Temporal and spatial variations of soil 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 at three differently managed grasslands

Temporal and spatial variations of soil CO<sub>2</sub>, CH<sub>4</sub> and N<sub>2</sub>O fluxes at three differently managed grasslands

... Williams, M., Baronti, S., Berretti, F., and Grosz, B.: Effects of climate and management intensity on nitrous oxide emissions in grassland systems across Europe, ... See full document

15

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

... increase of cloud condensation nucleus activity by secondary aerosol for- mation and condensation: A case study for regional air pol- lution in northeastern China, ... See full document

9

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>

... site of interest there are 90 ◦ changes in the azimuth angle with each turn and many smaller degree changes in both elevation and azimuth angles due to fine tracking on uneven dirt ...2.0 m long beam ... See full document

20

Sensitivity of simulated CO&lt;sub&gt;2&lt;/sub&gt; concentration to  regridding of global fossil fuel CO&lt;sub&gt;2&lt;/sub&gt; emissions

Sensitivity of simulated CO<sub>2</sub> concentration to regridding of global fossil fuel CO<sub>2</sub> emissions

... series of the hourly concentration difference for the TAP site shows the largest value of about ...< 2 m s −1 ) and in the daytime of 13 January (3.5 m s −1 ) compared to the ... See full document

8

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

... Rigby, M., Saito, R., and Wilson, C.: TransCom model simulations of CH 4 and related species: linking transport, surface flux and chemical loss with CH 4 variability in the troposphere and lower ... See full document

26

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

... Bernhofer, C., Carrara, A., Chevallier, F., De Noblet, N., Friend, A. D., Friedlingstein, P., Grunwald, T., Heinesch, B., Keronen, P., Knohl, A., Krinner, G., Loustau, D., Manca, G., Matteucci, G., Miglietta, F., ... See full document

49

Tropospheric photooxidation of CF&lt;sub&gt;3&lt;/sub&gt;CH&lt;sub&gt;2&lt;/sub&gt;CHO and CF&lt;sub&gt;3&lt;/sub&gt;(CH&lt;sub&gt;2&lt;/sub&gt;)&lt;sub&gt;2&lt;/sub&gt;CHO initiated by Cl atoms and OH radicals

Tropospheric photooxidation of CF<sub>3</sub>CH<sub>2</sub>CHO and CF<sub>3</sub>(CH<sub>2</sub>)<sub>2</sub>CHO initiated by Cl atoms and OH radicals

... cell of variable pathlength from 1 to 8 m (Specac, Cyclone C5) sealed with ZnSe win- dows (transmittance range: 450–17 000 cm −1 ...means of a low power diode laser ...pathlength of 8 ... See full document

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Chlorine activation by N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;: simultaneous, in situ detection of ClNO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; by chemical ionization mass spectrometry

Chlorine activation by N<sub>2</sub>O<sub>5</sub>: simultaneous, in situ detection of ClNO<sub>2</sub> and N<sub>2</sub>O<sub>5</sub> by chemical ionization mass spectrometry

... campaign. We greatly appreciate the efforts of the RV Knorr crew exhibited during the entire cruise. We thank V. Faye McNeill for insights into nitryl chloride detection, G. M. Wolfe for help with ... See full document

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