Injection of lightning‐produced NO x , water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements-Reference-Cited by-同舟云学术

Injection of lightning‐produced NO x , water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements

Published:2016-06-11 Issue:11 Volume:121 Page:6638-6668
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Huntrieser H.¹,Lichtenstern M.¹,Scheibe M.¹,Aufmhoff H.¹,Schlager H.¹,Pucik T.¹²,Minikin A.¹,Weinzierl B.¹³,Heimerl K.¹,Pollack I. B.⁴⁵⁶,Peischl J.⁴⁵,Ryerson T. B.⁴,Weinheimer A. J.⁷,Honomichl S.⁷,Ridley B. A.⁷,Biggerstaff M. I.⁸,Betten D. P.⁸,Hair J. W.⁹,Butler C. F.⁹,Schwartz M. J.¹⁰,Barth M. C.⁷

Affiliation:

1. Deutsches Zentrum für Luft‐ und Raumfahrt Institut für Physik der Atmosphäre Oberpfaffenhofen Germany

2. Masaryk University Brno Czech Republic

3. Faculty of Physics University of Vienna Vienna Austria

4. NOAA Boulder Colorado USA

5. CIRES University of Colorado Boulder Boulder Colorado USA

6. Now at Atmospheric Science Department Colorado State University Fort Collins Colorado USA

7. NCAR Boulder Colorado USA

8. School of Meteorology University of Oklahoma Norman Oklahoma USA

9. NASA Langley Research Center Hampton Virginia USA

10. Jet Propulsion Laboratory California Institute of Technology Pasadena California USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JD024273

Reference104 articles.

1. Impact of lightning NO emissions on North American photochemistry as determined using the Global Modeling Initiative (GMI) model

2. UV Dosage Levels in Summer: Increased Risk of Ozone Loss from Convectively Injected Water Vapor

3. Smoking Rain Clouds over the Amazon

4. Transport of biomass burning smoke to the upper troposphere by deep convection in the equatorial region

5. The tropospheric distribution of formaldehyde during TROPOZ II

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