Injection of lightning-produced NOx, water vapor, wildfire
emissions, and stratospheric air to the UT/LS as observed from
DC3 measurements

J 2016

Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements

HUNTRIESER, H.; M. LICHTENSTERN; M. SCHEIBE; H. AUFMHOFF; H. SCHLAGER et al.

Základní údaje

Originální název

Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements

Autoři

Vydání

Journal of Geophysical Research: Atmospheres, 2016, 0148-0227

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10509 Meteorology and atmospheric sciences

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 3.318 v roce 2015

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/16:00108674

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

SPECTRAL-RESOLUTION LIDAR; CLOUD-SCALE MODEL; UPPER TROPOSPHERE; AIRBORNE MEASUREMENTS; NITROGEN-OXIDES; UNITED-STATES; CONVECTIVE-TRANSPORT; GENERATED NOX; THUNDERSTORMS; OZONE

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 11. 5. 2020 11:27, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

During the Deep Convective Clouds and Chemistry (DC3) experiment in summer 2012, airborne measurements were performed in the anvil inflow/outflow of thunderstorms over the Central U.S. by three research aircraft. A general overview of Deutsches Zentrum fur Luft-und Raumfahrt (DLR)-Falcon in situ measurements (CO, O-3, SO2, CH4, NO, NOx, and black carbon) is presented. In addition, a joint flight on 29 May 2012 in a convective line of isolated supercell storms over Oklahoma is described based on Falcon, National Science Foundation/National Center for Atmospheric Research Gulfstream-V (NSF/NCAR-GV), and NASA-DC8 trace species in situ and lidar measurements. During DC3 some of the largest and most destructive wildfires in New Mexico and Colorado state's history were burning, which strongly influenced air quality in the DC3 thunderstorm inflow and outflow region. Lofted biomass burning (BB) plumes were frequently observed in the mid-and upper troposphere (UT) in the vicinity of deep convection. The impact of lightning-produced NOx (LNOx) and BB emissions was analyzed on the basis of mean vertical profiles and tracer-tracer correlations (CO-NOx and O-3-NO). On a regular basis DC3 thunderstorms penetrated the tropopause and injected large amounts of LNOx into the lower stratosphere (LS). Inside convection, low O-3 air (similar to 80 nmol mol(-1)) from the lower troposphere was rapidly transported to the UT/LS region. Simultaneously, O-3-rich stratospheric air masses (similar to 100-200 nmol mol(-1)) were present around and below the thunderstorm outflow and enhanced UT-O-3 mixing ratios significantly. A 10 year global climatology of H2O data from the Aura Microwave Limb Sounder confirmed that the Central U.S. is a preferred region for convective injection into the LS.

Citovat

HUNTRIESER, H.; M. LICHTENSTERN; M. SCHEIBE; H. AUFMHOFF; H. SCHLAGER; Tomáš PÚČIK; A. MINIKIN; B. WEINZIERL; K. HEIMERL; I.B. POLLACK; J. PEISCHL; T.B. RYERSON; A. J. WEINHEIMER; S. HONOMICHL; B. A. RIDLEY; M. I. BIGGERSTAFF; D. P. BETTEN; J. W. HAIR; C. F. BUTLER; M. J. SCHWARTZ a M. C. BARTH. Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements. Journal of Geophysical Research: Atmospheres. 2016, roč. 121, č. 11, s. 6638-6668. ISSN 0148-0227. Dostupné z: https://doi.org/10.1002/2015JD024273.

@article{1355912,
   author = {Huntrieser, H. and Lichtenstern, M. and Scheibe, M. and Aufmhoff, H. and Schlager, H. and Púčik, Tomáš and Minikin, A. and Weinzierl, B. and Heimerl, K. and Pollack, I.B. and Peischl, J. and Ryerson, T.B. and Weinheimer, A. J. and Honomichl, S. and Ridley, B. A. and Biggerstaff, M. I. and Betten, D. P. and Hair, J. W. and Butler, C. F. and Schwartz, M. J. and Barth, M. C.},
   article_number = {11},
   doi = {https://doi.org/10.1002/2015JD024273},
   keywords = {SPECTRAL-RESOLUTION LIDAR; CLOUD-SCALE MODEL; UPPER TROPOSPHERE; AIRBORNE MEASUREMENTS; NITROGEN-OXIDES; UNITED-STATES; CONVECTIVE-TRANSPORT; GENERATED NOX; THUNDERSTORMS; OZONE},
   language = {eng},
   issn = {0148-0227},
   journal = {Journal of Geophysical Research: Atmospheres},
   title = {Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements},
   url = {http://onlinelibrary.wiley.com/doi/10.1002/2015JD024273/full},
   volume = {121},
   year = {2016}
}

TY  - JOUR
ID  - 1355912
AU  - Huntrieser, H. - Lichtenstern, M. - Scheibe, M. - Aufmhoff, H. - Schlager, H. - Púčik, Tomáš - Minikin, A. - Weinzierl, B. - Heimerl, K. - Pollack, I.B. - Peischl, J. - Ryerson, T.B. - Weinheimer, A. J. - Honomichl, S. - Ridley, B. A. - Biggerstaff, M. I. - Betten, D. P. - Hair, J. W. - Butler, C. F. - Schwartz, M. J. - Barth, M. C.
PY  - 2016
TI  - Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements
JF  - Journal of Geophysical Research: Atmospheres
VL  - 121
IS  - 11
SP  - 6638-6668
EP  - 6638-6668
SN  - 01480227
KW  - SPECTRAL-RESOLUTION LIDAR
KW  - CLOUD-SCALE MODEL
KW  - UPPER TROPOSPHERE
KW  - AIRBORNE MEASUREMENTS
KW  - NITROGEN-OXIDES
KW  - UNITED-STATES
KW  - CONVECTIVE-TRANSPORT
KW  - GENERATED NOX
KW  - THUNDERSTORMS
KW  - OZONE
UR  - http://onlinelibrary.wiley.com/doi/10.1002/2015JD024273/full
L2  - http://onlinelibrary.wiley.com/doi/10.1002/2015JD024273/full
N2  - During the Deep Convective Clouds and Chemistry (DC3) experiment in summer 2012, airborne measurements were performed in the anvil inflow/outflow of thunderstorms over the Central U.S. by three research aircraft. A general overview of Deutsches Zentrum fur Luft-und Raumfahrt (DLR)-Falcon in situ measurements (CO, O-3, SO2, CH4, NO, NOx, and black carbon) is presented. In addition, a joint flight on 29 May 2012 in a convective line of isolated supercell storms over Oklahoma is described based on Falcon, National Science Foundation/National Center for Atmospheric Research Gulfstream-V (NSF/NCAR-GV), and NASA-DC8 trace species in situ and lidar measurements. During DC3 some of the largest and most destructive wildfires in New Mexico and Colorado state's history were burning, which strongly influenced air quality in the DC3 thunderstorm inflow and outflow region. Lofted biomass burning (BB) plumes were frequently observed in the mid-and upper troposphere (UT) in the vicinity of deep convection. The impact of lightning-produced NOx (LNOx) and BB emissions was analyzed on the basis of mean vertical profiles and tracer-tracer correlations (CO-NOx and O-3-NO). On a regular basis DC3 thunderstorms penetrated the tropopause and injected large amounts of LNOx into the lower stratosphere (LS). Inside convection, low O-3 air (similar to 80 nmol mol(-1)) from the lower troposphere was rapidly transported to the UT/LS region. Simultaneously, O-3-rich stratospheric air masses (similar to 100-200 nmol mol(-1)) were present around and below the thunderstorm outflow and enhanced UT-O-3 mixing ratios significantly. A 10 year global climatology of H2O data from the Aura Microwave Limb Sounder confirmed that the Central U.S. is a preferred region for convective injection into the LS.
ER  -

HUNTRIESER, H.; M. LICHTENSTERN; M. SCHEIBE; H. AUFMHOFF; H. SCHLAGER; Tomáš PÚČIK; A. MINIKIN; B. WEINZIERL; K. HEIMERL; I.B. POLLACK; J. PEISCHL; T.B. RYERSON; A. J. WEINHEIMER; S. HONOMICHL; B. A. RIDLEY; M. I. BIGGERSTAFF; D. P. BETTEN; J. W. HAIR; C. F. BUTLER; M. J. SCHWARTZ a M. C. BARTH. Injection of lightning-produced NOx, water vapor, wildfire emissions, and stratospheric air to the UT/LS as observed from DC3 measurements. \textit{Journal of Geophysical Research: Atmospheres}. 2016, roč.~121, č.~11, s.~6638-6668. ISSN~0148-0227. Dostupné z: https://doi.org/10.1002/2015JD024273.

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