BATAL: The Balloon measurement campaigns of the Asian Tropopause Aerosol Layer
J.-P. Vernier
(1, 2)
,
T. D. Fairlie
(1)
,
T. Deshler
(3)
,
M. Venkat Ratnam
(4)
,
H. Gadhavi
(4)
,
M. Natarajan
(1)
,
A. K. Pandit
(4)
,
A Raj
(4)
,
A. H. Kumar
(4)
,
A. Jayaraman
(4)
,
A. K. Singh
(5)
,
N. Rastogi
,
P. R. Sinha
,
S. Kumar
(5)
,
S. Tiwari
(5)
,
T. Wegner
(1)
,
N. Baker
(1)
,
D. Vignelles
(6)
,
G. Stenchikov
(7)
,
I. Shevchenko
,
J Smith
,
K. Bedka
(1)
,
A. Kesarkar
(4)
,
V. Singh
(4)
,
J. Bhate
(4)
,
V. Ravikiran
(4)
,
M. D. Rao
(4)
,
S. Ravindrababu
(4)
,
A. Patel
(8)
,
H. Vernier
(9)
,
F. G. Wienhold
(10)
,
H. Liu
(11)
,
T. Knepp
(1, 2)
,
L. Thomason
(1)
,
J. Crawford
(1)
,
L. Ziemba
(1)
,
J. Moore
(2)
,
S. Crumeyrolle
(12)
,
M. Williamson
(13)
,
Gwenaël Berthet
(6)
,
Fabrice Jegou
(6)
,
Jean-Baptiste Renard
(6)
1
LaRC -
NASA Langley Research Center [Hampton]
2 SSAI - Science Systems and Applications, Inc. [Hampton]
3 Department of Atmospheric Science [Laramie]
4 NARL - National Atmospheric Research Laboratory [Tirupati]
5 BHU - Banaras Hindu University [Varanasi]
6 LPC2E - Laboratoire de Physique et Chimie de l'Environnement et de l'Espace
7 RU - Rutgers, The State University of New Jersey [New Brunswick]
8 PRL - Physical Research Laboratory [Ahmedabad]
9 VIMS - Virginia Institute of Marine Science
10 ETH Zürich - Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich]
11 NIA - National Institute of Aerospace [Hampton]
12 LOA - Laboratoire d’Optique Atmosphérique - UMR 8518
13 Smith and Williamson Inc
2 SSAI - Science Systems and Applications, Inc. [Hampton]
3 Department of Atmospheric Science [Laramie]
4 NARL - National Atmospheric Research Laboratory [Tirupati]
5 BHU - Banaras Hindu University [Varanasi]
6 LPC2E - Laboratoire de Physique et Chimie de l'Environnement et de l'Espace
7 RU - Rutgers, The State University of New Jersey [New Brunswick]
8 PRL - Physical Research Laboratory [Ahmedabad]
9 VIMS - Virginia Institute of Marine Science
10 ETH Zürich - Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich]
11 NIA - National Institute of Aerospace [Hampton]
12 LOA - Laboratoire d’Optique Atmosphérique - UMR 8518
13 Smith and Williamson Inc
N. Rastogi
- Function : Author
- PersonId : 2429
- IdHAL : nalin-rastogi
- ORCID : 0000-0002-7199-7747
- IdRef : 069286973
P. R. Sinha
- Function : Author
S. Kumar
- Function : Author
- PersonId : 755286
- ORCID : 0000-0002-1065-9883
I. Shevchenko
- Function : Author
J Smith
- Function : Author
H. Liu
- Function : Author
- PersonId : 773883
- ORCID : 0000-0003-2300-2626
Gwenaël Berthet
- Function : Author
- PersonId : 18957
- IdHAL : gwenael-berthet
- ORCID : 0000-0003-3169-1636
- IdRef : 070409153
Fabrice Jegou
- Function : Author
- PersonId : 181480
- IdHAL : fabrice-jegou
- ORCID : 0000-0003-3527-1399
Jean-Baptiste Renard
- Function : Author
- PersonId : 1027086
Abstract
We describe and show results from a series of field campaigns using balloon-borne instruments launched from India and Saudi Arabia during the summers 2014-2017 to study the nature, formation and impacts of the Asian Tropopause Aerosol Layer (ATAL). The campaign goals were to i) characterize the optical, physical and chemical properties of the ATAL, ii) assess its impacts on water vapor and ozone, and iii) understand the role of convection in its formation. In order to address these objectives, we launched 68 balloons from 4 locations, one in Saudi-Arabia and 3 in India, with payload weights ranging from 1.5 kg to 50 kg. We measured meteorological parameters, ozone, water vapor, and aerosol backscatter, concentration, volatility and composition in the Upper Troposphere and Lower Stratosphere (UTLS) region. We found peaks in aerosol concentrations of up to 25 part/cm3 for radius > 75 nm, associated with Scattering Ratio at 940 nm of ~1.9 near the cold point tropopause. During medium-duration balloon flights near the tropopause, we collected aerosols and found, after offline ion chromatography analysis, the dominant presence of nitrate ions with a concentration of about 100 ng/m3. Deep convection was found to influence aerosol loadings 1 km above the cold point tropopause. The BATAL project will continue for the next 3-4 years and the results gathered will be used to formulate a future NASA-ISRO airborne campaign with NASA high altitude aircraft.
Domains
Meteorology
Origin : Files produced by the author(s)
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