TY - JOUR
T1 - Measurement report
T2 - Altitudinal variation of cloud condensation nuclei activation across the Indo-Gangetic Plain prior to monsoon onset and during peak monsoon periods: Results from the SWAAMI field campaign
AU - Manoj, Mohanan R.
AU - Satheesh, Sreedharan K.
AU - Moorthy, Krishnaswamy K.
AU - Trembath, Jamie
AU - Coe, Hugh
N1 - Funding Information:
Airborne data were obtained using the BAe-146-301 Atmospheric Research Aircraft flown by Airtask Ltd and managed by FAAM Airborne Laboratory, jointly operated by UKRI and the University of Leeds. We thank Divecha Centre for Climate Change for the support. ERA-Interim wind field data were provided courtesy of IMD. The gridded rainfall data were provided courtesy of ECMWF. We also thank the NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT model used in this publication. Sreedha-ran Krishnakumari Satheesh was supported by a J. C. Bose Fellowship and the Tata Education and Development Trust.
Publisher Copyright:
© Copyright:
PY - 2021/6/14
Y1 - 2021/6/14
N2 - Vertical distributions (altitude profiles) of condensation nuclei (CN) and cloud condensation nuclei (CCN) and their spatial variations across the Indo-Gangetic Plain (IGP) have been investigated based on airborne measurements carried out during the SWAAMI field campaign (June to July 2016) capturing the contrasting phases of the Indian monsoon activity in 2016 just prior to its onset and during its active phase. Prior to the monsoon onset, high concentrations of CN and CCN prevailed across the IGP, and the profiles revealed frequent occurrence of elevated layers (in the altitude range 1-3ĝkm). Highest concentrations and elevated peaks with high values occurred over the central IGP. The scenario changed dramatically during the active phase of the monsoon, when the CN and CCN concentrations dropped (CN by 20ĝ% to 30ĝ% and CCN by 6ĝ% to 25ĝ%) throughout the IGP with more pronounced changes at altitudes higher than 3ĝkm where decreases as high as >ĝ80ĝ% were observed. These reductions have an east-to-west decreasing gradient, being most remarkable in the eastern IGP and very weak over the western IGP where the CN concentrations above 3ĝkm increased during the monsoon. The activation ratios (ARs) showed contrasting features, increasing with increase in altitude, prior to the onset of monsoon, reversing the trend to decrease with increase in altitude during the active phase of the monsoon. The supersaturation spectrum became flatter during the active phase of the monsoon, indicating an increase in the hygroscopicity of aerosols following the mixing of surface-based emissions with the advected marine air mass.
AB - Vertical distributions (altitude profiles) of condensation nuclei (CN) and cloud condensation nuclei (CCN) and their spatial variations across the Indo-Gangetic Plain (IGP) have been investigated based on airborne measurements carried out during the SWAAMI field campaign (June to July 2016) capturing the contrasting phases of the Indian monsoon activity in 2016 just prior to its onset and during its active phase. Prior to the monsoon onset, high concentrations of CN and CCN prevailed across the IGP, and the profiles revealed frequent occurrence of elevated layers (in the altitude range 1-3ĝkm). Highest concentrations and elevated peaks with high values occurred over the central IGP. The scenario changed dramatically during the active phase of the monsoon, when the CN and CCN concentrations dropped (CN by 20ĝ% to 30ĝ% and CCN by 6ĝ% to 25ĝ%) throughout the IGP with more pronounced changes at altitudes higher than 3ĝkm where decreases as high as >ĝ80ĝ% were observed. These reductions have an east-to-west decreasing gradient, being most remarkable in the eastern IGP and very weak over the western IGP where the CN concentrations above 3ĝkm increased during the monsoon. The activation ratios (ARs) showed contrasting features, increasing with increase in altitude, prior to the onset of monsoon, reversing the trend to decrease with increase in altitude during the active phase of the monsoon. The supersaturation spectrum became flatter during the active phase of the monsoon, indicating an increase in the hygroscopicity of aerosols following the mixing of surface-based emissions with the advected marine air mass.
U2 - 10.5194/acp-21-8979-2021
DO - 10.5194/acp-21-8979-2021
M3 - Article
AN - SCOPUS:85108121180
SN - 1680-7316
VL - 21
SP - 8979
EP - 8997
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 11
ER -