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Proceedings Paper

Assessment of cirrus cloud and aerosol radiative effect in South-East Asia by ground-based NASA MPLNET lidar network data and CALIPSO satellite measurements
Author(s): Simone Lolli; James R. Campbell; Jasper R. Lewis; Ellsworth J. Welton; Paolo Di Girolamo; Fatkhuroyan Fatkhuroyan; Yu Gu; Jared W. Marquis
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Paper Abstract

Aerosol, together with cirrus clouds, play a fundamental role in the earth-atmosphere system radiation budget, especially at tropical latitudes, where the Earth surface coverage by cirrus cloud can easily reach 70%. In this study we evaluate the combined aerosol and cirrus cloud net radiative effects in a wild and barren region like South East Asia. This part of the world is extremely vulnerable to climate change and it is source of important anthropogenic and natural aerosol emissions. The analysis has been carried out by computing cirrus cloud and aerosol net radiative effects through the Fu-Liou-Gu atmospheric radiative transfer model, adequately adapted to input lidar measurements, at surface and top-of-the atmosphere. The aerosol radiative effects were computed respectively using the retrieved lidar extinction from Cloud-Aerosol Lidar with Orthogonal Polarization in 2011 and 2012 and the lidar on-board of Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations for the South East Asia Region (27N-12S, 77E-132E) with 5° x 5° spatial resolution. To assess the cirrus cloud radiative effect, we used the ground-based Micro Pulse Lidar Network measurements at Singapore permanent observational site. Results put in evidence that strong aerosol emission areas are related on average to a net surface cooling. On the contrary, cirrus cloud radiative effect shows a net daytime positive warming of the system earth-atmosphere. This effect is weak over the ocean where the albedo is lower and never counter-balances the net cooling produced by aerosols. The net cooling is stronger in 2011, with an associated reduction in precipitations by the four of the five rain-gauges stations deployed in three regions as Sumatra, Kalimantan and Java with respect to 2012. We can speculate that aerosol emissions may be associated with lower rainfall, however some very important phenomena as El Nino Southern Oscillation , Madden-Julian Oscillation, Monsoon and Indian Dipole are not considered in the analysis.

Paper Details

Date Published: 13 October 2017
PDF: 7 pages
Proc. SPIE 10424, Remote Sensing of Clouds and the Atmosphere XXII, 1042405 (13 October 2017); doi: 10.1117/12.2278987
Show Author Affiliations
Simone Lolli, NASA Goddard Space Flight Ctr. (United States)
Instituto di Metodologie per l'Analisi Ambientale, CNR (Italy)
James R. Campbell, U.S. Naval Research Lab. (United States)
Jasper R. Lewis, NASA Goddard Space Flight Ctr. (United States)
Ellsworth J. Welton, NASA Goddard Space Flight Ctr. (United States)
Paolo Di Girolamo, Univ. degli Studi della Basilicata (Italy)
Fatkhuroyan Fatkhuroyan, BMKG (Indonesia)
Yu Gu, Univ. of California, Los Angeles (United States)
Jared W. Marquis, Univ. of North Dakota (United States)


Published in SPIE Proceedings Vol. 10424:
Remote Sensing of Clouds and the Atmosphere XXII
Adolfo Comerón; Evgueni I. Kassianov; Klaus Schäfer, Editor(s)

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