Abstract. A better understanding of aerosol–cloud interaction processes is important
to quantify the role of clouds and aerosols on the climate system. There
have been significant efforts to explain the ways aerosols modulate cloud
properties. However, from the observational point of view, it is indeed
challenging to observe and/or verify some of these processes because no
single instrument or platform has been proven to be sufficient. Discrimination between
aerosol and cloud is vital for the quantification of aerosol–cloud
interaction. With this motivation, a set of observational field campaigns
named balloon-borne aerosol–cloud interaction studies (BACIS) is proposed
and conducted using balloon-borne in situ measurements in addition to the
ground-based (lidar; mesosphere, stratosphere and troposphere (MST) radar; lower atmospheric wind profiler; microwave radiometer; ceilometer) and space-borne
(CALIPSO) remote sensing instruments from Gadanki (13.45∘ N, 79.2∘ E), India. So far, 15 campaigns have been conducted as a part of BACIS campaigns
from 2017 to 2020. This paper presents the concept of the observational
approach, lists the major objectives of the campaigns, describes the
instruments deployed, and discusses results from selected campaigns.
Balloon-borne measurements of aerosol and cloud backscatter ratio and cloud
particle count are qualitatively assessed using the range-corrected data
from simultaneous observations of ground-based and space-borne lidars.
Aerosol and cloud vertical profiles obtained in multi-instrumental observations
are found to reasonably agree. Apart from this, balloon-borne profiling is
found to provide information on clouds missed by ground-based and/or
space-borne lidar. A combination of the Compact Optical Backscatter AerosoL Detector (COBALD) and Cloud Particle Sensor (CPS) sonde is employed for the first time in this study to discriminate cloud and aerosol in an in situ profile. A threshold value of the COBALD colour index (CI) for ice clouds is found to be between 18 and 20, and CI values for coarse-mode aerosol particles range between 11 and 15. Using the data from balloon measurements, the relationship between cloud and aerosol is quantified for the liquid clouds. A statistically significant slope (aerosol–cloud interaction index) of 0.77 found between aerosol backscatter and cloud particle count reveals the role of aerosol in the cloud activation process. In a nutshell, the results presented here demonstrate the observational approach to quantifying aerosol–cloud interactions.