Abstract. We are building a 3D description of upper tropospheric
(UT) cloud systems in order to study the relation between convection and
cirrus anvils. For this purpose we used cloud data from the Atmospheric
InfraRed Sounder and the Infrared Atmospheric Sounding Interferometer and
atmospheric and surface properties from the meteorological reanalyses
ERA-Interim and machine learning techniques. The different artificial neural
network models were trained on collocated radar–lidar data from the
A-Train in order to add cloud top height, cloud vertical extent and cloud
layering, as well as a rain intensity classification to describe the UT
cloud systems. The latter has an accuracy of about 65 % to 70 % and allows
us to build objects of strong precipitation, used to identify convective
organization. This rain intensity classification is more efficient to detect
large latent heating than cold cloud temperature. In combination with a
cloud system analysis, we found that deeper convection leads to larger heavy
rain areas and a larger detrainment, with a slightly smaller thick anvil
emissivity. This kind of analysis can be used for a process-oriented
evaluation of convective precipitation parameterizations in climate models.
Furthermore, we have shown the usefulness of our data to investigate tropical
convective organization metrics. A comparison of different tropical
convective organization indices and proxies to define convective areas has
revealed that all indices show a similar annual cycle in convective
organization, in phase with convective core height and anvil detrainment.
The geographical patterns and magnitudes in radiative heating rate
interannual changes with respect to one specific convective organization
index (Iorg) for the period 2008 to 2018 are similar to the ones
related to the El Niño–Southern Oscillation. However, since the
interannual anomalies of the convective organization indices are very small
and noisy, it was impossible to find a coherent relationship with those of
other tropical mean variables such as surface temperature, thin cirrus area
or subsidence area.