Atmospheric aerosols affect the Earth's climate in many ways, including acting as the seeds
on which cloud droplets form. Since a large fraction of these particles is anthropogenic, the …

The liquid water path (LWP) adjustment due to aerosol–cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …

The estimation of cloud radiative forcing due to aerosol‐cloud interactions, RFaci (also
known as the first indirect effect), relies on approximating the cloud albedo susceptibility to …

Clouds play a significant role in weather forecasts, water cycle, and climate system.
However, existing methods ignore the relations of ground‐based cloud images. In this letter …

We compare turbulence properties in coupled and decoupled marine stratocumulus-topped
boundary layers (STBLs) using high-resolution in situ measurements performed by the …

We have analyzed near-global stratospheric data (and mesospheric data as well for H 2 O)
in terms of absolute abundances, variability, and trends for O 3, H 2 O, HCl, N 2 O, and HNO …

Impact of clouds and their vertical structures on the radiative budget, hydrological cycle, and
climate is strong but still uncertain. There is a need to monitor and investigate cloud …

Satellite-based cloud base and top height (CBH and CTH) and cloud geometrical thickness
(CGT) are validated against ground-based lidar measurements and provide new scientific …

A technique is presented that uses attenuated backscatter profiles from the CALIOP satellite
lidar to estimate cloud base heights of lower-troposphere liquid clouds (cloud base height …

An initially well‐mixed stratocumulus deck can remain overcast for several tens of hours
under warm‐advection conditions, although moisture supply is cut off from the ocean due to …