Shallow cumulus clouds in the trade-wind regions cool the planet by reflecting solar
radiation. The response of trade cumulus clouds to climate change is a key uncertainty in …

The trade wind subcloud layer is an important structural component of the atmosphere. Its
thermodynamic variability has long been characterized using simple frameworks, of which …

Understanding the drivers of cloud organization is crucial for accurately estimating cloud
feedbacks and their contribution to climate warming. Shallow mesoscale circulations are …

In early 2020, an international team set out to investigate trade wind cumulus and their
coupling to the large-scale circulation through the field campaign EUREC 4 A: ElUcidating …

The response of trade cumulus clouds to warming remains a major source of uncertainty for
climate sensitivity. Recent studies have highlighted the role of the cloud–convection …

The transition layer in the trades has long been observed and simulated, but the physical
processes producing its structure remain little investigated. Using extensive observations …

The imprint of marine atmospheric boundary layer (MABL) dynamical structures on sea
surface roughness, as seen from Sentinel‐1 synthetic aperture radar (SAR) acquisitions, is …

During the EUREC 4 A field study, microwave radiometric measurements were performed at
Barbados Cloud Observatory (BCO) and aboard RV Meteor and RV Maria S Merian in the …

Although airborne optical array probes (OAPs) have existed for decades, our ability to
maximize extraction of meaningful morphological information from the images produced by …

Naturally available, stable, and heavy water molecules such as HDO and H 2 18 O have a
lower saturation vapour pressure than the most abundant light water molecule H 2 16 O; …