Cloud feedbacks are a leading source of uncertainty in the climate sensitivity simulated by
global climate models (GCMs). Low-latitude boundary-layer and cumulus cloud regimes are …

How clouds respond to warming remains the greatest source of uncertainty in climate
projections. Improved computational and observational tools can reduce this uncertainty …

Seamless Stratocumulus Simulation across the Turbulent Gray Zone in: Monthly Weather
Review Volume 142 Issue 4 (2014) Jump to Content Jump to Main Navigation Logo Logo Logo …

Over the last 100 years, boundary layer meteorology grew from the subject of mostly near-
surface observations to a field encompassing diverse atmospheric boundary layers (ABLs) …

A W-Band Radar–Radiometer System for Accurate and Continuous Monitoring of Clouds and
Precipitation in: Journal of Atmospheric and Oceanic Technology Volume 34 Issue 11 (2017) …

The stratocumulus to cumulus transition (SCT) is typically considered to be a slow, multiday
process, caused primarily by dry air entrainment associated with overshooting cumulus, with …

An intercomparison between 10 single-column (SCM) and 5 large-eddy simulation (LES)
models is presented for a radiation fog case study inspired by the Local and Non-local Fog …

Lagrangian large‐eddy simulations of a composite stratocumulus to cumulus transition case
over the subtropical northeast Pacific Ocean are subject to perturbed forcings that isolate the …

We argue that combining direct numerical simulation (DNS) with large‐eddy simulation
(LES) and field studies could accelerate current lines of stratocumulus research. LES allows …

Increased horizontal and vertical resolution in global atmospheric models can reduce a
significant amount of the biases associated with subtropical marine stratocumulus. The …