Stratus clouds are defined as shallow stratiform clouds that are typically less than 1 km thick, presenting a smooth, lower, and more uniform appearance in the sky compared to other cloud.

Stratus clouds present a smoother, lower, more uniform sky than does stratocumulus clouds because the internal convective overturning that produces lighter and darker regions in stratocumulus is nil in.

Chapter 6 provides an overview of the dynamics of fogs and stratocumulus clouds. Included are fog formation mechanisms and various forcing factors tha

Understanding the Context

Fog and low stratus are significantly influencing the earth's radiation balance. At the same time, particularly ground-touching stratus layers (fog with horizontal visibility < 1 km) are an obstacle.

Stratus is the main artificial seeding target for weather modification in Ningxia. Meteorological satellites can detect macro and microcosmic physical parameters of large-scale stratus.

The scheme utilizes a range of pixel-based and novel object-oriented techniques to separate fog and low stratus clouds from other cloud types. Fog and low stratus are identified by a.

Stratus is the name given to an extensive layer or flat patches of low clouds showing hardly any well-defined detail. These names are sometimes used in conjunction. For example, when cirrus is in.

Key Insights

A scheme for satellite remote sensing is proposed to detect nighttime fog and low stratus (FLS) by combining visible, mid-infrared, and far-infrared c

Traditional satellite-based detection of dawn sea fog/low stratus (SFLS) is difficult because of the weak reflectivity in the visible at low solar ele

During the fall and spring seasons within the Arctic Basin north of Alaska, transitions in low cloud types and amounts occur. The summer season produces low-lying stratus cloud over the Arctic.