The term "more stratiform" is an adjective used to describe a specific type of cloud formation or meteorological phenomenon. It refers to a cloud or weather pattern that exhibits an increased degree of stratification or layering.
In meteorology, stratiform clouds are those that appear in sheets or layers, often covering large areas of the sky. They are characterized by their uniform appearance and horizontal development, having smooth, flat bases and often resembling a blanket or a layer of fog. Examples of stratiform clouds include altostratus, nimbostratus, and stratus clouds.
When the term "more stratiform" is used, it indicates that the cloud formation or weather pattern being referred to possesses a higher level of stratification compared to other similar phenomena. This could mean that the clouds are more extensive, with larger coverage across the sky, or that they have more distinct and defined layers. It suggests that the cloud formation is more vertically structured and organized, with a greater visibility of stratification.
The concept of "more stratiform" can also be extended to describe other weather-related phenomena, such as precipitation. For instance, a "more stratiform" rain refers to rainfall that is characterized by a longer duration and more widespread pattern, with a consistent and uniform distribution across an area, as opposed to scattered or isolated showers.
Overall, "more stratiform" is a term used to emphasize and quantify the level of stratification or layering in cloud formations or weather patterns, indicating a higher degree of uniformity and structure.
