Examples of 'deep convection' in a sentence
Meaning of "deep convection"
deep convection - It describes the process in meteorology where warm air rises, cools, condenses, and forms clouds or storms
How to use "deep convection" in a sentence
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deep convection
Deep convection continuing near the center.
Curvature in the deep convection to the west.
Deep convection seems to be more impressive today.
One important process is deep convection itself.
Deep convection continued to accelerate.
Exposed to the southwest of the deep convection.
Deep convection rapidly dissipated shortly thereafter due to interaction with land.
The associated area of deep convection.
The central area of deep convection moved across every island in the archipelago.
The wave was associated with some curvature of deep convection.
The deep convection continued to build along with the strong equatorward outflow.
The south of the deep convection.
The deep convection warmed slightly and underwent slight fluctuations during the afternoon.
Main area of deep convection.
This tropical disturbance has an extensive area of deep convection.
See also
The latent heating induced by deep convection also affects gravity wave drag.
And had lost much of its associated deep convection.
The low maintained an area of deep convection and quickly strengthened into a tropical storm.
It is caused by a discontinuity in hydrogen abundance left behind by the deep convection.
The associated deep convection.
An approaching trough caused the storm to stall and weaken the deep convection.
The weakening trend slowed that afternoon as deep convection returned to the disorganized storm.
Deep convection developed around the center with strong outflow towards the north.
An important source is latent heat release due to deep convection in the tropics.
Deep convection formed near the center and the storm began transitioning to a warm core system.
The depression was already exhibiting persistent deep convection in the western portion of its circulation.
The mechanism creating these rocket dust storms on Mars is called a deep convection.
Satellite imagery shows flaring deep convection over a consolidating low level circulation center.
It then moved over relatively cooler waters and weakened as the deep convection quickly vanished.
The system maintained scattered deep convection across offshore waters and environmental conditions favored tropical cyclogenesis.
It developed a well-defined center with concentrated deep convection.
However, deep convection persisted around the center.
The storm continued to the southwest while deep convection persisted near the center.
However, deep convection gradually organized around the center.
O Fritsch-Chappel type deep convection scheme.
Deep convection had started to form over a low-level circulation center.
By the night, only minimal deep convection remained.
Deep convection was flaring around the low-level circulation center.
The associated rain-causing mechanisms mainly involve deep convection.
Clustering, deep convection around the center is a sign of a healthy tropical cyclone.
Late that evening, new bursts of deep convection developed with the storm.
Deep convection weakened somewhat and the eye had become cloud-filled.
A microwave satellite image of the storm depicted an eye-feature surrounded by deep convection.
Deep convection formed around a prominent mid-level circulation as it moved towards the west.
The cyclone turned to the south, and lost its associated deep convection.
Early the next day, deep convection persisted in a small area northeast of the center.
By that time, the system had a well-defined eye in the center of deep convection.
During its weakening stage, deep convection existed only in the northwestern quadrant of the circulation.
After several days, an associated area of low pressure gained deep convection and organization.
Little deep convection remained associated with the system, and the cyclone stayed stationary.
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