capping inversion造句
例句与造句
- However, the presence of a capping inversion prevented thunderstorms from developing.
- Such capping inversions typically precede the development of tornadoes in the Midwestern United States.
- This is known as a capping inversion.
- Surface cooling causes a small capping inversion to form aloft allowing the air to become stable.
- A " cap " or capping inversion is usually required to form an updraft of sufficient strength.
- It's difficult to find capping inversion in a sentence. 用capping inversion造句挺难的
- Potential temperature, wind speed has a sharp increase across the capping inversion, while moisture has a sharp decrease.
- However, if the air at the surface is unstable enough, strong updrafts can be forced through the capping inversion.
- This layer extends from the earth surface to a capping inversion that typically locates at a height of 1 2 km by midafternoon over land.
- If the capping inversion layer or " cap " is too strong ( too close to the surface ), it will prevent thunderstorms from developing.
- When the thermals reach the capping inversion at the top of the residual layer, they meet resistance to vertical motion and the mixed layer growth rate rapidly decreases.
- A strong capping inversion suppressed thunderstorm development until near sunset, when a supercell thunderstorm developed in the western part of Hennepin County ahead of an advancing cold front near a surface low pressure center.
- One of the many factors that forecasters must ponder before predicting severe thunderstorms is the strength of a capping inversion, a layer of air near 5, 000 feet in which temperature increases with increasing altitude.
- A capping inversion occurs when there is a boundary layer with a normal temperature profile ( warm air rising into cooler air ) and the layer above that is an inversion layer ( cooler air below warm air ).
- Below the capping inversion ( 10-60 % of CBL depth, also called entrainment zone in the daytime ), CBL is divided into two sub-layers : mixed layer ( 35-80 % of CBL depth ) and surface layer ( 5-10 % of CBL depth ).
- Thunderstorm activity across Oklahoma during the mid-afternoon hours was largely limited to far northern parts of the state due in part to a capping inversion that did not erode farther south until later in the day, aided by a shortwave trough that pushed into the region from the Texas Panhandle and a stronger trough located over Colorado.
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