Answer:
A dry-line is a line over a territory that detaches wet air and dry air. One of the most unquestionable cases of such a division Happens in central North America especially in Texas , Oklahoma and Kansas where the wet air from the Bay of Mexico meets dry air from desert south - western states.
Tempests were generally conceivable as the dry-line approaches. The temperature may ascend after the dry-line outperforms away, in light of the fact that evaporate air warms more rapidly than damp air. The dry-line are very much reported on a superficial level maps by a ran yellow line.
All of the above options are reasonable for dry-line to happen.
South Western and South Eastern breezes - in the event that we consider Rocky mountains in US which separate the warm clammy air from the South-east which are windy, from the dry air from South-west piece of US .
High temperature - After the dry lines goes there is a chance of high temperature over the locale in light of the fact that the evaporate air warms more rapidly than wet air.
Low Dew focuses and High Dew focuses - Considering the rough mountains , Dew focuses along the east of the dry-line, extend from the upper 40 degrees to low 60 degrees, with twists from the southeast. Presently considering Along the West of the dry-line, dew focuses are a lot of lower, in the 20 degree and 30 degree, which is just about 40 degrees not exactly those found along the east of the dry-line.