Pakistani sporadic and local collisions.Pakistan is in a

Pakistani rain differs greatly in size, timing, and air distribution. Nearly two thirds of the rains are concentrated during the three summer months of July and September. The average annual rainfall on the Indus bottom falls below 100 mm below 750 mm near the Indo-Superiore ski area.There are two major headquarters in Pakistan: monsoons and western riots. For most canal managers, the relative proportion of sludge is low compared to two other irrigation water, ie with sewerage and underground water. More than 60% of Harifu’s seasonal rainfall is concentrated on almost all control channels by mid-July.Monsoons come from the Bay of Bengal and usually travel to Pakistan in early July after crossing India. Continue to September. Indus Plains will receive most of the monsoon rain. Two storms in Pakistan: (1) from April to June (2) from October to November. These periods are the driest parts of the year, especially in October and November. At this time, storms are caused by convection of sporadic and local collisions.Pakistan is in a dry and semi-dry climate zone. The entire Indus area will receive 212 millimeters (confidence interval 95 ± 28%) and 53 millimeters (95% confidence interval ± 8) in the seasonal high season Harida and Rabbi.The rain varies when we move north and northeast to the south. Only the Northwest Border Provinces (NWFP) and Central Punjab North Csatornaparancsai suffer from severe rainfall in the summer and winter. Channel channels over bicycle stations (for example, NWFP) receive almost 55% of annual rainfall in Harif’s season. The Upper and Lower Indian Channels in the Harif period receive 75% and 85-90% of annual precipitation. The annual variability of precipitation increases with southward movement. The dominant area of ??Guddu and Sukkur dams is located in the area with the highest variability.Based on the ten-year average (1990-1999), the annual rainfall of the Meteorological Department in Pakistan in some major cities is as follows: