For a catchment isohyets are drawn and area is calculated using planimeter as shown in figure. The average precipitation over the catchment area is mm. A 55.06 mm B 62.53 mm C 75.53 mm D 71.31 mm A₁-40 sq. km A₂ = 62 sq. km P₁ = 50 mm A₂ = 65 sq. km P₂=75 mm P₁ = 85 mm A₂-70 sq. km P₁ = 110 mm

Q: In a border-irrigation-system, the following information is given The border length is 300 m The…

A: Boundary irrigation is a kind of surface irrigation in which the field is split into strips by…

Q: Q1/Separate the given hydrograph in to its components using method four, if the catchment area is…

A: Time(day)Direct runoff Discharge (m3/s112228318041900522006120072308100910010601120121513121410

Q: A 프 B Water flows at the rate of 21.6 [cfs] from reservoir A to reservoir B through two cast iron…

A:

Q: What is the negative deviation value in this diagram 600 550- *Observed inflow adjusted for…

A: Given data- Mass-inflow variation with year is given in the form graph as shown-

Q: boundaries. Create a chart like Figure 1.5 illustrating fluxes in the b Estimate the average annual…

A:

Q: 8. Route the inflow hydrograph in the following table through a river reach for which x = 0.2 and K…

A: given data k=2daystable is given with time and inflow dataFindroute of inflow htdrograph

Q: Find area precipitation by isohyetal method for a certain catchment area given the following data

A:

Q: Year Rainfall (mm) Year Rainfall (mm) 1994 28.2 2004 31.5 1995 31.2 2005 42.5 1996 34.4 2006 39.5…

A: year rainfall increasing order 1994 28.2 20.5 1995 31.2 23.6 1996 34.4 25.4 1997 39.0 27.2…

Q: 10-min unit hydrograph for a catchment is given in Table 1 below. Table 1: 10-min Unit Hydrograph…

A: Given Data is of a Unit hydrograph. Time has been given in minutes Discharge is given in m3/s…

Q: use ripple diagram or cumulative mass curve ,estimate the active reservoir capacity to supply…

A: See explanation below:Explanation:Plot the cumulative mass curve using Python:import pandas as pd…

Precipitation

Precipitation forms the basis of the water cycle on the Earth. The air is packed with water molecules in the form of moisture or water vapor. This water vapor usually rises to the atmosphere due to density differences. Precipitation represents any form of water, in liquid form or frozen form that forms in the earth's atmosphere. The water vapor up in the atmosphere condenses due to low temperature and it leads to the formation of clouds. The water vapor that forms clouds on account of condensation, is preferably known as cloud droplet. These cloud droplets when become heavy and can no longer sustain the weight of condensed water droplets, they come to the Earth in the form of rain, snow, ice pellets, and hail. Precipitation patterns, evaporation, and condensation are the three parameters that decide the global water cycle, climate change, and weather. Additionally, smoke and dust particles are equally important parameters for precipitation, as they provide the surface area for the water vapors to get condensed and to form water droplets. So they are known as condensation nuclei. The presence of other pollutants in the air also serves as condensation nuclei. Precipitation always results in the pure water supply to earth, as the salt from the seawater does not evaporate with the water.