Use the following information to answer question two to the best of your ability or knowledge qualitativeconversioneducational maticant interpretEarth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyahoga Community CollegeTable 2.-Rainfall intensity and duration patterns for North Platte, NE**D.M. Herschfield; 1961; Rainfall Frequency Atlas of the United States; U.S. Weather Bureau.Frequency of rainfall eventDuration of rainfall event and total rainfall (in)30 minutes1 hour2 hours1 year0.91.11.22 years5 years10 years100 years1.11.41.51.51.92.11.82.22.52.63.43.72. For the North Platte, NE data set plot frequency (years) on x-axis versus total 30-minuterainfall (in) on y-axis. Connect the dots with a colored pencil. Make curves for the 1 hour and2 hours data in the same way. Label axes and include units in parentheses. Include a title foryour graph and a legend for colors that correspond to the different duration curves.Look at the amount that is occurring at a frequency of 1 year: At the rainfall rate of the 30-minuteevent, how much total rain would be expected to fall in an hour?a. (show your work)b. Since this doesn't match the total rainfall for the 1-hour rainfall event, what does it say about therainfall intensity of the shorter duration events?Restricted infiltration and ponding result in poor soil aeration. This leads to poor root function, poorplant growth, nitrogen volatilization, reduced availability of nutrients for plant use, and reduced cyclingof nutrients by soil organisms.The soil infiltration rate is most affected by conditions near the soil surface, and the rate can changedrastically as a result of management. Infiltration is rapid through large continuous pores at the soilsurface, and it slows as pores become smaller. Steady-state infiltration rates typically occur when thesoil is nearly saturated. These rates are given for various textural classes in table 3. They areaverage values and should not be generalized for all soil types.Table 3.-Steady-state infiltration rates*(Soils are wet deep into the profile. Values should be used only for comparing to the infiltration rate of the second inch ofwater applied.) *Hillel, 1982.Soil texture & type Steady-state infiltration rate (in/hr)Sand0.8Sandy and silty soils 0.4-0.8Loam0.2-0.4Clayey soils0.04-0.2Sodic clayey soils

Question

Use the following information to answer question two to the best of your ability or knowledge qualitativeconversioneducational maticant interpretEarth SUPPLEMENTAL EXERCISES - ESCI 103L - Cuyahoga Community CollegeTable 2.-Rainfall intensity and duration patterns for North Platte, NE**D.M. Herschfield; 1961; Rainfall Frequency Atlas of the United States; U.S. Weather Bureau.Frequency of rainfall eventDuration of rainfall event and total rainfall (in)30 minutes1 hour2 hours1 year0.91.11.22 years5 years10 years100 years1.11.41.51.51.92.11.82.22.52.63.43.72. For the North Platte, NE data set plot frequency (years) on x-axis versus total 30-minuterainfall (in) on y-axis. Connect the dots with a colored pencil. Make curves for the 1 hour and2 hours data in the same way. Label axes and include units in parentheses. Include a title foryour graph and a legend for colors that correspond to the different duration curves.Look at the amount that is occurring at a frequency of 1 year: At the rainfall rate of the 30-minuteevent, how much total rain would be expected to fall in an hour?a. (show your work)b. Since this doesn't match the total rainfall for the 1-hour rainfall event, what does it say about therainfall intensity of the shorter duration events?Restricted infiltration and ponding result in poor soil aeration. This leads to poor root function, poorplant growth, nitrogen volatilization, reduced availability of nutrients for plant use, and reduced cyclingof nutrients by soil organisms.The soil infiltration rate is most affected by conditions near the soil surface, and the rate can changedrastically as a result of management. Infiltration is rapid through large continuous pores at the soilsurface, and it slows as pores become smaller. Steady-state infiltration rates typically occur when thesoil is nearly saturated. These rates are given for various textural classes in table 3. They areaverage values and should not be generalized for all soil types.Table 3.-Steady-state infiltration rates*(Soils are wet deep into the profile. Values should be used only for comparing to the infiltration rate of the second inch ofwater applied.) *Hillel, 1982.Soil texture & type Steady-state infiltration rate (in/hr)Sand>0.8Sandy and silty soils 0.4-0.8Loam0.2-0.4Clayey soils0.04-0.2Sodic clayey soils<0.0412Edited from D. Steer, The Good Earth. Also created by K. Sasowsky (Sup. Ex.3, 7, 6a, parts of Sup. Ex. A&B, part, 24, 25, 38, Sup. Alt. Energy 1 and 2, Sup. Switchthe Energy Project Discussion Questions); copyrights retained by authors, 2021.

Accepted Answer

Rainfall rate is the measurement of precipitation over a defined area within a specific time frame,…