Please help me solve the following MATLAB problems. This is one single question but has 12 requirements which needs to be solved sequentially. The question 2 which this question is referring to is provided right at the bottom and is titled "This is question 2" . Any help provided will be greatly appreciated. The answers to the problems will be used to verify my own work and prepare for exams. Thank you.

THE QUESTION 2 WHICH THE ABOVE QUESTION IS REFERRING TO IS PROVIDED BELOW:

Introduction Your tesk is to determine if the dam from Question 2 is sufficient for the farmer's needs based on the year's rainfall and consumption. Assume thst at the start of July, the depth of the wster in the middle of the dam is 2 Any dates for which there is no rainfall reading should take the worst-case scenario: no rainfall. You are to test the following scenarios: 1. The dam has shape 1 from Qustion 2, there are 2 m per day of water used from the dam and there is no rainfall 2. The same as scenario 1, except the dam has shape 2 from Question 2. 3. The same as scenario 2, except there is rainfall. . The same as scenario 3, except there are (4+9.8007) In per day of water used from the 5. The same as scenario 3, except the depth of water in the middle of the dsm is initially To test these scenarios, you are to record the depth of wster in the middle of the dam at To model the evsporation, use the Penman equstion. This isn't the most accurste model, dam and the depth of water in the middle of the dam is initially 4 m. m and there is also evsporation. the start of each day. but it is one of the simplest to calculate. The Shuttleworth formulation2 of the evaporstion rate (in mm/day)is: (13) where dpsa (14) (15) (16) Pexp 19.05- 0.001628Gp The ssturation pressure is Pss (the formuls is an spproximation from Ref.), the psychrometric constant is , p is the atmospheric pressure (in kPa), T is the atmospheric temperature (in K), U is the wind speed (in m/s), is the relative humidity (0 1), and Au-2.443 MJ/kg is the latent hest of vaporisation of water. The solar insolstion for Dalby can be approximated by: (17) where d is the day of the year (1st January: d- 1; 31st December: d- 365). In order for the answer for Eq. (13) to be in the correct units, all the quantities must be calculated using the units as ststed. Use the values at 3:00 pm as representative of the relevant atmospheric values Requirements For this sssessment item, you must perform hand calculations: 1. Calculate the depth of water after 4 days and after 365 days for scenario 1 i.e. derive an analytical solution for the depth as a function of time and use thst formuls to calculste the depth of water) Introduction Your tesk is to determine if the dam from Question 2 is sufficient for the farmer's needs based on the year's rainfall and consumption. Assume thst at the start of July, the depth of the wster in the middle of the dam is 2 Any dates for which there is no rainfall reading should take the worst-case scenario: no rainfall. You are to test the following scenarios: 1. The dam has shape 1 from Qustion 2, there are 2 m per day of water used from the dam and there is no rainfall 2. The same as scenario 1, except the dam has shape 2 from Question 2. 3. The same as scenario 2, except there is rainfall. . The same as scenario 3, except there are (4+9.8007) In per day of water used from the 5. The same as scenario 3, except the depth of water in the middle of the dsm is initially To test these scenarios, you are to record the depth of wster in the middle of the dam at To model the evsporation, use the Penman equstion. This isn't the most accurste model, dam and the depth of water in the middle of the dam is initially 4 m. m and there is also evsporation. the start of each day. but it is one of the simplest to calculate. The Shuttleworth formulation2 of the evaporstion rate (in mm/day)is: (13) where dpsa (14) (15) (16) Pexp 19.05- 0.001628Gp The ssturation pressure is Pss (the formuls is an spproximation from Ref.), the psychrometric constant is , p is the atmospheric pressure (in kPa), T is the atmospheric temperature (in K), U is the wind speed (in m/s), is the relative humidity (0 1), and Au-2.443 MJ/kg is the latent hest of vaporisation of water. The solar insolstion for Dalby can be approximated by: (17) where d is the day of the year (1st January: d- 1; 31st December: d- 365). In order for the answer for Eq. (13) to be in the correct units, all the quantities must be calculated using the units as ststed. Use the values at 3:00 pm as representative of the relevant atmospheric values Requirements For this sssessment item, you must perform hand calculations: 1. Calculate the depth of water after 4 days and after 365 days for scenario 1 i.e. derive an analytical solution for the depth as a function of time and use thst formuls to calculste the depth of water)