Application:
Everyone knows that Ramona gets hot in the summertime! To es- cape the heat, you can drive up to Big Bear and relax in the cool pines. It’s cooler at Big Bear, but how much cooler? Turns out that science has an answer for that! The Adiabatic Lapse Rate can be used to calculate how much cooler Big Bear at 6,752 feet above sea level will be from Ramona at 1,395 feet. In this project you will pro- gram should use the standard dry Adiabatic Lapse Rate (given be- low) to determine what the temperature at Big Bear is given the temperature in Ramona, oh, and, one more thing, we only have the temperature in Ramona in Celsius but we need to know the tem- perature in Big Bear in Fahrenheit!
Processing Guidelines:
1. Declare the needed variables of the appropriate data types. Names of the variables should be meaningful.
2. Ask the user to enter the temperature in Ramona (Celsius), the elevation in Ramona and the elevation in Big Bear. Assign these values to the variables. This is so we can use the program for any temperature and elevation change.
3. Your program should then calculate the temperature at Big Bear in Fahrenheit given the inputs from the user. The dry Adiabatic Lapse Rate says that the Fahrenheit temperature will fall by 5.38 degrees for every 1000 feet in elevation change.
4. Generate the output (to both the screen and to a disk file)
