Barometric pressure: The air pressure is known as barometric pressure which is measured by barometers. The barometric pressure will be higher at sea level. The pressure changes within the earth’s atmosphere but always within the set range. Humidity: The amount of water vapor present in the atmosphere is known as humidity. The vapor is in invisible gaseous state and it is an important aspect of the atmosphere. Temperature: The heat present in the object is referred as temperature. It is measured with thermometer on scale. The scale can be in Fahrenheit or Celsius units.

Question

The average daily temperature for an area can be approximated using the following equation: T = Tmean + (Tpeak – Tmean) cos (@(t – tpeak) %3D where Tmean is the mean temperature over a year, Tpeak is the highest daily mean temperature, w is the frequency of annual variation, tpeak is the day that the peak temperature occurs, and t represents the days 33 to 400 (inclusive, increments of 1). w has the value 2n/365. A. Write a function that takes Tpeak, tpeak, Tmean and t as inputs (4 inputs) and outputs the following 3 return values: The temperature for for each day The minimum temperature for the year The day with the minimum temperature B. In 2008, Melbourne's temperature statistics were: Tpeak = 25.9°C, tpeak = 13 and Tmean = 19.8°C Use the function you wrote in part A to plot on a single figure the following: Temperature for every day of the year as a black continuous line Use fprintf() to print the minimum temperature and the day it occurred. Then use a red asterisk to mark it on…

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Chapter 5.2, Problem 2RQ

Program Plan Intro

Barometric pressure:

The air pressure is known as barometric pressure which is measured by barometers. The barometric pressure will be higher at sea level. The pressure changes within the earth’s atmosphere but always within the set range.

Humidity:

The amount of water vapor present in the atmosphere is known as humidity. The vapor is in invisible gaseous state and it is an important aspect of the atmosphere.

Temperature:

The heat present in the object is referred as temperature. It is measured with thermometer on scale. The scale can be in Fahrenheit or Celsius units.

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The average daily temperature for an area can be approximated using the following equation: T = Tmean + (Tpeak – Tmean) cos (@(t – tpeak) %3D where Tmean is the mean temperature over a year, Tpeak is the highest daily mean temperature, w is the frequency of annual variation, tpeak is the day that the peak temperature occurs, and t represents the days 33 to 400 (inclusive, increments of 1). w has the value 2n/365. A. Write a function that takes Tpeak, tpeak, Tmean and t as inputs (4 inputs) and outputs the following 3 return values: The temperature for for each day The minimum temperature for the year The day with the minimum temperature B. In 2008, Melbourne's temperature statistics were: Tpeak = 25.9°C, tpeak = 13 and Tmean = 19.8°C Use the function you wrote in part A to plot on a single figure the following: Temperature for every day of the year as a black continuous line Use fprintf() to print the minimum temperature and the day it occurred. Then use a red asterisk to mark it on…

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