Problem 88
Question
When the relative humidity is \(100 \%\) air cools \(5.8^{\circ} \mathrm{F}\) for every 1 -mile increase in altitude. If the temperature is \(80^{\circ} \mathrm{F}\) on the ground, then \(f(x)=80-5.8 x\) calculates the air temperature \(x\) miles above the ground. Find \(f(3)\) and interpret the result. (Source: Battan, \(L\). Weather in Your Life, W.H. Freeman.)
Step-by-Step Solution
Verified Answer
The temperature is \( 62.6^{\circ}F \) at 3 miles altitude.
1Step 1: Substitute the Value of x
First, insert the value of \( x \) into the function \( f(x) = 80 - 5.8x \). Here, we need to find \( f(3) \). So, substitute \( x = 3 \) into the function.
2Step 2: Calculate Expression
Calculate \( f(3) = 80 - 5.8 \times 3 \). Multiply \( 5.8 \) by \( 3 \) to get \( 17.4 \).
3Step 3: Perform Subtraction
Subtract \( 17.4 \) from \( 80 \). This gives \( 80 - 17.4 = 62.6 \).
4Step 4: Interpret the Result
The value \( f(3) = 62.6 \) indicates that when the altitude is 3 miles, the air temperature is \( 62.6^{\circ}F \) under the given conditions.
Key Concepts
Understanding FunctionsReal-World Applications of FunctionsDelving Into Temperature GradientExploring Altitude Effects on Temperature
Understanding Functions
In mathematics, a function is like a machine that takes an input, performs a specific operation, and gives an output. Imagine you have a formula, like a recipe, that tells you how to mix ingredients to get a particular dish. Functions work in a similar way: they use a rule or a formula to transform given numbers (inputs) into new numbers (outputs). For instance, the function \( f(x) = 80 - 5.8x \) creates a connection between altitude (the input \(x\)) and temperature (the output \(f(x)\)).
Here are some key points about functions:
Here are some key points about functions:
- The "\(x\)" is the independent variable, while "\(f(x)\)" is the dependent variable because its value depends on what \(x\) is.
- Each input \(x\) has one unique output \(f(x)\), ensuring that for every altitude, there’s a specific temperature.
- Functions help in modeling real-world situations, providing a simple and systematic way to predict changes.
Real-World Applications of Functions
Functions aren't just abstract mathematical concepts—they are powerful tools that solve real-world problems. In this exercise, the function \( f(x) = 80 - 5.8x \) helps us predict temperature changes as we go higher above the ground. This particular scenario relates to meteorology, which is the study of weather systems.
Real-world applications of functions include:
Real-world applications of functions include:
- Predicting temperature fluctuations at different altitudes for aviation and weather forecasts.
- Modeling financial growth where the input could be time, and the output could be profit or loss.
- Calculating distance over time in physics applications, such as speed or velocity functions.
Delving Into Temperature Gradient
A temperature gradient describes the rate of temperature change over a certain distance or depth. In our exercise, the temperature gradient is \(5.8^{\circ} F\) per mile. This means for every mile you ascend, the temperature cools by \(5.8^{\circ} F\).
Important aspects of temperature gradients:
Important aspects of temperature gradients:
- They show how rapidly temperature changes over a distance, which helps predict environmental conditions.
- A larger gradient indicates a faster change, while a smaller gradient signals a slower change.
- Temperature gradients are crucial for understanding weather patterns and how they might affect various activities like hiking or flying.
Exploring Altitude Effects on Temperature
The exercise highlights a common environmental phenomenon: as altitude increases, the temperature typically decreases. This is due to the thinning atmosphere at higher elevations, which holds less heat.
Here’s why altitude affects temperature:
Here’s why altitude affects temperature:
- With higher altitude, air pressure drops, causing air to expand and its temperature to lower, a process called "adiabatic cooling."
- The thinner air at higher altitudes absorbs less heat from the Earth’s surface.
- Mountains and higher terrains, therefore, are usually cooler than low-lying areas, which is why we often see snow at high elevations even during warmer months.
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