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Earth and Space - The Water Cycle and Weather Patterns

Grade 5IB

Review the key concepts, formulae, and examples before starting your quiz.

🔑Concepts

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The Water Cycle, also known as the hydrologic cycle, describes the continuous movement of water on, above, and below the surface of the Earth through various states of H2OH_2O.

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Evaporation is the process where liquid water (H2O(l)H_2O_{(l)}) absorbs solar energy and transforms into water vapor (H2O(g)H_2O_{(g)}).

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Transpiration is a biological process where plants release water vapor (H2O(g)H_2O_{(g)}) into the atmosphere through small pores in their leaves called stomata.

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Condensation occurs when water vapor (H2O(g)H_2O_{(g)}) loses thermal energy and cools down to form liquid water droplets (H2O(l)H_2O_{(l)}), which cluster together to form clouds.

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Precipitation is the product of condensation that falls under gravity, including rain, snow (H2O(s)H_2O_{(s)}), sleet, or hail.

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Weather patterns are influenced by the interaction of solar radiation, the atmosphere, and the water cycle, measured by variables like temperature (TT), air pressure (PP), and humidity.

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Air Pressure is the weight of the atmosphere pressing down on Earth. Changes in pressure often indicate changes in weather; for example, low pressure often brings clouds and precipitation.

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Humidity is the amount of water vapor present in the air. Relative humidity is expressed as a percentage (%) of the maximum amount of moisture the air can hold at a specific temperature.

📐Formulae

H2O(l)+Heat Energy→H2O(g)H_2O_{(l)} + \text{Heat Energy} \rightarrow H_2O_{(g)}

H2O(g)−Heat Energy→H2O(l)H_2O_{(g)} - \text{Heat Energy} \rightarrow H_2O_{(l)}

Relative Humidity=(Actual Water VaporMaximum Water Vapor Capacity)×100%\text{Relative Humidity} = \left( \frac{\text{Actual Water Vapor}}{\text{Maximum Water Vapor Capacity}} \right) \times 100\%

TCelsius=59(TFahrenheit−32)T_{Celsius} = \frac{5}{9}(T_{Fahrenheit} - 32)

💡Examples

Problem 1:

During a sunny afternoon, the temperature is 30∘C30^{\circ}C. A puddle of water (H2O(l)H_2O_{(l)}) disappears after a few hours. What process occurred, and what happened to the energy?

Solution:

The process is evaporation.

Explanation:

The liquid water molecules (H2O(l)H_2O_{(l)}) absorbed thermal energy from the Sun, increasing their kinetic energy until they transitioned into a gaseous state (H2O(g)H_2O_{(g)}).

Problem 2:

A weather station records that the air contains 10g/m310g/m^3 of water vapor, but the air at that temperature can hold a maximum of 20g/m320g/m^3. Calculate the Relative Humidity.

Solution:

Relative Humidity=(1020)×100%=50%\text{Relative Humidity} = \left( \frac{10}{20} \right) \times 100\% = 50\%

Explanation:

Relative humidity is the ratio of current water vapor to the maximum possible water vapor the air can hold at that temperature, expressed as a percentage.

Problem 3:

Explain why dew forms on grass in the early morning when the temperature drops to 10∘C10^{\circ}C.

Solution:

This is caused by condensation.

Explanation:

As the temperature (TT) decreases at night, the air can hold less H2O(g)H_2O_{(g)}. When the air cools to its dew point, the water vapor loses energy and changes phase back into liquid droplets (H2O(l)H_2O_{(l)}) on cool surfaces.