Weather and Climate

Once students understand how water moves around the planet as the result of sunlight converting to heat energy, they look at how this process drives weather and climate. Specifically, they record and analyze weather data over a period of time, connecting specific weather patterns with the seasons.

• Seasons are times of year that have specific weather patterns and amounts of daylight.
• Different temperatures on Earth aren’t just caused by Earth’s shape. Earth is also tilted on its axis, which means it leans a little to one side. This also affects how much sunlight a particular area on Earth receives.
• Scientists study patterns of weather across different seasons and regions to determine future weather conditions.
• Weather is made up of different factors, and scientists take measurements of all of these parts to help them better understand the weather conditions.
• Scientists analyze weather data from many sources. They use weather balloons, weather stations, and satellites.
• Air is matter, and scientists measure the amount of air molecules in a given area.
• Wind is related to air molecules because wind is moving air.

• Why is it summer in the northern hemisphere at the same time as it is winter in the southern hemisphere?
• How does Earth’s orbit affect the seasons?
• Why do seasons occur predictably every year?
• Are there any patterns in the temperature map that appear in both the winter season and the summer season?
• Why are temperatures lower in the winter season compared to the summer season?
• How is air pressure related to the molecules that make up air? How is air pressure related to weather?
• What kind of weather can we expect if the water in the neck of the glass barometer rises?
• How do scientists measure wind speed? Why is it important for scientists to measure wind speed?

Air Pressure : a measure of the force of air’s weight on Earth’s surface; measured with a barometer

Climate : the average weather over a span of 30 years

Evaporation : the process of liquid water changing into water vapor, its gas state

Precipitation : the process of water falling back to Earth in the form of rain, snow, sleet, or hail

Proportion : the relationship between things, as to size, quantity, or number

Season : a time of year that has specific weather patterns and amounts of daylight

System : a set of connected, interacting parts that form a more complex whole

Temperature : a measure of heat; measured with a thermometer

Water Cycle : the circulation of water from a collection to the atmosphere and back to Earth in

Four Steps: evaporation, condensation, precipitation, collection

Weather : the conditions of the atmosphere (temperature, humidity, wind speed, air pressure, and precipitation) in a particular place at a particular time

Wind Speed : a measure of how fast wind is moving; measured with an anemometer

Sensing the Seasons

Monarch butterflies can sense when to begin their journey south. They can tell when the days start to become shorter.

The changing amounts of daylight are a sign that the seasons are changing. A season is a time of year that has specific weather patterns and amounts of daylight.

Different parts of the world have different seasons and different kinds of weather. For example, the tropical climate zone has two seasons. Its seasons are rainy and dry. The temperate climate zone has four seasons. Its four seasons are summer, fall, winter, and spring.

Earth’s Tilt

Earth has seasons because of Earth’s movement in the solar system. As you read this, you are here on Earth. You probably feel like you are not moving. But Earth is in constant motion.

Earth is always spinning. This is also called rotating. Earth rotates on an imaginary line that goes from the North Pole to the South Pole. This line is called an axis.

Earth’s axis is tilted. This means that it leans a little to one side. Earth completely rotates around its axis about once every 23 hours and 56 minutes. This equals one Earth day.

As Earth rotates, part of the planet gets light, and then dark. The sun always shines, but its light only hits one half of the planet at a time.

Because of Earth’s tilt, half of Earth is always tilted toward the sun. The part of Earth tilted toward the sun gets more direct sunlight than the part of Earth tilted away from the sun.

 

For the hands-on activity of this lesson, students create a model weather station to collect and analyze daily weather data locally, and then compare weather patterns in two different locations.

Students analyze and graph data about wind speed, air pressure, temperature, and general weather conditions over the course of five days. Students use their weather station data and temperature comparisons to analyze weather patterns, connecting the weather conditions with a region and the seasons.