12 minute read
Measuring Weather
Measuring Weather Temperature Temperature is a measure of how hot or cold the air around us is. It is measured in degrees Celsius (oC) or degrees Fahrenheit (oF). Temperature is measured using a thermometer. When the temperature is high, the weather can be described as warm or hot. When the temperature is low, the weather can be described as cool or cold. By using different instruments and technology, we are able to accurately describe and predict weather. We can measure and predict temperature, the strength and direction of wind, or when it will rain. We are also able to predict extreme weather events like thunderstorms and hurricanes. thermometer How does the weather change from day to day? How can we measure weather? old. old education t or red in n hrenheit ( renheit ( a thermomete hermomete gh, the weather he weather or hot. When hot. Whe weather can ather can nd
Advertisement
53
Think Deeply
The summit of Mount Everest is almost 9,000 meters. How would the air pressure at that height compare to the air pressure on the ground?
barometer ba aro ometer e
Air Pressure and Wind
Like all matter, the air in the Earth’s atmosphere osphe has mass. Air pressure is caused by the weight the eight of the air pressing down on the Earth’s surface. s surf In lower areas of the Earth’s surface there is s ace re more air pressing down than high areas. So air n high areas. S pressure is higher at sea level and decreases evel and de with height. Air pressure changes with temperature. When with tempe the heat from the Sun heats the surface of the n heats he Earth, the air surrounding the Earth is heated. undi the E This causes the air to rise and the air pressure to an decreases. The weather changes as the air pressure in an ather changes area changes. Generally, low air pressure will nges. Gener result in bad weather such as strong winds and bad weath rain. High air pressure is associated with calmer igh air pres weather with clearer skies and little wind. ather w th ressure
Air pressure is measured using a barometer.
54
wind sock
Wind is moving air. When the heat from the e Sun warms the air in one area, the air rises and and the air pressure decreases. In places where the th the air is cooler, the air falls and the air pressure e increases. Wind is caused when air moves from an area of high pressure to an area of of f low pressure. The greater the difference in air ence in air pressure, the stronger the wind. We can measure the speed of wind using an anemometer or a wind sock. These tools can also be used to measure the direction the wind is blowing. d using an ese tools ca rection t
anemometer
55
A Closer Look Sea Breezes and Land Breezes s A good example to help understand the relationship between temperature, air pressure and wind is to look at sea breezes and land breezes. During the day, the Sun heats both the land and ocean, but the land gets heated faster. This causes the air above the land to become warmer than the air above the ocean. The air above the land rises and the cool air from the ocean moves to take its place. This causes wind to blow from the ocean to the land. This movement of the air is called a sea breeze. ducation he ts the of the e ucation
During a sea breeze, wind blows from the ocean onto land. R sea br se
56
near-shore wind farm
During the night, there is no Sun in the sky to warm the surface of the Earth. Both the land and the ocean begin to cool. The land cools down faster than the ocean. The warmer air above the ocean rises and the cooler air from the land moves to takes its place. This causes the wind to blow from the land to the ocean. This movement of the air is called a land breeze. Did You Know? Wind farms are often located near the coast. They use the energy in sea breezes and land breezes to generate electricity.ducatio and wn bove the land land the wind to nd to his movement ca a
During a land breeze, wind blows from the land to the ocean. R land b la
57
Precipitation Precipitatio ecipitati
Think Deeply
Water that falls from clouds in the sky is Water that fal called precipitation. There are four main calledll preci Earth is the only known planet types of precipitation – rain, sleet, snow s of pes and hail. The air in our atmosphere contains water in the form of a gas called water vapor. When warm air rises, it begins to cool and the water vapor forms tiny water droplets in clouds. The droplets attach to dust and other particles. As more water droplets form and combine, they form larger drops. The drops fall to Earth as rain. to contain water in three states. What are these three states and where can they be found on Earth? an The air i in the f Whe the i a Rega 58
sleet
In very cold temperatures, falling rain may freeze into small pieces of ice before reaching the ground. This type of ype of precipitation is called sleet. If the air in the clouds is cold enough, the water vapor can rapidly freeze and form snowflakes. Snowflakes fall to the ground as snow. During a thunderstorm, raindrops in storm clouds can freeze to form balls of ice. These balls of ice fall to the ground as hail.
enough, the eeze and form all to the groun
Activity 9.2AB How is rain different from sleet, snow and hail? Reg Reg orm, raindropraindr e to form balls of ifor alls ce fall to the groundll to the gro ega ain differe ow and hail
hailstones
59
A Closer Look The Water Cycle
Water on Earth is constantly being heated and cooled. As this happens, water moves in a cycle between the surface of the Earth and the atmosphere. This process is called the water cycle.
The heat from the Sun causes the water in the ocean, lakes and rivers to change into a gas called water vapor. This process of changing from a liquid to a gas is called evaporation.
The water vapor in the air cools as it rises and changes to liquid water in the form of tiny water droplets in clouds. This process of changing from a gas to a liquid is called condensation. t the s. This a
evaporation evaporation condensation condensonden
60
The water droplets combine with other water droplets and eventually fall back to the surface of the Earth as precipitation. The precipitation flows on and under the ground into rivers, lakes and the ocean.
AB Activity 9.3
precipitation
Try This! How long does it take for water to evaporate outside? Plan and conduct an investigation to find out. What factors affect the rate of evaporation? Go Online! Watch the water cycle in action in a video on the NGScience website. QuickCode: C4D6 tion oes it take vaporate out nduc igation to find t factors af of evaporation?catati Go Onli Watch cti NG
61
Weather satellites atellit orbit the Earth collecting Earth collecti and sending weather din we eat a her information back to Earth. formation back t
Weather Forecasting
Weather scientists, called meteorologists, are constantly gists, are co using technology to gather information about the tion about weather. Weather stations all over the Earth collect data he Earth c on temperature, the movement of wind, air pressure and t of wind, air precipitation. Buoys in the ocean collect data about currents, an collect water temperature and wave height. Radars collect data height. Ra about the movements of clouds and precipitation. In space, of c weather satellites are constantly orbiting the Earth, collecting nstant and sending information about the weather back to Earth. ion about th
62
Meteorologists use powerful computers to analyze and interpret weather information. By observing patterns in the weather, they are able to predict what the weather will be like in the future. These predictions are called weather forecasts. Weather forecasts are very helpful to people. They can help us to plan our day or week. They can also warn and help us to prepare for severe weather events, such as thunderstorms, hurricanes, floods and droughts.
the mov and ecipit
AB
Activity 9.4 What information do meteorologists communicate to people during a weather forecast?uc
Weather radars are able to monitor the movement of clouds and precipitation.
Meteorologists analyze and interpret patterns in the weather to predict what hat the weather will be like in the future.
l
63