Layers of the atmosphere
Grade 9 Science Worksheet

Circle the best answer.
Read this first
Typical top of the troposphere (rounded)
Place Height (km) Poles 8 Mid-latitudes 11 Equator 17 Bo reads the table. Which explanation fits the troposphere being deepest at the equator?
- The ozone layer at the equator pushes the troposphere upward
- Strong heating at the equator lets air rise higher before it cools to match its surroundings
- Gravity is weaker at the equator, so air spreads higher
- The equator has less water vapor, so the troposphere is taller
A weather balloon rises at 5 m/s. The troposphere ends at about 11 km. Which layer does Luz say it is in after 1 hour?
- The stratosphere, at 18 km
- The troposphere, at 11 km
- The troposphere, at 1.8 km
- The thermosphere, at 180 km
A balloon sounding (example data)
Height (km) Temperature (°C) 4 -10 8 -37 12 -57 16 -57 20 -55 Noah looks for the tropopause, where cooling with height stops. Where is it?
- About 20 km, the highest reading
- About 12 km, where the cooling stops
- About 4 km, where the weather seems to end
- About 8 km, halfway up the cooling
US Standard Atmosphere
Height (km) Temperature (°C) Pressure (hPa) 47 -2.5 1.11 51 -2.5 0.67 71 -58.5 0.04 Temperature falls from −2.5 °C at 51 km to −58.5 °C at 71 km. Which reason does Pia give?
- Ozone is most plentiful here, so the air absorbs less sunlight and cools
- Little ozone is left to absorb ultraviolet light, so the air loses heat and cools
- The ground heats this layer, and the heat fades with distance
- Pressure rises with height here, which cools the air
Argon is 0.93% of dry air. Sea-level pressure is 1,013.25 hPa. Partial pressure of a gas = share × pressure. Ren finds the pressure of argon alone at sea level. What is it?
- About 790 hPa
- About 94 hPa
- About 0.94 hPa
- About 9.4 hPa
Carbon dioxide rose from about 280 ppm before industry to about 420 ppm now. By what percent has it risen, by Tala's math?
- About 50%
- About 140%
- About 0.014%
- About 33%
Oxygen is 21% of the air at the ground and at 11 km, yet a breath holds less oxygen at 11 km. Which reason does Zee give?
- The oxygen share falls to 7% at 11 km, so each breath holds less
- Oxygen sinks, leaving nitrogen on top, so there is less at 11 km
- Planes use up the oxygen at 11 km, so each breath holds less
- The air is thinner, so each breath holds fewer molecules though the share is still 21%
US Standard Atmosphere
Height (km) Temperature (°C) Pressure (hPa) 0 15.0 1,013.25 11 -56.5 226.32 Pressure is the weight of the air above you. What share of the air lies above 11 km, by Esme's math?
- About 2%, because 226 hPa is two tenths of 1,013
- About 22%, because 226 of the 1,013 hPa is air above 11 km
- About 78%, because 78% of the pressure is still above you
- About 50%, because pressure halves at 11 km
A model says pressure halves every 5.5 km. Ari tests it at 11 km against the table. What does it predict, and how does that compare?
- About 126 hPa, which is 44% too low
- About 253 hPa, which is 12% too low
- About 507 hPa, which is 124% too high
- About 253 hPa, which is 12% too high
Pressure 22,632 Pa, temperature 216.65 K. Density = pressure ÷ (287 × temperature in kelvins), in kg/m³. Kira finds the density of the air at 11 km. What is it?
- About 3.64 kg/m³
- About 0.0364 kg/m³
- About 0.289 kg/m³, using 273 K
- About 0.364 kg/m³

