Mesoscale Meteorology and Convection
This quiz will test your knowledge of mesoscale meteorology and convection.
Questions
What is the typical horizontal scale of mesoscale meteorological phenomena?
- 10-100 km
- 100-1000 km
- 1000-10000 km
- 10000-100000 km
What is the typical vertical scale of mesoscale meteorological phenomena?
- 1-10 km
- 10-100 km
- 100-1000 km
- 1000-10000 km
What is the most common type of mesoscale meteorological phenomenon?
- Thunderstorms
- Tornadoes
- Hurricanes
- Blizzards
What is the main cause of convection?
- Differences in temperature
- Differences in pressure
- Differences in humidity
- Differences in wind speed
What is the role of buoyancy in convection?
- It causes warm air to rise and cool air to sink.
- It causes cool air to rise and warm air to sink.
- It causes air to move horizontally.
- It causes air to move vertically.
What is the lapse rate?
- The rate at which temperature decreases with height
- The rate at which pressure decreases with height
- The rate at which humidity decreases with height
- The rate at which wind speed decreases with height
What is the dry adiabatic lapse rate?
- 9.8 °C/km
- 6.5 °C/km
- 3.5 °C/km
- 1.0 °C/km
What is the moist adiabatic lapse rate?
- 6.5 °C/km
- 3.5 °C/km
- 1.0 °C/km
- 0.5 °C/km
What is the difference between the dry and moist adiabatic lapse rates?
- The dry adiabatic lapse rate is greater than the moist adiabatic lapse rate.
- The moist adiabatic lapse rate is greater than the dry adiabatic lapse rate.
- The dry and moist adiabatic lapse rates are the same.
- The dry and moist adiabatic lapse rates are not related.
What is the role of the lapse rate in convection?
- It determines the stability of the atmosphere.
- It determines the direction of convection.
- It determines the speed of convection.
- It determines the intensity of convection.
What is a stable atmosphere?
- An atmosphere in which the lapse rate is greater than the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is less than the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is equal to the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is not related to the dry adiabatic lapse rate.
What is an unstable atmosphere?
- An atmosphere in which the lapse rate is less than the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is greater than the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is equal to the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is not related to the dry adiabatic lapse rate.
What is a conditionally unstable atmosphere?
- An atmosphere in which the lapse rate is less than the dry adiabatic lapse rate, but greater than the moist adiabatic lapse rate.
- An atmosphere in which the lapse rate is greater than the dry adiabatic lapse rate, but less than the moist adiabatic lapse rate.
- An atmosphere in which the lapse rate is equal to the dry adiabatic lapse rate.
- An atmosphere in which the lapse rate is not related to the dry adiabatic lapse rate.
What is the role of instability in convection?
- It promotes convection.
- It inhibits convection.
- It has no effect on convection.
- It is not related to convection.
What are some of the factors that can cause instability in the atmosphere?
- Heating from the sun
- Cooling from the ground
- Evaporation of water
- Condensation of water