Amplify Weather Patterns

What could have happened to the air parcel to cause rainfall on Day 2?

• The air parcel was warmer than the surrounding air, so it lost energy.

• The air parcel was warmer than the surrounding air, so it gained energy.

• The air parcel was at the same low temperature as the surrounding air, so it had low energy.

• The air parcel was cooler than the surrounding air, so it gained energy.

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

Air Parcel 1 is the same temperature as the surrounding air. Air parcel 2 is warmer than the surrounding air. Air Parcel 1 and Air Parcel 2 started with the same amount of water vapor in them. Which air parcel will have more rainfall and why?

• Both air parcels will have the same amount of rain. They have the same surrounding air temperature, so the same amount of water vapor will fall as rain.

• Air Parcel 1 is colder than Air Parcel 2, so more water vapor will fall as rain.

• Air Parcel 2 will gain energy from the surrounding air, which will cause more water vapor to fall as rain.

• Air Parcel 2 will lose energy to the surrounding air, which will cause more water vapor to fall as rain.

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

What could explain why Storm 1 had more rainfall than Storm 2? Before Storm 1, the air parcel at the surface could have been:

• warmer, so when the air parcel moved higher, it lost more energy.

• warmer, so when cooler air from above moved down, it lost more energy.

• cooler, so when the air parcel moved higher, it gained more energy.

• cooler, so the air parcel had low energy and remained near the surface.

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

If an air parcel is warmer than its surrounding air, then it will rise.

• True

• False

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

The temperature of the areas surrounding Kochi before each storm was about 10°C and there was the same amount of water vapor in the air. Given this information, which storm do you predict will have the most rainfall, and why?

Evaluate responses using AI:

OFF

Tags

NGSS.MS-ESS2-5

The surrounding air in the troposphere gets colder the higher you go up.

• True

• False

Conditions such as wind, temperature, cloud at a particular time and place

• transfer

• air parcel

• change

• weather

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

An air parcel will rise ....

• When the temperature is the same as the surrounding air

• When it is colder than the surrounding air

• When it is warmer than the surrounding air

Tags

NGSS.MS-ESS2-5

When does energy stop transferring out of an air parcel?

• When the air parcel temperature is warmer than the surrounding air.

• When the air parcel temperature is even colder than the surrounding air.

• When the air parcel temperature is the same as the surrounding air.

Tags

NGSS.MS-PS1-4

NGSS.MS-PS3-4

NGSS.MS-PS3-5

More surface water (larger body of water) =

• less water vapor and smaller storm

• less water vapor and larger storm

• more water vapor and smaller storm

• more water vapor and larger storm

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6