Energy Transfer & Convection
types air masses
air masses mechanical aspects
ocean currents
bonus stuff
100

True or False: Cold air rises.

False

100

An air mass forms over northern Canada during winter. The land is frozen and dry.

cP (continental polar)

100

An air mass has the same

__________________ and moisture

content throughout.

temperature 

100

The two types of ocean currents are

surface and deep

100

what are the degrees on earth

0, 30, 60, 90

200

Which unequal heating condition causes a sea breeze to develop during the day?

Warmer air over land than water

200

An air mass forms over the warm waters of the Gulf of Mexico and moves toward the southeastern United States bringing humid conditions.

mT (maritime tropical)

200

what is the jet stream?

fast-moving band of air high in the atmosphere that helps move storms and weather across the planet.

200

Earth’s _____ causes ocean currents in

the Northern Hemisphere to curve

clockwise.

spinning on its axis

200

what are all the convection current cells 

hadley ferrell polar

300

Warm air near Earth’s surface rises, cools, and then sinks. This continuous movement of air forms a

Convection current

300

An air mass forms over the hot deserts of northern Mexico and the southwestern United States.

Desert Southwest → cT (continental tropical)

300

where is the warm air and cold air adjacent to the jet stream?

  • Warm air is on the south side of the jet stream (closer to the equator).

  • Cold air is on the north side of the jet stream (closer to the poles).

300

When a current comes into contact

with a continent or landmass it

changes direction.

300

how is sun thermal energy dispersed on earth

equator is warmest then over 30 degrees warm and the poles are cold

400

what is the process of gasses such as water vapor hold energy from the atmosphere to keep earth warm?

the greenhouse effect

400

An air mass forms over the cold waters of the North Pacific Ocean near Alaska.

North Pacific near Alaska → mP (maritime polar)

400

what are global wind patterns name the 3 patterns what are local wind patterns name the 2 patterns?

Global wind patterns are large wind systems that move air around the entire planet. These winds blow in predictable directions over long distances.

Examples of global winds:

  • Trade Winds

  • Westerlies

  • Polar Easterlies

    Local wind patterns are smaller winds that occur over short distances and are caused by temperature differences in a specific area.

    Examples of local winds:

    • Sea breeze (daytime wind from water → land)

    • Land breeze (night wind from land → water)

400

The horizontal movement of ocean

water that is caused by wind and

the Coriolis Effect.

surface currents

400

what is a front?

 A front is the boundary where two different air masses meet.

500

Explain how unequal heating of Earth creates global wind patterns. Where is the warmest part of earth and coldest parts?

Earth is heated unevenly because the Sun’s energy hits different parts of the planet at different angles. The equator receives the most direct sunlight, so it is the warmest region. Warm air near the equator heats up, becomes less dense, and rises. As this air rises and moves away from the equator, it cools and eventually sinks at higher latitudes.

500

An air mass forms over the Arctic region near the North Pole, where the ground is covered in ice and snow year-round. Temperatures are extremely cold and the air contains very little moisture.

cA – Continental Arctic

500

what is the Coriolis effect what is the movements of wind in the northern and southern hemisphere due to this effect?

bending of moving air and water caused by Earth rotating on its axis.

  • In the Northern Hemisphere, wind curves to the right.

  • In the Southern Hemisphere, wind curves to the left.

500

The _____ is a system of constantly

moving ocean circulation driven by

temperature and salinity.

Global Conveyor Belt

500

 Where are Hadley, Ferrell, and Polar cells located by degrees? where are the global winds located within these cells


Hadley Cell trade winds

0° – 30°

Ferrel Cell prevailing westerlies 

30° – 60° 

Polar Cell polar easterlies 

60° – 90°