When Worlds Collide: The Air Masses Fronts Quiz

If an air mass forms over water, it is maritime (moist), and if it forms near the equator, it is tropical (warm); therefore, the combination is Maritime Tropical.

If cold air is denser and moves faster than warm air, it will push under the warm air like a wedge; this specific boundary is defined as a cold front.

If neither air mass is strong enough to displace the other, the boundary remains "still" or stationary; therefore, the statement is true.

If red is the standard color for warmth and semicircles represent the direction of air flow for warm masses, then red semicircles are the correct map symbol.

If a volume of air spans thousands of kilometers and maintains consistent physical properties like moisture and heat, it is scientifically classified as an air mass.

If a cold front forces warm, moist air to rise rapidly, then the water vapor condenses quickly into tall clouds; this process results in heavy, sudden storms.

If "Continental" means forming over land (dry) and "Polar" means forming at high latitudes (cold), then a landmass like Northern Canada is the logical source.

If high pressure involves sinking air that prevents clouds from forming, then it leads to clear, fair weather; therefore, associating it with "bad" weather is false.

If a warm air mass is trapped and lifted entirely off the ground by two converging cooler masses, the complex boundary created is an occluded front.

If air masses with different densities and temperatures do not mix easily, they create a transition zone; this border is known in meteorology as a front.

If meteorologists classify air masses based on their source regions, they look for consistency in heat (temperature) and moisture (humidity) content.

If molecules in warm air are spread further apart, then the air is less dense; if it is less dense than the surrounding cold air, it must rise.

If a warm front represents the arrival of a warm, moist air mass, then the local conditions will transition to higher temperatures and higher moisture.

If the word "continental" refers to large landmasses, then air masses originating over these regions are dry and carry the "continental" label.

If the symbols for cold and warm fronts are pointed in opposite directions on the same line, it shows the masses are pushing against each other without moving.

If "maritime" air masses form over water, they evaporate and hold a large amount of moisture; therefore, calling them "dry" is factually incorrect.

If tropical regions are located near the equator where solar radiation is highest, then air masses from those regions will be characterized by high heat.

If a front is a clash of two different air masses, then the transition must cause shifts in heat, wind flow, and moisture condensation (rain/snow).

If the symbols for cold and warm fronts are combined into a single purple line, it indicates the cold front has overtaken the warm front, forming an occlusion.

If air in a low pressure system rises and cools, causing water vapor to condense into clouds, then the result is likely to be precipitation or rain.