With a simple balance you can find the weight (weight = mass in this case) of air.
I propose the following method.
Take the weight of the container (suppose it is a 1 litre container). And the weight is x kg. Take weight of the container full of water, say it is y kg. Weight of 1 litre of water is 1 kg. So the weight of the container is 'y -1' kg.
So the weight of the air in it is 'x - y +1' kg. It should be around 1.2 gm.
No. An anemometer measure wind speed. A front is a boundary between air masses.
There are two types of air masses: COLD AIR AND WARM AIR.Cold Air Masses-Cold air masses can cause thunderstorms and even tornadoes.Warm Air Masses-Warm air masses can bring many hours of steady rain and snow.
It separates hot air masses and cold air masses
There are two types of air masses: COLD AIR AND WARM AIR.Cold Air Masses-Cold air masses can cause thunderstorms and even tornadoes.Warm Air Masses-Warm air masses can bring many hours of steady rain and snow.
Air masses get their characteristics from where they are made
There are two types of air masses: COLD AIR AND WARM AIR.Cold Air Masses-Cold air masses can cause thunderstorms and even tornadoes.Warm Air Masses-Warm air masses can bring many hours of steady rain and snow.
The five types of air masses are polar, tropical, maritime, continental, and arctic. Polar air masses are cold and dry, tropical air masses are warm and dry, maritime air masses are warm and moist, continental air masses are dry and cold, and arctic air masses are extremely cold and dry.
Two types of air masses are cold and warm air masses. When they meet each other, a front forms.
Yes, warm air masses are lighter than cold air masses because warm air is less dense. As a result, warm air tends to rise while cold air sinks. This buoyancy difference plays a significant role in the movement of air masses in the atmosphere.
No, as cold air is denser.
The 4 major air masses are continental polar (cP), continental tropical (cT), marine polar (mP) and marine tropical (mT). Generally, continental air masses are drier than marine air masses, and polar air masses are cooler than tropical air masses. cT air masses are relatively limited in distribution existing in the south west North America and North Africa.
continental air masses