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Air Pressure

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Subido el 28 de mayo de 2007 por EducaMadrid

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NASA Why? Files segment explaining how air pressure affects weather.

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Wow we learned a lot from Dr. Chambers. I wrote this for my trip. Don't forget to 00:00:00
add water vapor and condensation. I know that's a clue because it's how rain is 00:00:05
made. Hi where's Dr. D? Is he here today? We haven't seen him yet. Hi guys I'm here. 00:00:10
You have that look like you're working on something. We're concerned about 00:00:16
missing our physics fair because of the storm. We don't want to miss riding those 00:00:19
roller coasters. Can you give us some clues on how to understand the weather? 00:00:23
Sure. Something you definitely need to understand is energy. There's an electric 00:00:27
motor that provides the energy to raise a roller coaster car to the top of the 00:00:32
first hill and then gravity takes over. What energy source makes the weather 00:00:35
happen? Do you mean what makes the winds blow? Or what raises the rain into the 00:00:39
clouds just like the roller coaster was lifted? Exactly. I don't know. I think you 00:00:44
do. It's the same energy source that makes the plants grow. Oh the Sun I knew 00:00:50
that. When the Sun heats the earth, some areas become hotter than others. This is 00:00:55
uneven heating that produces the winds. Wind? It can make wind? Air always moves 00:00:59
from a region of higher pressure to a region of lower pressure. Wait Dr. D we 00:01:04
haven't learned about pressure yet. What's that? I guess I better slow down a little 00:01:09
bit. Air is made up of molecules like oxygen and nitrogen. They're constantly in motion 00:01:12
traveling in straight lines until they bounce off of something. So you mean right 00:01:18
now we're being bombarded with molecules? That's right. 00:01:21
Molecules bounce off of something and they apply a force to that object. This force 00:01:27
creates what we call air pressure. Let me show you an example. These hemispheres have 00:01:31
molecules bouncing off the outside. I've taken most of the air out of the middle 00:01:35
so there are very few molecules on the inside pushing out. Here try to pull it 00:01:39
apart. Wow this is really hard. That force you talked about is very real. Now if I 00:01:43
let the air back into the middle we'll have molecules both pushing out and 00:01:51
pushing in. The pressure on the outside is the same as the pressure on the inside. It 00:01:54
shouldn't be a problem. It's much easier now. Let's try something else. Put on your 00:01:59
goggles and safety glasses. 00:02:05
I'm gonna heat the air inside this can. There's a little bit of water in it. 00:02:10
I'm gonna turn the can upside down into the pan of water and the pressure in the 00:02:15
can is gonna drop very very quickly and the higher pressure air on the outside is 00:02:20
gonna crush the can. 00:02:24
Watch this. That's amazing. Now when I blow up this balloon I'll be increasing the 00:02:28
density of the air inside. That means the molecules will be more tightly packed. 00:02:37
This makes the pressure on the inside greater than the pressure on the outside. 00:02:41
I knew that was going to happen. So that's what you meant when you said the 00:02:51
air went from a region of higher pressure like the balloon to a region of 00:02:57
lower pressure like this room. Very good. Now suppose you're at the beach in the 00:03:00
summer. The sand is hot and it warms the air above it. Now warmer air has a lower 00:03:04
pressure than cooler air because it's less dense. Now the air above the ocean 00:03:08
is cooler therefore it has a higher pressure than air above the sand. What 00:03:13
happens? Well I would think just like the balloon that the wind will blow from the 00:03:17
higher pressure air across the ocean toward the lower pressure air on the 00:03:20
beach. Very good. That's what's called a sea breeze. 00:03:24
There's an update from the Weather Channel. The problem that we reported earlier has slightly strengthened and 00:03:28
become more organized with maximum sustained wind now at 30 miles per hour. 00:03:33
This system has been upgraded to a tropical depression. It is currently 00:03:37
located at 15 degrees north and 40 degrees west and it is moving northwest 00:03:42
at 20 miles per hour. Here's a globe. Look here are the Antilles Islands. I think we 00:03:48
should start tracking the storm. Don't you? Oh I don't think so. It's far away. We 00:03:55
don't need to worry about it. Yes we do. The storm has turned into a tropical 00:04:00
depression. I don't want to miss the physics fair or our trip to Florida. 00:04:04
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Idioma/s:
en
Niveles educativos:
▼ Mostrar / ocultar niveles
      • Nivel Intermedio
Autor/es:
NASA LaRC Office of Education
Subido por:
EducaMadrid
Licencia:
Reconocimiento - No comercial - Sin obra derivada
Visualizaciones:
284
Fecha:
28 de mayo de 2007 - 15:33
Visibilidad:
Público
Enlace Relacionado:
NASAs center for distance learning
Duración:
04′ 08″
Relación de aspecto:
4:3 Hasta 2009 fue el estándar utilizado en la televisión PAL; muchas pantallas de ordenador y televisores usan este estándar, erróneamente llamado cuadrado, cuando en la realidad es rectangular o wide.
Resolución:
480x360 píxeles
Tamaño:
24.85 MBytes

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