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Grade 10
TM
by
thandi mngomezulu
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Updated May 31, 2021
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Chapters
00:00
Chapter 1
00:19
Chapter 2
01:03
Chapter 3
01:16
Chapter 4
05:00
Chapter 5
05:38
Chapter 6
05:43
Chapter 7
05:45
Chapter 8
05:50
Chapter 9
Audio Transcript
Auto-generated
00:00 - 00:01
Hey, Great.
00:02 - 00:04
And to be, we're gonna be looking into the heating
00:04 - 00:04
of the atmosphere.
00:05 - 00:08
Request for me to discuss and know what is atmosphere?
00:09 - 00:12
Atmosphere is a layer of set of layers of gas
00:12 - 00:15
surrounding the planet or other material body that is held
00:16 - 00:18
in place by the gravity of the body.
00:19 - 00:23
Yeah. Now we're gonna be looking into the layers of
00:23 - 00:24
the atmosphere.
00:24 - 00:29
We have five layers of the atmosphere mainly exhaust fear.
00:30 - 00:37
Yeah. The most fear Mesosphere stratosphere to oppose fear in
00:37 - 00:41
the atmosphere is where we find our state light, our
00:41 - 00:44
space, our spaceships in the atmosphere.
00:45 - 00:48
We found our aurora in the mesosphere, we found our
00:48 - 00:54
metal years, metal, geological rocket and in the stratosphere we
00:55 - 00:57
find our radio salt in the troposphere.
00:57 - 00:58
We find our hottie.
00:59 - 01:08
But moving right along, now look into this picture of
01:08 - 01:09
the layers of the atmosphere.
01:09 - 01:15
You're gonna see uh spaceship, the hot air balloon and
01:15 - 01:16
so forth.
01:19 - 01:21
Now we're gonna be getting into details with the process
01:22 - 01:23
of heating of the atmosphere.
01:24 - 01:27
We have the insulation, we have the reflection, We have
01:27 - 01:30
the absorption, we have the scattering, we have the radiation,
01:31 - 01:31
we have the conduction.
01:32 - 01:33
We have the conviction.
01:34 - 01:35
Let's look into the isolation isolation.
01:36 - 01:38
Meet incoming solar radiation.
01:38 - 01:43
The sun energy is received by the act reflection, reflection
01:44 - 01:48
insulation is redirected back to the atmosphere.
01:49 - 01:54
And then absorption insulation is retained by a substance and
01:54 - 02:00
converted into heat energy, scattering a small particles and gas
02:00 - 02:06
particles diffuse the insulation, radiation emission of energy.
02:07 - 02:10
An object and then conduction is the transfer of heat
02:11 - 02:13
from one object to the other.
02:14 - 02:17
And conviction is the transfer of heat energy by the
02:17 - 02:18
vertical movement.
02:23 - 02:27
Yeah. Mhm.
02:28 - 02:29
Yeah. Mhm.
02:31 - 02:32
Mhm. Mhm.
02:36 - 02:37
Mhm. Mhm.
02:42 - 02:42
Yeah. What?
02:43 - 02:45
Okay. Uh huh.
02:49 - 02:52
Yeah. Let's go more.
02:59 - 03:03
Mhm. Yeah.
03:10 - 03:11
Okay. Nothing like that.
03:15 - 03:18
Yeah. Mhm.
03:22 - 03:23
Where are my brothers?
03:26 - 03:27
Mhm. Yeah.
03:28 - 03:29
Right. Has been.
03:30 - 03:33
Yeah. Thank you.
03:40 - 03:43
Yeah. Mhm.
03:46 - 03:49
Yeah. Right.
03:49 - 03:50
Right. Yeah.
03:53 - 03:53
All right.
03:54 - 03:54
Uh huh.
03:58 - 04:01
Mhm. Yeah.
04:05 - 04:05
Uh huh.
04:09 - 04:15
People people sure romance.
04:23 - 04:23
Thank you.
04:25 - 04:26
Yeah you go.
04:27 - 04:34
Yes. Okay.
04:37 - 04:41
Well. Yeah.
04:43 - 04:48
Yeah. Okay.
04:49 - 04:50
Mhm. Yeah.
04:51 - 04:55
Okay. So you bought it.
04:55 - 04:56
I had technical issues.
04:57 - 04:58
Please allow me to continue.
04:59 - 05:00
Thank you.
05:03 - 05:05
Now we're gonna be looking into the factors that affect
05:05 - 05:10
temperature. We have the latitude altitude, distance distance from the
05:11 - 05:18
sea. Ocean current, latitude the temperatures are high at all
05:18 - 05:23
places near the equator and then altitude height above sea
05:24 - 05:27
level. The difference from the sea is the different in
05:28 - 05:29
heat of the land and water.
05:30 - 05:33
And it affected the temperature of the place located near
05:34 - 05:34
the coast.
05:35 - 05:37
Mhm. We have warm and ocean current.
05:39 - 05:41
Yeah. Yeah.
05:44 - 05:53
Right. Thank you so much.
05:55 - 05:55
Goodbye.
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