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Quarter 3: Science 8 Week 4 | Conditions for Storms | MATATAG Curriculum

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0:01

Okay. So, welcome grade 8 students.

0:03

Okay, so this week is for week number

0:07

four ano and I hope you enjoyed our

0:09

lessons from week number two and 3.

0:12

Okay, types of eruption and types of

0:14

volcano. So, mga mam pinagawa ko kasi

0:16

sila dito ng mga bulkan e and then

0:18

pina-erupt namin ah in the class and

0:22

then they really enjoy it. Okay. So

0:24

hopefully naman. Okay. And then next

0:26

year may mga ganun pa din tayo. Okay? Sa

0:29

grade 8 pa din. Hopefully sa grade 8 pa

0:31

din ako next year ano. And for today's

0:33

lesson, we're going to talk about

0:34

storms. Okay? Yes. Okay. You've heard it

0:37

right. Let's dig deeper and understand

0:40

them even better. Okay. So since our

0:43

country is prone to typhoon or uh

0:46

storms, okay, mas maganda na mas

0:49

maintindihan ninyo yung mga anak kung

0:51

papaano ba sila nabubuo or ano yung mga

0:54

conditions for it to be. Okay? So I am

0:58

Sir Wawi, Rever Curious Science Buddy.

1:00

Don't forget to like, share, and

1:02

subscribe para lagi kayong updated sa

1:04

mga susunod pang videos. All right,

1:07

let's begin. So our topic for week

1:09

number four it's like um what do you

1:12

call this preparatory topic kasi medyo 3

1:16

weeks natin okay na idi-discuss yung

1:19

about typhoons like

1:21

formation of typhoons, parts of typhoon

1:23

and then the typon prepare preparedness.

1:26

Okay? So madali lang naman siya. Ayan.

1:30

So for our topic it's about condition

1:32

for storms. Ayan for the learning

1:34

competency, gather information from

1:37

secondary sources to explain how

1:39

typhoons develop and why the Philippines

1:42

is prone to typons. And for our learning

1:45

objectives, locate the Philippine area

1:47

of responsibility in the map. Explain

1:50

why the intertropical convergence zone

1:53

or the ITCZ is a factor for storm

1:57

formation. And then three, determine the

2:00

conditions needed to form a typhoon. Ano

2:02

ba yung mga conditions or factors for a

2:04

typhoon to be formed? And then number

2:07

four, differentiate the types of

2:09

tropical cyclones. Okay? And then number

2:12

five, identify the parts of a typhoon.

2:14

Actually, iyung parts of a typon is um

2:17

hindi natin dito madi-discuss to be

2:19

specific, it is part of week number

2:22

five. Okay. And then number six,

2:24

describe the situation in each storm

2:26

signal wording. Similar din ito. Okay?

2:29

Hindi rin natin siya mata-touch. Okay?

2:31

Part siya ng week number ah five, okay?

2:35

Or six. I'm not sure about that. But

2:37

hindi natin siya possible or hindi natin

2:39

siya madi-discuss dito. So ang atin

2:41

lang, sinunod ko lang po kasi yung nasa

2:43

le kung ano yung objectives doon. So

2:46

possible yung ating ma explain yung sa

2:49

Philippine era responsibility, the

2:51

intertropical conference zone. Okay? And

2:54

then yung ating types of tropical

2:56

cyclones together with the conditions.

2:58

Yun yung highlight ngayon sa ating

3:00

discussion. Conditions needed to form a

3:03

typon. Okay? So pwede nating i-erase

3:05

yung 5 and six if you want. Okay? So for

3:08

our review, okay, part of our review,

3:10

layers of the atmosphere. And I know

3:12

that you are already familiar with the

3:14

different layers of atmosphere, right?

3:16

Grate. Okay. So sige. Okay. So for its

3:20

description we have okay altitude is

3:23

zero from the earth surface to 12 km. It

3:26

varies up to 8 km at pols okay 18 km at

3:30

equator. Okay. So for notes, it's the

3:33

closest layer to earth surface. It

3:36

contains 75 to 80% of atmosphere's mass

3:40

and all weather events. Okay. And then

3:42

clouds like rain, storms will cure here.

3:46

And then the temperature decreases with

3:48

altitude about 6.5°

3:51

celsus per km. Okay. So what layer is

3:55

being described in this um slide?

3:59

What do you think? It's correct.

4:04

Okay, it's the troposphere. Okay, so

4:06

ayan po. And then nandiyan din po

4:08

lumilipad sa troposphere yung mga

4:10

parachute. Okay. Dumadaan yung mga

4:12

airplane, something like that. Okay. And

4:14

then the clouds, the rain. Okay. So

4:18

next, what about this one? So for its

4:21

altitude is ranging from 12 to 50 km.

4:25

Okay. Altitude mga papataas. kung gaano

4:28

sila kataas. Okay. It contains the ozon

4:30

layer which absorbs harmful UV

4:33

radiation. So ozon layer in chemistry O3

4:36

ano which absorbs harmful UV radiation.

4:40

And then sabi dito airplanes fly in the

4:42

lower stratosphere okay or sort of

4:45

troposphere ano to avoid turbulence.

4:48

Okay. So next temperature increases with

4:51

altitude due to ozone absorption of

5:00

ayan. So what layer is this? Okay. What

5:02

layer is being described in this slide?

5:05

What do you think? Correct. It's

5:08

ayan

5:10

the stratosphere.

5:12

Okay. So the stratosphere tandaan natin

5:14

sa stratosphere nandiyan 'yung ozen

5:16

layer. Okay. Next layer. Okay. Altitude.

5:20

Okay. From 50 to 85 km. It's the coldest

5:23

layer of the atmosphere up to 90° celus.

5:27

It protects Earth by burning up atmers.

5:30

Okay. And then temperature decreases

5:31

with altitude.

5:33

Okay. So ayan the massosphere. Tandaan

5:36

natin. It's the coldest layer because it

5:40

burns up meteors. Okay. Next.

5:46

Okay. Altitude from 85 to 60 km. It's

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very hot up to 2000° Celus or more

5:54

because it absorbs high energy, solar

5:57

radiation and of course Aurora or the

6:01

northern and southern lights occur here.

6:04

Okay? Kasi nga bakit po nagkakaroon ng

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northern and southern lights? Because in

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this part mayong mga charged particles.

6:10

When they interact, okay, or nagkakaroon

6:13

sila ng interaction, nakaka-create sila

6:15

ng mga lights. Okay? And then satellites

6:18

and the international space station

6:19

orbit in this radian region. Okay. What

6:23

layer is this? It's the thermosphere,

6:25

ano? Okay. And next, altitude from 600

6:29

km to 10,000 km gradually merges into

6:33

outer space. Kumbaga ito na yung

6:34

pinaka-last. The outermost layer of the

6:36

atmosphere, air is extremely thine and

6:40

atoms and molecules can scape into space

6:43

mainly composed of hydrogen and helium.

6:46

Okay. What layer is this? Correct. It's

6:48

the excess, the outermost. layer kumbaga

6:52

ito na yung pinaka um what do you call

6:55

this merge uh it merges into outer space

6:59

na papunta na sa outer space and so

7:02

hopefully na-refresh tayo d sa layers of

7:04

atmosphere okay ayan so bakit ko ba yan

7:08

diniscuss or inintroduce dito may

7:09

kinalaman po ba yan sir of cours and so

7:12

where do storms form in the atmosphere

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also in the layers of the atmosphere

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saan po nabo yung ating storm

7:21

Okay, nandiyan na po yung sagot. Hindi

7:23

ko na itos

7:26

fear. Dapat po arelete ko ano. Okay. So,

7:29

sorry that's in the trophosphere. Sorry

7:33

for that. Okay. It's in the

7:34

trophosphere. Tandaan natin, storms form

7:37

in the trophosphere which is the lowest

7:39

layer of the atmosphere. Okay. Kumbaga

7:41

nandi yan yung mga water disturbances.

7:44

Okay, since okay, nandiyan yung mga

7:46

formation ng clouds. Okay, so tandaan

7:48

natin ang storms po ay nabubuo sa

7:51

troposphere. Okay, next.

7:54

So, before we begin, meron po akong

7:56

video ah video or before kayo

7:58

mag-continue. Meron po akong four videos

8:00

na nandon sa ating description.

8:03

Hopefully mapanood niyo muna before tayo

8:05

before ninyo i-continue na manood ng

8:08

video kasi it's important for you to

8:10

understand what I'm talking ah what I'm

8:13

talking here ano. So hopefully panoorin

8:15

niyo muna bago tayo mag dito sa ating

8:18

lecture or magpatuloy. So nasa link po

8:21

okay or nasa description ng ating video

8:24

yung link ng bawat video kasi pa ako

8:26

pwedeng mag-play dito baka tayo

8:28

ma-report. Okay. So, what is the role of

8:31

air pressure and temperature in the

8:32

typon formations? Okay. So, meron po

8:35

bang role or may factor ba? Okay. Yung

8:39

ating pressure and temperature in the

8:41

formation of typhoon.

8:44

Okay. So, of course, ayan. So the answer

8:47

is yes. Okay. So meron pong kinalaman or

8:50

merong role na ginagampanan yung

8:52

pressure and temperature in typhoon

8:54

formation because warm air rises. Okay?

8:58

Warm air rises. Okay? Low pressure

9:02

forms. Okay? So sa low pressure area,

9:06

okay? Umaangat, okay? Or tumataas yung

9:09

ating air or warm air. Okay. And then

9:13

pag nag uh tumaas yan, it will cause

9:18

strong winds and rain. Kasi nga habang

9:21

tumataas yung ating warm air, okay, the

9:24

air or the regions in that part becomes

9:27

cooler, okay? And then it the molecules

9:30

in that part expands. Okay? So yun yung

9:33

pinaka-reason. Okay. Kung bakit sa ating

9:36

low pressure area, okay, nabubuo yung

9:39

ating mga storms. Okay? So ipapaliwanag

9:41

ko pa rin naman yan later kung ano ba

9:43

yung kinalaman ng pressure, okay sa

9:45

formation ng typhoon. Okay. And then how

9:48

does the latitude of a place relate to

9:51

its temperature? Okay. Air pressure. How

9:55

does the latitude of a place rate to its

9:57

temperature or air pressure? The answer

9:59

is near the equator. Sa atin sa equator,

10:02

it's too hot and low pressure. Okay.

10:05

Nearp, cold and high pressure. So in

10:08

this part, okay, in this part ha or

10:12

papipiliin ko kayo low pressure and high

10:14

pressure, saan diyan possible mabuo yung

10:17

ating typhoon or storms? In low pressure

10:20

or in high pressure? Correct. Okay. In

10:23

low pressure area. Okay. So kadalasan

10:26

din yan or madalas talaga nandiyan po

10:28

nabubuo yung ating mga typon sa low

10:32

pressure area. Okay? Ang high pressure

10:34

kasi mga anak it can cause clear sky.

10:38

Okay? Yung mga ganyan sa high pressure

10:40

natin. Sa low pressure ito yung may mga

10:43

cloudy. Okay yung paligid. Okay kasi nga

10:46

tumataas yung warm air expands. Okay the

10:50

region and that part becomes cooler.

10:52

Okay so next. So for our activity number

10:56

one decoding storm conditions. So at the

10:58

end of the activity students will be

11:00

able to identify and understand key

11:02

terms related to the conditions

11:04

necessary for a storm formation by

11:07

decoding hidden words using number

11:09

letter substitution. So nagawa na naman

11:12

natin ito. Okay? So parang magde-decode

11:14

lang tayo. Ano? So this one, A is for

11:16

number one, B is for number two, and so

11:18

on and so forth. Okay? So kumbaga

11:21

ide-decode niyo lang for you to come up

11:23

in the correct word. Okay? So are you

11:25

ready? So let's start. What about this?

11:29

Okay. So raise your hand or you just

11:31

have to try this. Pause the video para

11:33

makapagsagot.

11:35

Correct. It's adiabatic temperature

11:38

change. Okay. Next.

11:42

Correct. It's air pressure.

11:45

Next,

11:47

it's altitude. Okay. Next,

11:52

humidity. What about this one?

11:56

Correct. It's intertropical convergence

11:58

zone.

12:00

What about this one?

12:02

Low pressure area.

12:06

Correct. Okay. It's pag-asa.

12:10

What about this one? Storms. Okay. And

12:13

then okay, we are done in that. So

12:16

syempre we those words are related to

12:19

our discussion and of course okay

12:21

di-discuss natin yun one by one ano. So

12:23

for our activity number two, sharing

12:25

insight and storm vocabulary. Let's uh

12:28

explain those vocabulary words. Okay. So

12:32

at the end of the activity students will

12:34

be able to explain the meaning of key

12:36

decoded vocabulary words and discuss

12:38

their importance in the conditions for

12:40

storm formation. So magsisimula muna

12:42

tayo sa adiabatic temperature change.

12:46

Ano ba yung tinatawag nating adiabatic

12:48

temperature change? Okay. So it means

12:51

that it is a cooling or heating of air.

12:53

Cooling or heating of the air caused by

12:57

the contraction or expansion or

12:59

expansion of air molecules as opposed

13:02

the loss of gain or heat. Okay? Sabi

13:05

diyan, "When air rises, it goes to a

13:08

place where the pressure is lower. It

13:11

expands and becomes cooler. Just what

13:14

just what I'm talking earlier. Okay. So

13:17

in a low pressure area, okay, or low

13:20

pressure, yung air is nagra-rise, okay?

13:23

Tumataas, okay? And then when it uh

13:26

rises, okay, the molecules expands and

13:30

the region becomes cooler. Okay. Kaya

13:33

nabubuo or ito yung pinaka parang good

13:35

conditions for a storm to B4. Kaya ano

13:39

naman 'yung opposing site niya? Okay.

13:41

When air sinks, it goes to a place where

13:43

the pressure is higher. It gets

13:45

compressed and becomes warmer. Okay? Ito

13:48

naman sa when air sinks. Okay. Sa higher

13:51

pressure area naman ito. Pag nag-sink sa

13:53

higher pressure area, iyung ating air is

13:55

nagsi-sink. Okay? Yung ating mga

13:57

molecules nako-compress and the regions

14:00

become warmer.

14:01

Okay, tatandaan natin. But in overall um

14:06

an overall what do you call this? Uh

14:08

event or occurrence, okay, yung ating

14:11

cooling and heating of air is known as

14:14

adiabatic temperature change. Okay?

14:18

Which occures when air rises and when

14:21

air sinks. Okay? So sige. So meron pa ba

14:25

tayong idadagdag dito?

14:29

Okay. So wala na naman. So next we have

14:32

air pressure. Ano naman yyung air

14:34

pressure natin? Okay when we say air

14:36

pressure the amount of force exerted on

14:38

a unit surface area. Okay? High

14:41

pressure, low altitude. Okay? Air is

14:44

squeeze. Okay? Nai-squeeze.

14:47

Okay? Nako-compress yung ating mga

14:49

molecules. Okay? Molecules become close

14:53

and yung effect, yung region nagiging

14:56

warmer. Okay. In um low pressure area,

15:01

yung ating low pressure area, kadalasan

15:03

yan ay nandon sa high altitude. Air

15:06

expands, then the molecule spreads out

15:09

and then the region become or becomes

15:12

cooler lumalig. Okay? So that's the main

15:16

difference. Okay. Meron tayong high

15:18

pressure at meron tayong low pressure

15:21

area. But in the two, okay? Saan po yung

15:25

good condition for a storm to be formed?

15:28

In a low pressure area? Tatandaan natin.

15:31

So sabi diyan, air pressure is simply

15:33

the force of air. Okay? Pushing on a

15:36

surface.

15:38

Okay. Tatandaan natin that in a low

15:39

pressure area lagi ang nasa high

15:41

altitude. Ano? Okay. Altitude. Okay.

15:46

Causing the air to rise. Okay. And then

15:49

yung molecules mag-spread out. Okay. The

15:52

regions become cooler. In high pressure,

15:54

low altitude lagi. Okay. Yung ating

15:57

molecules, yung air natin na-squeeze

15:59

causing the molecules to become close

16:02

and then making the regions become

16:04

warmer. Okay.

16:07

Ayan. Parang this one. Okay. Tingnan

16:10

natin yung molecules. When molecules

16:12

rises, it expands.

16:15

Okay. When uh air sinks,

16:19

okay, it becomes compress. Parang ganun

16:21

lang ating scenario. Nakukuha? Ayan.

16:25

Next. Altitude.

16:28

Okay. So, altitude lang. Okay. It's the

16:30

height above Ca level. Okay, tandaan

16:32

natin the height above Ca level, the

16:35

higher you go, of course, the cooler it

16:37

gets dahil syempre bumababa ang

16:40

pressure. Okay? Tig nga ang pressure,

16:42

low pressure is nasa high um altitude.

16:47

Okay? So tatandaan natin, altitude is

16:49

the height above Ca level. The higher

16:51

you go, the cooler it gets. Dahil nga

16:55

sabi nga natin bumababa yung air or

16:57

pressure. Okay? So height express as the

17:01

distance above a reference point which

17:03

is normally sa level or ground level.

17:06

Okay. It pertains to height lang namin.

17:09

Okay? Ayan.

17:11

Next.

17:13

Humidity. Okay. The degree to which the

17:16

air is charged with water vapor, this

17:18

may be expressed as an absolute

17:20

humidity, relative humidity and specific

17:23

humidity. Okay? So dito sa humidity the

17:26

amount of water vapor in the air. It's

17:28

the amount of water vapor present in the

17:31

air. Okay? It can be yun nga sabi ko

17:34

absolute relative or specific. So iyung

17:37

atin the higher the humidity the more

17:40

moist the air fail. the air fills. Okay?

17:44

Kumbaga 'ag mataas ang humidity parang

17:48

um ma-moist 'yung buong region. Okay?

17:52

Pag nangyari 'yun, ibig sabihin parang

17:55

mataas 'yung humidity. Okay? Pag mataas

17:57

'yung humidity mga anak, kadalasan ah

18:00

let's say nagpapawis tayo, mga ganyan.

18:03

Okay? Pinagpapawisan.

18:05

Okay. Next.

18:09

Pag-asa. Okay. So ano naman yung

18:12

pag-asa? Okay. Pag-asa is the Philippine

18:15

Atmosphere Geophysical and Astronomical

18:18

Services administration is responsible

18:21

for the provision of weather forecast

18:23

and tropical cyclone cyclone warnings,

18:26

flood bulletins and advisories and

18:28

hydrological, climatological and far

18:31

weather forecast. Okay. Kumbaga ito yung

18:34

agency sa Philippines. Okay. This is the

18:37

our agency or official agency na

18:39

nagmo-monitor ng weather, typhoons and

18:42

storms, even the flood advisories, ano.

18:45

So lahat ng warning about bagyo galing

18:48

sa kanila. Okay? It's Pag-asa. Tandaan

18:51

Philippine Atmospheric, Geophysical and

18:53

Astronomical Services Administration.

18:57

Okay. Pagbagyo, pag-asa. Okay. So next.

19:02

Ayan.

19:03

So a storms, okay storms is the

19:06

atmospheric disturbances that are

19:09

typified by lightning, thunder, heavy

19:12

precipitation and powerful winds.

19:15

Examples, tornadoes, blizzards, okay,

19:18

and tropical cyclopes are examples of

19:20

storm forms. Okay? So yung ating storm

19:23

are atmospheric disturbances, ano? Okay

19:26

na merong mga lighting okay and then may

19:29

mga dalang thunder and strong weight.

19:33

Okay. So kadalasan yung storms natin

19:35

dito sa Philippines we have typon. Okay.

19:40

Next we have intertropical convergence

19:43

zone. Ano naman yyung intertropical

19:45

convergence zone? An area close to the

19:47

equator where the trade winds and the

19:49

northern

19:51

winds of the northern and southern

19:52

hemisphere meet. I ating wind from the

19:55

northern and southern hemisphere meat.

19:58

'yung area kung saan sila nagtatagpo is

20:00

known as the intertropical

20:03

convergence zone. Okay? Yung wind po

20:06

galing sa north and then sa south ay

20:08

nagme-mit. Kung yung area kung saan sila

20:10

nag-met is the intertropical convergent

20:14

zone. Okay? Pag nagme-meet sila, okay,

20:17

napapansin natin pwedeng maka-form ng

20:19

mga clouds and it can create, okay,

20:22

storms. Okay, thunderstorms. Okay. And

20:26

ito yyung area, okay? Ito yung din

20:28

nakakatulong nung ating ITZ. Okay. Is a

20:31

factor kung bakit nakakabuot tayo ng mga

20:35

bagyo, okay? Or typon. Okay. Sabi diyan

20:39

'yung ITCZ natin is 'yung zone na

20:41

malapit sa equator. Kung makikita natin

20:43

'yung red line. Okay. So it is near the

20:46

equator where the trade winds from the

20:48

north nga. Okay. And then south pyramid.

20:52

Okay. So yung area na iyon has warm

20:54

ocean water and intense sunlight. Okay,

20:58

because of this air in the ITCZ becomes

21:01

warmer and more humid. Okay. So, the

21:04

converging trade winds, nagco-converge,

21:07

nagme-mind, push the warm air upward.

21:11

Pinu-push nila. Okay. Pag nagbanggaan

21:13

yung dalawa, pinu-push nila yung air

21:15

upward causing a chain of convection

21:18

process. 'Di ba? Pag nagra-rise ang wind

21:21

or yung air rises, it will create what?

21:25

Low pressure area. Kasi pag nagtaas yung

21:28

wind, tumaas, umangat, okay, the

21:31

molecules will expand and the region in

21:34

that parts become cooler. Okay? So yun

21:36

iyung pinaka-perfect condition for a

21:39

storm to be form. Ayan. So sige. Okay.

21:43

Sabi pa dito, ano pang sinasabi yan? The

21:45

converging trade push the warm air

21:47

upward. Kaya nga causing a chain of

21:49

convection process. yung it the air

21:52

rises, okay, it expand, it cools. And

21:55

then pag nag-cool down yung air area na

21:58

yun, it can form clouds. Kaya nga yung

22:00

nakita ninyo kanina, clouds or bands of

22:03

clouds and then will okay ano po okay

22:06

release, a rain, okay and then thunder

22:10

storms. So in tropical countries na atin

22:12

like the Philippines, the movement

22:14

syempre of the ITZ affects our seasons.

22:18

Okay. So, we experience this thing two

22:20

seasons lang naman. Wet and dry seasons.

22:23

Ano, if the ITCZ stays too long, okay,

22:26

pag nag-stay siya too long in one area,

22:29

okay, magkakaroon diyan ng severe

22:32

weather disruptions. Okay? Magkakaroon

22:34

ng severe weather disruptions talaga,

22:37

okay? Or possible may mga storms,

22:39

madaming storms yung mabuo diyan. Okay.

22:42

At yung ating ITZ sometimes tinatawag

22:46

din siya na DU drums. Ano ba yung DL

22:48

drums? Okay. In in other references ang

22:52

meaning ng dull drums D O L D R U N S.

22:56

Ang meaning niya is yyung area of a very

23:00

width because the air is mostly rising.

23:04

Okay? Very calm wind. Kasi 'yung air nga

23:07

is nagra-rice. Bakit po nag-rise 'yung

23:09

wind or tumaas? Because 'yung northern

23:12

and southern ah wind or trade winds

23:15

converge or met. Okay. So hopefully

23:20

nakuha natin yung explanation. Sobrang

23:21

haba. Ayan. So next yan. So before tayo

23:27

mag-proceed, panoorin natin iyung video

23:29

about intertropical convergence zone.

23:32

Okay? So the intertropical convergence

23:34

zone or also known as the ITCZ air

23:37

becomes more ayan humit okay during this

23:41

time and boyant nagiging magaan causing

23:44

it to rise ano due to the combination of

23:47

warm tropical waters and intense

23:50

sunheat. So by joining forces the trade

23:53

winds help elevate the buant air which

23:55

sets off a chain of thunderstorms. As

23:58

the air rises ba sabi as the air rises

24:01

it expands. Ano yung nag-expand? Yung

24:04

mga molecules and it cools. Okay? It

24:07

cools down the whole region releasing

24:09

stored moisture. Okay? Unlike the

24:12

typical cold and warm season found in

24:14

the higher latitudes, the seasonal

24:16

movement of the ITCZ results in changes

24:19

in rainfall. in many tropical countries

24:22

giving rice to distinct wet and dry

24:25

seasons. Ito yung main reason kung bakit

24:27

two season lang din yung ating

24:28

nae-experience. Okay? A unique to

24:31

tropical regions. So severe weather

24:33

disruptions may arise from extended

24:36

movements within the ITC. Okay. So

24:39

tatandaan natin.

24:41

So next we have low pressure area. Okay.

24:44

So what is a low pressure area? An area

24:46

with meteorological characteristics such

24:49

as cloud cover, precipitation,

24:52

temperature and wind that is

24:54

characterized by lower air pressure than

24:56

the surrounding area. Okay. So dito sa

25:00

atin yan tingnan natin low pressure

25:02

area. 'Di ba sa low pressure area, sabi

25:04

ko sa inyo mga anak kanina, okay? The

25:08

air rises up and then the molecules will

25:11

expand causing the regions to become

25:14

cooler. Pag naging cool, nakaka-create

25:16

na ng mga bands of clouds, yan na

25:19

sunod-sunod na. 'ag may bands of clouds

25:21

na, may mga group of clouds na,

25:24

makaka-create na tayo ng mga

25:25

thunderstorms or even r. Okay? So

25:29

hopefully is nakakasunod tayo. Ano?

25:32

Ayan. Okay. So dito sa low pressure area

25:36

na there is a convection or heat

25:38

transfer through fluids. Okay? Like air

25:41

and the water. Okay? So hot air becomes

25:44

less dense causing ito rice kaya

25:47

nagiging less dense, nagiging buant,

25:49

magaan causing it rice. Okay? So cooler

25:53

air sinks and this creates the

25:55

convection current. Okay. So an LPA is

25:59

an area or low pressure area is an area

26:02

where the air pressure is lower than its

26:06

surroundings. Okay? Kaya naging cooler

26:08

eh. When air converge into the LPA,

26:11

okay, it rises, okay? Or cools and forms

26:14

clouds. This leads to rain or tenter

26:17

storms like what I'm explaining earlier.

26:20

Okay. So, an LPA can intensify into a

26:22

tropical depression. Pwede siyang

26:24

ma-intensify. May mga level agag meron

26:26

na tayong LPA or low pressure area,

26:30

pwede siyang ma-intensify mga anak.

26:32

Okay? Or mag kung let's say what do you

26:34

mean? How can I explain the word

26:36

intensify? Pwede siyang mag-level up,

26:39

okay? Kumbaga pwede siyang magmature,

26:42

okay? Like for example, from low

26:44

pressure area, pwede siyang maging

26:46

tropical depression, tropical storm

26:48

until such time na maging typhoon siya,

26:51

maging super typon or worst. Okay? Yun

26:54

yung pinaka-stages na yon. Okay? Kaya

26:56

nga pag may low pressure area, laging

26:58

binabantayan ng pag-asa kasi nandiyan

27:01

na. Okay, possible may ma-create, okay,

27:04

na bagyo. Okay. So, convection is a mode

27:08

of heat transfer that occures in fluids.

27:11

Tatandaan natin, it allows hot fluids to

27:14

be less dense, okay? Causing the fluid

27:17

to rise, making the cool air sink. Okay,

27:21

this is called the current or the

27:22

convection current. Okay. So 'ag mayong

27:26

convection current, okay, it makes 'di

27:29

ba sabi diyan? It makes or uh allows hot

27:32

fluids, hot fluids, hot fluids to be

27:36

less dense yung hot fluid magiging less

27:38

dense causing it okay and then yung sa

27:41

taas ng mga cool air making the cool air

27:45

sink. Okay? Yung process or yung

27:47

pag-ikot na yon ng cool and warm air is

27:51

conduction correct.

27:53

So in terms of LPA it is an area with

27:55

meteorological characteristics such as

27:58

cloud cover, precipitation temperature

28:02

and wind that is characterized by lower

28:05

air pressure than the surrounding area.

28:08

The air r ris rises cools and forms

28:11

cloud as it converges into the LPA which

28:14

causes rain or storms to form. Okay. To

28:19

form. The LPA has the potential to

28:21

intensify into many weather systems such

28:23

as storms or tropical cyclopes. Kumbaga

28:26

ito 'yung summary nung ating discussion.

28:29

So next, you can watch a video, okay,

28:32

about low pressure area and how it

28:34

affects yung mga aviation um aviation

28:39

ah what do you call this? Yung aviation

28:42

yung sa mga ano paano ba nakakaapekto

28:44

yung low pressure era sa aviation.

28:48

Ah yung sa mga airplane okay kung paano

28:52

ba sila paano ba nagkakaroon ng

28:55

tinitingnan din ng mga pilot kung saan

28:58

okay yung high and low pressure area at

29:00

yun yung mga iiwasan nila kasi pag

29:03

possible agag hindi nila yan na-track

29:05

kung saan yung may low pressure area at

29:07

sila ay nakadaan doon okay nakadaan yung

29:10

ating mga planes or airplane possible

29:13

maka-cause yun ng turbulence okay which

29:16

ah possible accidents, okay, or

29:19

magkaroon ng mga crash or worse. Okay?

29:22

So yun lang po kung paano nakakaapekto

29:24

itong low pressure area sa aviation

29:27

process. Okay. So next,

29:30

exploring the types of tropical

29:32

cyclones. Ano ba yung types ng tropical

29:34

cyclones? For the objective, students

29:36

will identify the different types of

29:38

tropical cyclones and discuss their

29:40

characteristics and differences, ano.

29:43

Okay. So, let's start.

29:46

So first is the tropical cyclone. Ito po

29:49

according to pag-asa yung ni-release

29:51

nila. Okay. Kung gaano ka lakas yung

29:54

kanila or speed nung hangin. Okay. First

29:56

stages. Okay. Pag may LPA tayo mga anak

29:59

at ito ay nag-intensify, pwede siyang

30:02

magka-create ng tropical cyclone. Okay?

30:05

Ano ba yung tropical cyclone?

30:08

The general term for a storm system that

30:10

forms overwarm or tropical oceans. It

30:13

include tropical depression, tropical

30:15

storm, and typhoon. So tandaan natin mga

30:18

anak. Okay. Mayon po tayong iba't ibang

30:20

type ng tropical cyclone depending on

30:22

the area or location. Okay? So,

30:25

hurricane ang tawag natin if yung ating

30:27

tropical cyclone ay nag-originate sa

30:30

Atlantic at Northeast Pacific Ocean.

30:33

Okay. So the term used for tropical

30:35

cyclone here is hurricade. Pag yung atin

30:38

namang tropical cyclone ay na-form in

30:40

South Pacific and Indian Oceans, the

30:43

term used for tropical cyclone is just a

30:45

word cyclone. Pero pag ang tropical

30:48

cyclone ay na-form in Western Pacific,

30:51

the term used for tropical cyclone is

30:53

typon. like what we are using here in

30:56

the Philippines. Kasi nga iyung mga

30:58

tropical cyclone na nafo-form sa

31:01

nafo-form ay sa Western Pacific. Kaya

31:03

yung term natin ay typon. Sa US

31:07

Hurricane ang kanilang term kasi nabuo

31:10

yung tropical cyclone sa Atlantic at

31:12

Northeast Pacific. Okay? Sige. So

31:17

classification of tropical cyclones by

31:19

wind strength and it is according to

31:21

Pag-asa naman.

31:23

Okay. So, decode, the number. Okay. So,

31:27

what is the answer here? A tropical

31:29

cyclone with maximum sustain winds of up

31:32

to 61 km/h.

31:34

Okay, it's a tropical depression. Ag

31:36

yung ating sustained winds is up to 61

31:38

km/h, it's a tropical depression. This

31:41

is the first stage where iyung LPA natin

31:44

mga anak, ay nag-intensify.

31:46

Okay? Kumbaga nag naglevel up siya.

31:50

Okay. Naging tropical depression na.

31:53

Okay. So yan. Naku, nakakatakot na 'yan.

31:56

Delikado na bakaform siyang typon. Ano

31:59

sir ang tropical depression ba possible

32:01

malusaw? Possible naman k malusaw siya

32:04

especially kung walang enough or yung

32:06

conditions is hindi na met ano. Okay

32:09

after this tropical depression kung siya

32:11

ay nag-intensify pa okay it can level

32:14

up. Okay? A tropical cyclone with

32:16

maximum wind speed of 62 to 88 km/h.

32:20

It is known as tropical store. Okay,

32:23

tumaas na yung kanyang wind speed naging

32:26

62 to 88 km/h. And then let's say

32:29

nag-intensify pa siya. Okay. A stronger

32:32

tropical cyclone with maximum sustained

32:35

winds of 89 to 117 km/h. Tatawagin natin

32:39

siyang sever tropical storm or STS.

32:43

Okay? Pero pag nag-intensify pa to, ayan

32:46

na buo na. Okay. A mature tropical

32:49

cyclone with maximum sustained winds of

32:52

118 to 184 km/h.

32:56

It's a typhoon. Okay. Yan na maging

32:59

typon na. Okay. And then let's say yung

33:01

typon nag-intensify pa. Super intensify.

33:05

Okay. The most intense tropical cyclone

33:07

with maximum sustained winds of 185 km

33:12

perhour or higher. Okay? So it's super

33:15

typon. 'Yung ibang mga books, it's 200

33:18

km/h yung kanilang nakalagay ng super

33:21

typon na 'to. Okay? At ngayong taon may

33:25

mga super typon na pumasok sa Pilipinas.

33:29

Okay? So nakakatakot ano? Ayan. So those

33:32

are the classification of tropical

33:35

cyclones. Okay.

33:37

Ayan. So for our activity number four,

33:39

observing the Philippine area of

33:41

responsibility. Students will examine

33:43

the Philippine area of responsibility

33:45

and answer guide questions to understand

33:48

its role in tracking tropical cyclone.

33:51

Okay? Ano naman yung ating ano dito? So

33:54

the Philippine area of responsibility

33:57

okay or par is a designated region in

33:59

Western Pacific where the Philippine

34:02

atmospheric geophysical and astronomical

34:05

services administration. Okay? Or

34:08

pagasam monitors weather disturbances

34:10

like tropical depression, storms and

34:12

typhoons. So here mga anak, yung ating

34:16

par or yung Philippine area of

34:18

responsibility, ito yung area kung saan

34:20

nagmo-monitor yung pag-asa. Tandaan

34:22

natin na yung par is iba yan doon sa ah

34:26

what do you call this? Anong tawag natin

34:28

doun? Sa ah boundaries, okay? Or area ng

34:32

Philippines kung saan yung sakop niya.

34:35

Ang Philippine area of responsibility is

34:37

for ano lamang to for weather

34:40

observations. Tatandaan natin monitors

34:43

weather disturbances lamang.

34:46

So what can you say about the

34:48

geographical location of the

34:49

Philippines? What can you say location

34:52

ng Philippines? It is surrounded by

34:54

oceans and lies near the Pacific. Kaya

34:57

nga tayo is prone to typhoon kasi tayo

34:59

surrounded by oceans. And remember that

35:01

typhoons is formed in the oceans because

35:04

ocean is the main source of energy for

35:08

typons. Tandaan natin mga anak, pag ang

35:10

bagyo ay nasa tubig, malakas siya. But

35:13

once the typon landed or it make a land

35:16

pole in a land or in a continent, okay,

35:20

the typon will weaken. Kaya nga during

35:23

the times when na typon reaches Shar

35:25

Madre, it weaken kasi lumalayo siya sa

35:28

source of energy niya which is water.

35:31

Pero pag umano ulit siya sa tubig, okay,

35:34

pwedeng maka-regain siya ng strength,

35:37

okay? Or lakas ulit. Okay? Basta yung

35:40

mga landforms, it can awaken a typon. So

35:43

what environmental phenomena can be

35:45

associated with the location of the

35:47

Philippines?

35:49

So answer typhoons, earthquakes and

35:51

volcanic eruption. So ito yyung mga

35:53

environmental phenomena na associated sa

35:56

location natin. Okay? Typhons, which is

35:58

our topic and earthquakes and volcanic

36:01

eruptions because we are um or we are we

36:05

belong to Pacific Ring of fire. Okay.

36:09

Next. What are the effects of this

36:12

phenomena on Filipinas? Ano ba yung

36:14

epekto sa atin? Damage to houses, loss

36:17

of lives, and floods. Okay. So ito yung

36:19

common ano. So hopefully naman kaya

36:22

maayos na yung mga sistema especially sa

36:24

flood control. Charing. Okay. So what do

36:27

you think are the conditions? Why we

36:29

experience this phenomena? Ano iyung mga

36:32

conditions? Okay? Because the

36:33

Philippines is near the Pacific Ocean or

36:36

Ty's form. Ito yung pinaka

36:40

reason kung bakit na-experience natin

36:42

yung mga um what you call this phenomena

36:46

na yon. Okay? So especially typon. So

36:50

for activity number five, the highlight

36:53

conditions for typon formation. Students

36:55

will identify and discuss the different

36:57

conditions needed for a typhoon to form.

37:00

Ano ba yung conditions or kailangan

37:02

natin para mabuo ang isang bagyo?

37:05

So pwede nating panoorin muna itong

37:07

video bago tayo mag-proceed.

37:09

Okay. So condition to form a typon.

37:12

Okay. So of course okay this one, this

37:14

part okay the center is the eye. Okay.

37:18

This one. Okay. Um the part where it

37:23

surrounds the eye. Okay? It's the eye

37:25

wall. Kumbaga ito yung uh wind. Okay na

37:30

pumapalibot doun sa ey sa gitna and in

37:33

the eye wall okay the air is strong

37:35

kumbaga ito yung napakalakas kasi ano po

37:38

ba ang eye yung eye ng bagyo is the calm

37:41

part of kumbaga calm part okay kalmado

37:45

tril pero yung ey niya yung nakapaligid

37:48

yun yung pinakamalakas

37:50

okay malakas iyung ah hangin okay and

37:54

then we also have okay feather rain

37:57

bands Okay. Meron tayong mga ah inner

38:01

and outer raid bands. Okay. This one is

38:04

cooling condensing air. Nasa baba is

38:08

warm air that rises. Okay. When the warm

38:11

air rises, okay, to a low pressure area.

38:15

Okay. Kasi nga naging buant iy warm air

38:18

na iyan. Okay? It will rise and then

38:20

when the air rises, the molecules will

38:24

expand and cool, okay? Causing the

38:27

regions to ah form clouds, okay, and

38:31

tender storms. Okay. So, next.

38:36

So, ito yyung mga conditions para

38:38

makaform tayo ng typhoon or bagyo. First

38:41

is tropical location. Dapat nasa 5° to

38:44

20° latitude. Okay? Tandaan natin,

38:48

typhoons usually form in this warm ocean

38:51

zones. Okay? Tatandaan natin yan ang

38:54

pinaka region, okay? Kung saan yung

38:58

ating bagyo ay posible lamang mabuo.

39:02

Okay? Kaya nga wala pong mga bagyo doun

39:04

sa um ating pols 'di ba? Okay? Kasi nga

39:09

hindi niya namet yung ganitong

39:10

kondisyon. Okay. So here yan tropical

39:15

location.

39:17

Next warm sea surface. Dapat yung ah

39:21

temperature nung surface or

39:24

sea or ocean is nasa 26.5°

39:28

or higher. Okay? So warm water gives

39:30

energy to the storm. Tatandaan natin

39:32

that yun yung pinaka-source niya ng

39:35

energy.

39:36

Third,

39:38

moist air. Okay. Okay. Pag may moist

39:41

air, mataas yung humidity, it provides

39:44

fuel for clouds and heaving. Okay. Next.

39:51

Okay. ITCZ or the intertropical

39:53

convergence zone. Trade winds and low

39:55

pressure area helps storm start. Okay.

39:58

So here sa intertropical convergence

40:01

nabanggit naman natin kanina it's when

40:03

the trade winds the northern and

40:05

southern uh trade winds met or converge

40:08

and when they converge it can create low

40:10

pressure area because it help the uh air

40:14

to rise. Okay? Nagra-rise and when the

40:17

air rises, okay, the air or the air

40:20

molecules expands and it can create

40:22

cooler regions creating a bond of

40:24

clouds. will uh certainly okay uh create

40:28

thunderstorms okay and many more.

40:34

Ayan so sige corolus effect number five

40:37

earth's rotation makes the storm spin.

40:39

Bakit kaya umiikot po yung ating storm

40:42

ano it um Earth rotation makes the storm

40:45

spin. Sir, paano po ba 'yung paano ba

40:48

'yung paglalakbay ng hangin? Okay

40:51

straight dapat 'yan din nga straight.

40:53

Okay. Yung paglalakbay or yung travel ng

40:55

hangin. Pero sir, bakit doon kanina

40:58

parang yung hangin is parang paikot?

41:01

Okay. Okay. Dapat straight yon. But

41:04

because the earth rotates kasi

41:06

nagro-rotate yung ating earth gumagalaw

41:09

yung ating air din. Okay? Parang

41:11

napapaslant niya. Okay? Ang tawag natin

41:14

doon sa parang nag-spin yung air is

41:17

corolis effect. Okay? Because bakit

41:21

parang nag-spin yung air? It's because

41:24

uh the earth rotates. Kung steady po ang

41:27

earth hindi gumagalaw, possible straight

41:29

yung travel ng air. Okay? Pero dahil nga

41:32

nagro-rotate siya, okay, it

41:36

create corolis effect. Okay, that helps

41:39

the typons uh or storm to spin.

41:44

Okay, next, why do you think typons do

41:46

not usually form near the equator or 0

41:49

degree latitude? Okay? Kasi nga because

41:51

there is no corolus effect to make them

41:54

spin. Wala namang corolis effect doon.

41:57

Okay. Next. How does Ocean water

42:00

contribute to the strength of a typon?

42:03

Okay, it gives heat and moisture that

42:05

power the store. Okay, so proceed tayo

42:09

sa formative assessment. Okay, choose

42:12

the letter of your answer. In which of

42:13

the following layers of the atmosphere

42:15

does weather occur? Correct. In the

42:17

troposphere.

42:19

Next, which of the following is the

42:21

generic term for an intense circulating

42:23

weather system over tropical seas or

42:26

ocean? Correct. It's letter C tropical

42:29

cyclone. How is the weather in the eye

42:32

of the typhoon described? Ano yung sabi

42:34

ko kanina? Okay. It's cal ano? Okay.

42:37

Yung violent talaga is nandun sa eywall.

42:41

How does the land form affect typhoons?

42:43

Paano nga nakaka-affect iyung landform?

42:44

Like what I'm talking to Sharad earlier,

42:47

it makes the typon more violent. It

42:49

disrupts the rotation of the typhoon. It

42:52

helps the formation of typhoons or it

42:54

does not affect the typhoon at all.

42:57

Correct. It's letter B. It disrupts the

42:59

rotation of typon. Okay. Para maweaken

43:03

yung type natin. What causes tropical

43:06

cyclones to spin? Bakit ang spin?

43:08

Gravitational pool of the sun,

43:09

gravitational pool of the moon,

43:11

revolution of the earth around the sun,

43:13

or rotation of earth in its axis? Ang

43:16

sabi ko kanina, because of rotation of

43:19

earth in its axis. Okay? So hopefully

43:24

you learn something for our discussion.

43:26

So kayo na lang mamans magpahaba kung

43:28

meron po kayong idadagdag. Pero I think

43:31

mga dapat nating idagdag like for

43:33

example yung parts, okay, madi-discuss

43:35

naman natin siya in the following weeks.

43:37

So no need to be to worry. Okay?

43:39

Especially mga storm warning signals,

43:41

madi-discuss natin yan in the following

43:43

weeks. Okay? So, thank you again and

43:46

have a good day. M.

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