Quarter 3: Science 8 Week 4 | Conditions for Storms | MATATAG Curriculum
FULL TRANSCRIPT
Okay. So, welcome grade 8 students.
Okay, so this week is for week number
four ano and I hope you enjoyed our
lessons from week number two and 3.
Okay, types of eruption and types of
volcano. So, mga mam pinagawa ko kasi
sila dito ng mga bulkan e and then
pina-erupt namin ah in the class and
then they really enjoy it. Okay. So
hopefully naman. Okay. And then next
year may mga ganun pa din tayo. Okay? Sa
grade 8 pa din. Hopefully sa grade 8 pa
din ako next year ano. And for today's
lesson, we're going to talk about
storms. Okay? Yes. Okay. You've heard it
right. Let's dig deeper and understand
them even better. Okay. So since our
country is prone to typhoon or uh
storms, okay, mas maganda na mas
maintindihan ninyo yung mga anak kung
papaano ba sila nabubuo or ano yung mga
conditions for it to be. Okay? So I am
Sir Wawi, Rever Curious Science Buddy.
Don't forget to like, share, and
subscribe para lagi kayong updated sa
mga susunod pang videos. All right,
let's begin. So our topic for week
number four it's like um what do you
call this preparatory topic kasi medyo 3
weeks natin okay na idi-discuss yung
about typhoons like
formation of typhoons, parts of typhoon
and then the typon prepare preparedness.
Okay? So madali lang naman siya. Ayan.
So for our topic it's about condition
for storms. Ayan for the learning
competency, gather information from
secondary sources to explain how
typhoons develop and why the Philippines
is prone to typons. And for our learning
objectives, locate the Philippine area
of responsibility in the map. Explain
why the intertropical convergence zone
or the ITCZ is a factor for storm
formation. And then three, determine the
conditions needed to form a typhoon. Ano
ba yung mga conditions or factors for a
typhoon to be formed? And then number
four, differentiate the types of
tropical cyclones. Okay? And then number
five, identify the parts of a typhoon.
Actually, iyung parts of a typon is um
hindi natin dito madi-discuss to be
specific, it is part of week number
five. Okay. And then number six,
describe the situation in each storm
signal wording. Similar din ito. Okay?
Hindi rin natin siya mata-touch. Okay?
Part siya ng week number ah five, okay?
Or six. I'm not sure about that. But
hindi natin siya possible or hindi natin
siya madi-discuss dito. So ang atin
lang, sinunod ko lang po kasi yung nasa
le kung ano yung objectives doon. So
possible yung ating ma explain yung sa
Philippine era responsibility, the
intertropical conference zone. Okay? And
then yung ating types of tropical
cyclones together with the conditions.
Yun yung highlight ngayon sa ating
discussion. Conditions needed to form a
typon. Okay? So pwede nating i-erase
yung 5 and six if you want. Okay? So for
our review, okay, part of our review,
layers of the atmosphere. And I know
that you are already familiar with the
different layers of atmosphere, right?
Grate. Okay. So sige. Okay. So for its
description we have okay altitude is
zero from the earth surface to 12 km. It
varies up to 8 km at pols okay 18 km at
equator. Okay. So for notes, it's the
closest layer to earth surface. It
contains 75 to 80% of atmosphere's mass
and all weather events. Okay. And then
clouds like rain, storms will cure here.
And then the temperature decreases with
altitude about 6.5°
celsus per km. Okay. So what layer is
being described in this um slide?
What do you think? It's correct.
Okay, it's the troposphere. Okay, so
ayan po. And then nandiyan din po
lumilipad sa troposphere yung mga
parachute. Okay. Dumadaan yung mga
airplane, something like that. Okay. And
then the clouds, the rain. Okay. So
next, what about this one? So for its
altitude is ranging from 12 to 50 km.
Okay. Altitude mga papataas. kung gaano
sila kataas. Okay. It contains the ozon
layer which absorbs harmful UV
radiation. So ozon layer in chemistry O3
ano which absorbs harmful UV radiation.
And then sabi dito airplanes fly in the
lower stratosphere okay or sort of
troposphere ano to avoid turbulence.
Okay. So next temperature increases with
altitude due to ozone absorption of
ayan. So what layer is this? Okay. What
layer is being described in this slide?
What do you think? Correct. It's
ayan
the stratosphere.
Okay. So the stratosphere tandaan natin
sa stratosphere nandiyan 'yung ozen
layer. Okay. Next layer. Okay. Altitude.
Okay. From 50 to 85 km. It's the coldest
layer of the atmosphere up to 90° celus.
It protects Earth by burning up atmers.
Okay. And then temperature decreases
with altitude.
Okay. So ayan the massosphere. Tandaan
natin. It's the coldest layer because it
burns up meteors. Okay. Next.
Okay. Altitude from 85 to 60 km. It's
very hot up to 2000° Celus or more
because it absorbs high energy, solar
radiation and of course Aurora or the
northern and southern lights occur here.
Okay? Kasi nga bakit po nagkakaroon ng
northern and southern lights? Because in
this part mayong mga charged particles.
When they interact, okay, or nagkakaroon
sila ng interaction, nakaka-create sila
ng mga lights. Okay? And then satellites
and the international space station
orbit in this radian region. Okay. What
layer is this? It's the thermosphere,
ano? Okay. And next, altitude from 600
km to 10,000 km gradually merges into
outer space. Kumbaga ito na yung
pinaka-last. The outermost layer of the
atmosphere, air is extremely thine and
atoms and molecules can scape into space
mainly composed of hydrogen and helium.
Okay. What layer is this? Correct. It's
the excess, the outermost. layer kumbaga
ito na yung pinaka um what do you call
this merge uh it merges into outer space
na papunta na sa outer space and so
hopefully na-refresh tayo d sa layers of
atmosphere okay ayan so bakit ko ba yan
diniscuss or inintroduce dito may
kinalaman po ba yan sir of cours and so
where do storms form in the atmosphere
also in the layers of the atmosphere
saan po nabo yung ating storm
Okay, nandiyan na po yung sagot. Hindi
ko na itos
fear. Dapat po arelete ko ano. Okay. So,
sorry that's in the trophosphere. Sorry
for that. Okay. It's in the
trophosphere. Tandaan natin, storms form
in the trophosphere which is the lowest
layer of the atmosphere. Okay. Kumbaga
nandi yan yung mga water disturbances.
Okay, since okay, nandiyan yung mga
formation ng clouds. Okay, so tandaan
natin ang storms po ay nabubuo sa
troposphere. Okay, next.
So, before we begin, meron po akong
video ah video or before kayo
mag-continue. Meron po akong four videos
na nandon sa ating description.
Hopefully mapanood niyo muna before tayo
before ninyo i-continue na manood ng
video kasi it's important for you to
understand what I'm talking ah what I'm
talking here ano. So hopefully panoorin
niyo muna bago tayo mag dito sa ating
lecture or magpatuloy. So nasa link po
okay or nasa description ng ating video
yung link ng bawat video kasi pa ako
pwedeng mag-play dito baka tayo
ma-report. Okay. So, what is the role of
air pressure and temperature in the
typon formations? Okay. So, meron po
bang role or may factor ba? Okay. Yung
ating pressure and temperature in the
formation of typhoon.
Okay. So, of course, ayan. So the answer
is yes. Okay. So meron pong kinalaman or
merong role na ginagampanan yung
pressure and temperature in typhoon
formation because warm air rises. Okay?
Warm air rises. Okay? Low pressure
forms. Okay? So sa low pressure area,
okay? Umaangat, okay? Or tumataas yung
ating air or warm air. Okay. And then
pag nag uh tumaas yan, it will cause
strong winds and rain. Kasi nga habang
tumataas yung ating warm air, okay, the
air or the regions in that part becomes
cooler, okay? And then it the molecules
in that part expands. Okay? So yun yung
pinaka-reason. Okay. Kung bakit sa ating
low pressure area, okay, nabubuo yung
ating mga storms. Okay? So ipapaliwanag
ko pa rin naman yan later kung ano ba
yung kinalaman ng pressure, okay sa
formation ng typhoon. Okay. And then how
does the latitude of a place relate to
its temperature? Okay. Air pressure. How
does the latitude of a place rate to its
temperature or air pressure? The answer
is near the equator. Sa atin sa equator,
it's too hot and low pressure. Okay.
Nearp, cold and high pressure. So in
this part, okay, in this part ha or
papipiliin ko kayo low pressure and high
pressure, saan diyan possible mabuo yung
ating typhoon or storms? In low pressure
or in high pressure? Correct. Okay. In
low pressure area. Okay. So kadalasan
din yan or madalas talaga nandiyan po
nabubuo yung ating mga typon sa low
pressure area. Okay? Ang high pressure
kasi mga anak it can cause clear sky.
Okay? Yung mga ganyan sa high pressure
natin. Sa low pressure ito yung may mga
cloudy. Okay yung paligid. Okay kasi nga
tumataas yung warm air expands. Okay the
region and that part becomes cooler.
Okay so next. So for our activity number
one decoding storm conditions. So at the
end of the activity students will be
able to identify and understand key
terms related to the conditions
necessary for a storm formation by
decoding hidden words using number
letter substitution. So nagawa na naman
natin ito. Okay? So parang magde-decode
lang tayo. Ano? So this one, A is for
number one, B is for number two, and so
on and so forth. Okay? So kumbaga
ide-decode niyo lang for you to come up
in the correct word. Okay? So are you
ready? So let's start. What about this?
Okay. So raise your hand or you just
have to try this. Pause the video para
makapagsagot.
Correct. It's adiabatic temperature
change. Okay. Next.
Correct. It's air pressure.
Next,
it's altitude. Okay. Next,
humidity. What about this one?
Correct. It's intertropical convergence
zone.
What about this one?
Low pressure area.
Correct. Okay. It's pag-asa.
What about this one? Storms. Okay. And
then okay, we are done in that. So
syempre we those words are related to
our discussion and of course okay
di-discuss natin yun one by one ano. So
for our activity number two, sharing
insight and storm vocabulary. Let's uh
explain those vocabulary words. Okay. So
at the end of the activity students will
be able to explain the meaning of key
decoded vocabulary words and discuss
their importance in the conditions for
storm formation. So magsisimula muna
tayo sa adiabatic temperature change.
Ano ba yung tinatawag nating adiabatic
temperature change? Okay. So it means
that it is a cooling or heating of air.
Cooling or heating of the air caused by
the contraction or expansion or
expansion of air molecules as opposed
the loss of gain or heat. Okay? Sabi
diyan, "When air rises, it goes to a
place where the pressure is lower. It
expands and becomes cooler. Just what
just what I'm talking earlier. Okay. So
in a low pressure area, okay, or low
pressure, yung air is nagra-rise, okay?
Tumataas, okay? And then when it uh
rises, okay, the molecules expands and
the region becomes cooler. Okay. Kaya
nabubuo or ito yung pinaka parang good
conditions for a storm to B4. Kaya ano
naman 'yung opposing site niya? Okay.
When air sinks, it goes to a place where
the pressure is higher. It gets
compressed and becomes warmer. Okay? Ito
naman sa when air sinks. Okay. Sa higher
pressure area naman ito. Pag nag-sink sa
higher pressure area, iyung ating air is
nagsi-sink. Okay? Yung ating mga
molecules nako-compress and the regions
become warmer.
Okay, tatandaan natin. But in overall um
an overall what do you call this? Uh
event or occurrence, okay, yung ating
cooling and heating of air is known as
adiabatic temperature change. Okay?
Which occures when air rises and when
air sinks. Okay? So sige. So meron pa ba
tayong idadagdag dito?
Okay. So wala na naman. So next we have
air pressure. Ano naman yyung air
pressure natin? Okay when we say air
pressure the amount of force exerted on
a unit surface area. Okay? High
pressure, low altitude. Okay? Air is
squeeze. Okay? Nai-squeeze.
Okay? Nako-compress yung ating mga
molecules. Okay? Molecules become close
and yung effect, yung region nagiging
warmer. Okay. In um low pressure area,
yung ating low pressure area, kadalasan
yan ay nandon sa high altitude. Air
expands, then the molecule spreads out
and then the region become or becomes
cooler lumalig. Okay? So that's the main
difference. Okay. Meron tayong high
pressure at meron tayong low pressure
area. But in the two, okay? Saan po yung
good condition for a storm to be formed?
In a low pressure area? Tatandaan natin.
So sabi diyan, air pressure is simply
the force of air. Okay? Pushing on a
surface.
Okay. Tatandaan natin that in a low
pressure area lagi ang nasa high
altitude. Ano? Okay. Altitude. Okay.
Causing the air to rise. Okay. And then
yung molecules mag-spread out. Okay. The
regions become cooler. In high pressure,
low altitude lagi. Okay. Yung ating
molecules, yung air natin na-squeeze
causing the molecules to become close
and then making the regions become
warmer. Okay.
Ayan. Parang this one. Okay. Tingnan
natin yung molecules. When molecules
rises, it expands.
Okay. When uh air sinks,
okay, it becomes compress. Parang ganun
lang ating scenario. Nakukuha? Ayan.
Next. Altitude.
Okay. So, altitude lang. Okay. It's the
height above Ca level. Okay, tandaan
natin the height above Ca level, the
higher you go, of course, the cooler it
gets dahil syempre bumababa ang
pressure. Okay? Tig nga ang pressure,
low pressure is nasa high um altitude.
Okay? So tatandaan natin, altitude is
the height above Ca level. The higher
you go, the cooler it gets. Dahil nga
sabi nga natin bumababa yung air or
pressure. Okay? So height express as the
distance above a reference point which
is normally sa level or ground level.
Okay. It pertains to height lang namin.
Okay? Ayan.
Next.
Humidity. Okay. The degree to which the
air is charged with water vapor, this
may be expressed as an absolute
humidity, relative humidity and specific
humidity. Okay? So dito sa humidity the
amount of water vapor in the air. It's
the amount of water vapor present in the
air. Okay? It can be yun nga sabi ko
absolute relative or specific. So iyung
atin the higher the humidity the more
moist the air fail. the air fills. Okay?
Kumbaga 'ag mataas ang humidity parang
um ma-moist 'yung buong region. Okay?
Pag nangyari 'yun, ibig sabihin parang
mataas 'yung humidity. Okay? Pag mataas
'yung humidity mga anak, kadalasan ah
let's say nagpapawis tayo, mga ganyan.
Okay? Pinagpapawisan.
Okay. Next.
Pag-asa. Okay. So ano naman yung
pag-asa? Okay. Pag-asa is the Philippine
Atmosphere Geophysical and Astronomical
Services administration is responsible
for the provision of weather forecast
and tropical cyclone cyclone warnings,
flood bulletins and advisories and
hydrological, climatological and far
weather forecast. Okay. Kumbaga ito yung
agency sa Philippines. Okay. This is the
our agency or official agency na
nagmo-monitor ng weather, typhoons and
storms, even the flood advisories, ano.
So lahat ng warning about bagyo galing
sa kanila. Okay? It's Pag-asa. Tandaan
Philippine Atmospheric, Geophysical and
Astronomical Services Administration.
Okay. Pagbagyo, pag-asa. Okay. So next.
Ayan.
So a storms, okay storms is the
atmospheric disturbances that are
typified by lightning, thunder, heavy
precipitation and powerful winds.
Examples, tornadoes, blizzards, okay,
and tropical cyclopes are examples of
storm forms. Okay? So yung ating storm
are atmospheric disturbances, ano? Okay
na merong mga lighting okay and then may
mga dalang thunder and strong weight.
Okay. So kadalasan yung storms natin
dito sa Philippines we have typon. Okay.
Next we have intertropical convergence
zone. Ano naman yyung intertropical
convergence zone? An area close to the
equator where the trade winds and the
northern
winds of the northern and southern
hemisphere meet. I ating wind from the
northern and southern hemisphere meat.
'yung area kung saan sila nagtatagpo is
known as the intertropical
convergence zone. Okay? Yung wind po
galing sa north and then sa south ay
nagme-mit. Kung yung area kung saan sila
nag-met is the intertropical convergent
zone. Okay? Pag nagme-meet sila, okay,
napapansin natin pwedeng maka-form ng
mga clouds and it can create, okay,
storms. Okay, thunderstorms. Okay. And
ito yyung area, okay? Ito yung din
nakakatulong nung ating ITZ. Okay. Is a
factor kung bakit nakakabuot tayo ng mga
bagyo, okay? Or typon. Okay. Sabi diyan
'yung ITCZ natin is 'yung zone na
malapit sa equator. Kung makikita natin
'yung red line. Okay. So it is near the
equator where the trade winds from the
north nga. Okay. And then south pyramid.
Okay. So yung area na iyon has warm
ocean water and intense sunlight. Okay,
because of this air in the ITCZ becomes
warmer and more humid. Okay. So, the
converging trade winds, nagco-converge,
nagme-mind, push the warm air upward.
Pinu-push nila. Okay. Pag nagbanggaan
yung dalawa, pinu-push nila yung air
upward causing a chain of convection
process. 'Di ba? Pag nagra-rise ang wind
or yung air rises, it will create what?
Low pressure area. Kasi pag nagtaas yung
wind, tumaas, umangat, okay, the
molecules will expand and the region in
that parts become cooler. Okay? So yun
iyung pinaka-perfect condition for a
storm to be form. Ayan. So sige. Okay.
Sabi pa dito, ano pang sinasabi yan? The
converging trade push the warm air
upward. Kaya nga causing a chain of
convection process. yung it the air
rises, okay, it expand, it cools. And
then pag nag-cool down yung air area na
yun, it can form clouds. Kaya nga yung
nakita ninyo kanina, clouds or bands of
clouds and then will okay ano po okay
release, a rain, okay and then thunder
storms. So in tropical countries na atin
like the Philippines, the movement
syempre of the ITZ affects our seasons.
Okay. So, we experience this thing two
seasons lang naman. Wet and dry seasons.
Ano, if the ITCZ stays too long, okay,
pag nag-stay siya too long in one area,
okay, magkakaroon diyan ng severe
weather disruptions. Okay? Magkakaroon
ng severe weather disruptions talaga,
okay? Or possible may mga storms,
madaming storms yung mabuo diyan. Okay.
At yung ating ITZ sometimes tinatawag
din siya na DU drums. Ano ba yung DL
drums? Okay. In in other references ang
meaning ng dull drums D O L D R U N S.
Ang meaning niya is yyung area of a very
width because the air is mostly rising.
Okay? Very calm wind. Kasi 'yung air nga
is nagra-rice. Bakit po nag-rise 'yung
wind or tumaas? Because 'yung northern
and southern ah wind or trade winds
converge or met. Okay. So hopefully
nakuha natin yung explanation. Sobrang
haba. Ayan. So next yan. So before tayo
mag-proceed, panoorin natin iyung video
about intertropical convergence zone.
Okay? So the intertropical convergence
zone or also known as the ITCZ air
becomes more ayan humit okay during this
time and boyant nagiging magaan causing
it to rise ano due to the combination of
warm tropical waters and intense
sunheat. So by joining forces the trade
winds help elevate the buant air which
sets off a chain of thunderstorms. As
the air rises ba sabi as the air rises
it expands. Ano yung nag-expand? Yung
mga molecules and it cools. Okay? It
cools down the whole region releasing
stored moisture. Okay? Unlike the
typical cold and warm season found in
the higher latitudes, the seasonal
movement of the ITCZ results in changes
in rainfall. in many tropical countries
giving rice to distinct wet and dry
seasons. Ito yung main reason kung bakit
two season lang din yung ating
nae-experience. Okay? A unique to
tropical regions. So severe weather
disruptions may arise from extended
movements within the ITC. Okay. So
tatandaan natin.
So next we have low pressure area. Okay.
So what is a low pressure area? An area
with meteorological characteristics such
as cloud cover, precipitation,
temperature and wind that is
characterized by lower air pressure than
the surrounding area. Okay. So dito sa
atin yan tingnan natin low pressure
area. 'Di ba sa low pressure area, sabi
ko sa inyo mga anak kanina, okay? The
air rises up and then the molecules will
expand causing the regions to become
cooler. Pag naging cool, nakaka-create
na ng mga bands of clouds, yan na
sunod-sunod na. 'ag may bands of clouds
na, may mga group of clouds na,
makaka-create na tayo ng mga
thunderstorms or even r. Okay? So
hopefully is nakakasunod tayo. Ano?
Ayan. Okay. So dito sa low pressure area
na there is a convection or heat
transfer through fluids. Okay? Like air
and the water. Okay? So hot air becomes
less dense causing ito rice kaya
nagiging less dense, nagiging buant,
magaan causing it rice. Okay? So cooler
air sinks and this creates the
convection current. Okay. So an LPA is
an area or low pressure area is an area
where the air pressure is lower than its
surroundings. Okay? Kaya naging cooler
eh. When air converge into the LPA,
okay, it rises, okay? Or cools and forms
clouds. This leads to rain or tenter
storms like what I'm explaining earlier.
Okay. So, an LPA can intensify into a
tropical depression. Pwede siyang
ma-intensify. May mga level agag meron
na tayong LPA or low pressure area,
pwede siyang ma-intensify mga anak.
Okay? Or mag kung let's say what do you
mean? How can I explain the word
intensify? Pwede siyang mag-level up,
okay? Kumbaga pwede siyang magmature,
okay? Like for example, from low
pressure area, pwede siyang maging
tropical depression, tropical storm
until such time na maging typhoon siya,
maging super typon or worst. Okay? Yun
yung pinaka-stages na yon. Okay? Kaya
nga pag may low pressure area, laging
binabantayan ng pag-asa kasi nandiyan
na. Okay, possible may ma-create, okay,
na bagyo. Okay. So, convection is a mode
of heat transfer that occures in fluids.
Tatandaan natin, it allows hot fluids to
be less dense, okay? Causing the fluid
to rise, making the cool air sink. Okay,
this is called the current or the
convection current. Okay. So 'ag mayong
convection current, okay, it makes 'di
ba sabi diyan? It makes or uh allows hot
fluids, hot fluids, hot fluids to be
less dense yung hot fluid magiging less
dense causing it okay and then yung sa
taas ng mga cool air making the cool air
sink. Okay? Yung process or yung
pag-ikot na yon ng cool and warm air is
conduction correct.
So in terms of LPA it is an area with
meteorological characteristics such as
cloud cover, precipitation temperature
and wind that is characterized by lower
air pressure than the surrounding area.
The air r ris rises cools and forms
cloud as it converges into the LPA which
causes rain or storms to form. Okay. To
form. The LPA has the potential to
intensify into many weather systems such
as storms or tropical cyclopes. Kumbaga
ito 'yung summary nung ating discussion.
So next, you can watch a video, okay,
about low pressure area and how it
affects yung mga aviation um aviation
ah what do you call this? Yung aviation
yung sa mga ano paano ba nakakaapekto
yung low pressure era sa aviation.
Ah yung sa mga airplane okay kung paano
ba sila paano ba nagkakaroon ng
tinitingnan din ng mga pilot kung saan
okay yung high and low pressure area at
yun yung mga iiwasan nila kasi pag
possible agag hindi nila yan na-track
kung saan yung may low pressure area at
sila ay nakadaan doon okay nakadaan yung
ating mga planes or airplane possible
maka-cause yun ng turbulence okay which
ah possible accidents, okay, or
magkaroon ng mga crash or worse. Okay?
So yun lang po kung paano nakakaapekto
itong low pressure area sa aviation
process. Okay. So next,
exploring the types of tropical
cyclones. Ano ba yung types ng tropical
cyclones? For the objective, students
will identify the different types of
tropical cyclones and discuss their
characteristics and differences, ano.
Okay. So, let's start.
So first is the tropical cyclone. Ito po
according to pag-asa yung ni-release
nila. Okay. Kung gaano ka lakas yung
kanila or speed nung hangin. Okay. First
stages. Okay. Pag may LPA tayo mga anak
at ito ay nag-intensify, pwede siyang
magka-create ng tropical cyclone. Okay?
Ano ba yung tropical cyclone?
The general term for a storm system that
forms overwarm or tropical oceans. It
include tropical depression, tropical
storm, and typhoon. So tandaan natin mga
anak. Okay. Mayon po tayong iba't ibang
type ng tropical cyclone depending on
the area or location. Okay? So,
hurricane ang tawag natin if yung ating
tropical cyclone ay nag-originate sa
Atlantic at Northeast Pacific Ocean.
Okay. So the term used for tropical
cyclone here is hurricade. Pag yung atin
namang tropical cyclone ay na-form in
South Pacific and Indian Oceans, the
term used for tropical cyclone is just a
word cyclone. Pero pag ang tropical
cyclone ay na-form in Western Pacific,
the term used for tropical cyclone is
typon. like what we are using here in
the Philippines. Kasi nga iyung mga
tropical cyclone na nafo-form sa
nafo-form ay sa Western Pacific. Kaya
yung term natin ay typon. Sa US
Hurricane ang kanilang term kasi nabuo
yung tropical cyclone sa Atlantic at
Northeast Pacific. Okay? Sige. So
classification of tropical cyclones by
wind strength and it is according to
Pag-asa naman.
Okay. So, decode, the number. Okay. So,
what is the answer here? A tropical
cyclone with maximum sustain winds of up
to 61 km/h.
Okay, it's a tropical depression. Ag
yung ating sustained winds is up to 61
km/h, it's a tropical depression. This
is the first stage where iyung LPA natin
mga anak, ay nag-intensify.
Okay? Kumbaga nag naglevel up siya.
Okay. Naging tropical depression na.
Okay. So yan. Naku, nakakatakot na 'yan.
Delikado na bakaform siyang typon. Ano
sir ang tropical depression ba possible
malusaw? Possible naman k malusaw siya
especially kung walang enough or yung
conditions is hindi na met ano. Okay
after this tropical depression kung siya
ay nag-intensify pa okay it can level
up. Okay? A tropical cyclone with
maximum wind speed of 62 to 88 km/h.
It is known as tropical store. Okay,
tumaas na yung kanyang wind speed naging
62 to 88 km/h. And then let's say
nag-intensify pa siya. Okay. A stronger
tropical cyclone with maximum sustained
winds of 89 to 117 km/h. Tatawagin natin
siyang sever tropical storm or STS.
Okay? Pero pag nag-intensify pa to, ayan
na buo na. Okay. A mature tropical
cyclone with maximum sustained winds of
118 to 184 km/h.
It's a typhoon. Okay. Yan na maging
typon na. Okay. And then let's say yung
typon nag-intensify pa. Super intensify.
Okay. The most intense tropical cyclone
with maximum sustained winds of 185 km
perhour or higher. Okay? So it's super
typon. 'Yung ibang mga books, it's 200
km/h yung kanilang nakalagay ng super
typon na 'to. Okay? At ngayong taon may
mga super typon na pumasok sa Pilipinas.
Okay? So nakakatakot ano? Ayan. So those
are the classification of tropical
cyclones. Okay.
Ayan. So for our activity number four,
observing the Philippine area of
responsibility. Students will examine
the Philippine area of responsibility
and answer guide questions to understand
its role in tracking tropical cyclone.
Okay? Ano naman yung ating ano dito? So
the Philippine area of responsibility
okay or par is a designated region in
Western Pacific where the Philippine
atmospheric geophysical and astronomical
services administration. Okay? Or
pagasam monitors weather disturbances
like tropical depression, storms and
typhoons. So here mga anak, yung ating
par or yung Philippine area of
responsibility, ito yung area kung saan
nagmo-monitor yung pag-asa. Tandaan
natin na yung par is iba yan doon sa ah
what do you call this? Anong tawag natin
doun? Sa ah boundaries, okay? Or area ng
Philippines kung saan yung sakop niya.
Ang Philippine area of responsibility is
for ano lamang to for weather
observations. Tatandaan natin monitors
weather disturbances lamang.
So what can you say about the
geographical location of the
Philippines? What can you say location
ng Philippines? It is surrounded by
oceans and lies near the Pacific. Kaya
nga tayo is prone to typhoon kasi tayo
surrounded by oceans. And remember that
typhoons is formed in the oceans because
ocean is the main source of energy for
typons. Tandaan natin mga anak, pag ang
bagyo ay nasa tubig, malakas siya. But
once the typon landed or it make a land
pole in a land or in a continent, okay,
the typon will weaken. Kaya nga during
the times when na typon reaches Shar
Madre, it weaken kasi lumalayo siya sa
source of energy niya which is water.
Pero pag umano ulit siya sa tubig, okay,
pwedeng maka-regain siya ng strength,
okay? Or lakas ulit. Okay? Basta yung
mga landforms, it can awaken a typon. So
what environmental phenomena can be
associated with the location of the
Philippines?
So answer typhoons, earthquakes and
volcanic eruption. So ito yyung mga
environmental phenomena na associated sa
location natin. Okay? Typhons, which is
our topic and earthquakes and volcanic
eruptions because we are um or we are we
belong to Pacific Ring of fire. Okay.
Next. What are the effects of this
phenomena on Filipinas? Ano ba yung
epekto sa atin? Damage to houses, loss
of lives, and floods. Okay. So ito yung
common ano. So hopefully naman kaya
maayos na yung mga sistema especially sa
flood control. Charing. Okay. So what do
you think are the conditions? Why we
experience this phenomena? Ano iyung mga
conditions? Okay? Because the
Philippines is near the Pacific Ocean or
Ty's form. Ito yung pinaka
reason kung bakit na-experience natin
yung mga um what you call this phenomena
na yon. Okay? So especially typon. So
for activity number five, the highlight
conditions for typon formation. Students
will identify and discuss the different
conditions needed for a typhoon to form.
Ano ba yung conditions or kailangan
natin para mabuo ang isang bagyo?
So pwede nating panoorin muna itong
video bago tayo mag-proceed.
Okay. So condition to form a typon.
Okay. So of course okay this one, this
part okay the center is the eye. Okay.
This one. Okay. Um the part where it
surrounds the eye. Okay? It's the eye
wall. Kumbaga ito yung uh wind. Okay na
pumapalibot doun sa ey sa gitna and in
the eye wall okay the air is strong
kumbaga ito yung napakalakas kasi ano po
ba ang eye yung eye ng bagyo is the calm
part of kumbaga calm part okay kalmado
tril pero yung ey niya yung nakapaligid
yun yung pinakamalakas
okay malakas iyung ah hangin okay and
then we also have okay feather rain
bands Okay. Meron tayong mga ah inner
and outer raid bands. Okay. This one is
cooling condensing air. Nasa baba is
warm air that rises. Okay. When the warm
air rises, okay, to a low pressure area.
Okay. Kasi nga naging buant iy warm air
na iyan. Okay? It will rise and then
when the air rises, the molecules will
expand and cool, okay? Causing the
regions to ah form clouds, okay, and
tender storms. Okay. So, next.
So, ito yyung mga conditions para
makaform tayo ng typhoon or bagyo. First
is tropical location. Dapat nasa 5° to
20° latitude. Okay? Tandaan natin,
typhoons usually form in this warm ocean
zones. Okay? Tatandaan natin yan ang
pinaka region, okay? Kung saan yung
ating bagyo ay posible lamang mabuo.
Okay? Kaya nga wala pong mga bagyo doun
sa um ating pols 'di ba? Okay? Kasi nga
hindi niya namet yung ganitong
kondisyon. Okay. So here yan tropical
location.
Next warm sea surface. Dapat yung ah
temperature nung surface or
sea or ocean is nasa 26.5°
or higher. Okay? So warm water gives
energy to the storm. Tatandaan natin
that yun yung pinaka-source niya ng
energy.
Third,
moist air. Okay. Okay. Pag may moist
air, mataas yung humidity, it provides
fuel for clouds and heaving. Okay. Next.
Okay. ITCZ or the intertropical
convergence zone. Trade winds and low
pressure area helps storm start. Okay.
So here sa intertropical convergence
nabanggit naman natin kanina it's when
the trade winds the northern and
southern uh trade winds met or converge
and when they converge it can create low
pressure area because it help the uh air
to rise. Okay? Nagra-rise and when the
air rises, okay, the air or the air
molecules expands and it can create
cooler regions creating a bond of
clouds. will uh certainly okay uh create
thunderstorms okay and many more.
Ayan so sige corolus effect number five
earth's rotation makes the storm spin.
Bakit kaya umiikot po yung ating storm
ano it um Earth rotation makes the storm
spin. Sir, paano po ba 'yung paano ba
'yung paglalakbay ng hangin? Okay
straight dapat 'yan din nga straight.
Okay. Yung paglalakbay or yung travel ng
hangin. Pero sir, bakit doon kanina
parang yung hangin is parang paikot?
Okay. Okay. Dapat straight yon. But
because the earth rotates kasi
nagro-rotate yung ating earth gumagalaw
yung ating air din. Okay? Parang
napapaslant niya. Okay? Ang tawag natin
doon sa parang nag-spin yung air is
corolis effect. Okay? Because bakit
parang nag-spin yung air? It's because
uh the earth rotates. Kung steady po ang
earth hindi gumagalaw, possible straight
yung travel ng air. Okay? Pero dahil nga
nagro-rotate siya, okay, it
create corolis effect. Okay, that helps
the typons uh or storm to spin.
Okay, next, why do you think typons do
not usually form near the equator or 0
degree latitude? Okay? Kasi nga because
there is no corolus effect to make them
spin. Wala namang corolis effect doon.
Okay. Next. How does Ocean water
contribute to the strength of a typon?
Okay, it gives heat and moisture that
power the store. Okay, so proceed tayo
sa formative assessment. Okay, choose
the letter of your answer. In which of
the following layers of the atmosphere
does weather occur? Correct. In the
troposphere.
Next, which of the following is the
generic term for an intense circulating
weather system over tropical seas or
ocean? Correct. It's letter C tropical
cyclone. How is the weather in the eye
of the typhoon described? Ano yung sabi
ko kanina? Okay. It's cal ano? Okay.
Yung violent talaga is nandun sa eywall.
How does the land form affect typhoons?
Paano nga nakaka-affect iyung landform?
Like what I'm talking to Sharad earlier,
it makes the typon more violent. It
disrupts the rotation of the typhoon. It
helps the formation of typhoons or it
does not affect the typhoon at all.
Correct. It's letter B. It disrupts the
rotation of typon. Okay. Para maweaken
yung type natin. What causes tropical
cyclones to spin? Bakit ang spin?
Gravitational pool of the sun,
gravitational pool of the moon,
revolution of the earth around the sun,
or rotation of earth in its axis? Ang
sabi ko kanina, because of rotation of
earth in its axis. Okay? So hopefully
you learn something for our discussion.
So kayo na lang mamans magpahaba kung
meron po kayong idadagdag. Pero I think
mga dapat nating idagdag like for
example yung parts, okay, madi-discuss
naman natin siya in the following weeks.
So no need to be to worry. Okay?
Especially mga storm warning signals,
madi-discuss natin yan in the following
weeks. Okay? So, thank you again and
have a good day. M.
UNLOCK MORE
Sign up free to access premium features
INTERACTIVE VIEWER
Watch the video with synced subtitles, adjustable overlay, and full playback control.
AI SUMMARY
Get an instant AI-generated summary of the video content, key points, and takeaways.
TRANSLATE
Translate the transcript to 100+ languages with one click. Download in any format.
MIND MAP
Visualize the transcript as an interactive mind map. Understand structure at a glance.
CHAT WITH TRANSCRIPT
Ask questions about the video content. Get answers powered by AI directly from the transcript.
GET MORE FROM YOUR TRANSCRIPTS
Sign up for free and unlock interactive viewer, AI summaries, translations, mind maps, and more. No credit card required.