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7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Lesson 16Lesson 16
How do Tropical RevolvingHow do Tropical RevolvingStorms Form?Storms Form?
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We need to understandWe need to understand howhowtropicaltropicalrevolving storms are created, theirrevolving storms are created, their impactsimpactsand knowand know how peoplehow peoplerespond to themrespond to them
We should also take into account the e!!ectsWe should also take into account the e!!ectso! glo"al warming on such eventso! glo"al warming on such events
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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What drives a TropicalWhat drives a Tropical
Storm?Storm?
Cold polar airmoves
towards thewarm
equator.
Hot tropicalair moves
towards thecold poles.
The planet is not evenl# heated
$t Athe heating is more direct %intense
Whereas at Bit is spread over a
larger sur!ace area % less intense
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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What causes wind?What causes wind?This uneven heating causes air toThis uneven heating causes air to
move around the planet, trying tomove around the planet, trying to
even out the temperature.even out the temperature.
$ir moving$ir moving
around thearound the
planet causesplanet causes
our wind, whichour wind, which
generall#generall#!ollows a known!ollows a known
patternpattern
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Tropical storms
!orm "etween
&'and ()' *orth+ South o! the
euator
The# need warmwater - a"ove
(.'c/ hence their
location
$s the 0arth rotates, this provides the spin2
needed to start the tropical storm on its
3ourne# across the $tlantic towards $merica
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Tropical revolving storms occur all around
the world, "ut are called di!!erent names
11%1%
!%
11%"#%
$$%
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Warm ceansWarm ceansThe !ood2 o! a tropical
storm is the warm moistwater !ound near the
euator The air here is
under LOWpressure, which
means it can li!t easil#
This li!ting encourages the
air to cool and condense, as
it does latent heatisreleased This is the name
given to energ# produced
when a su"stance changes
state ie vapour to a liuid
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Here is a check list
o! what is needed
!or a tropicalrevolving storm
to grow
$ storm can travel an#where !rom 1& to 4)mph
5nce the stormhas developed
it can grow 4))
miles wide
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Here is a 7
image o! a
Tropicalrevolving
storm *otice
the lowerlevel winds
"eing drawn in
and spiralling
counterclockwise
The lines iso"ars2 get closer together,
indicating !aster !lowing air
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Launch the h#per linkLaunch the h#per link
How Hurricanes &ormHow Hurricanes &orm
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Tropical Storm / Hurricane KeyFacts
Hurricanes are located in the low8pressure "elt near the euator as the
sun heats the oceans to a critical temperature o! 27
CThe oceans heat up all through the summer making their warmesttemperatures in the $utumn 9speci!ic heat capacit#:; this is Hurricaneseason in the $tlantic
The hurricane starts as a tropical depression, gaining more and moreenerg# !rom the warm ocean as it crosses the $tlantic The circulation o!the depression gets tighter 9iso"ars are closer together: and the windspeed increases into a tropical storm
The wind speeds continue to increase, "ecoming a categor# 1 up tocategor# & !or the most violent storm $s the hurricane makes land!all
damage is done "# the winds and rain and an advancing storm surge,which raise sea level "# &m< in some cases
The hurricane uickl# looses its energ# as it crosses the cooler land, asthe energ# suppl# has "een cut o!! The hurricane dies
Sometimes remnants o! hurricanes are "rought across "ack across the$tlantic at the mid latitudes giving us ver# strong depressions in the =>
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How are they measured?How are they measured?'lthough developed in the (S', the'lthough developed in the (S', the Sa)r*SimpsonSa)r*Simpsonscalescaleis used to grade tropical storm wind strength inis used to grade tropical storm wind strength inmany parts o& the world.many parts o& the world.
CategoryCategory WindWind
SpeedSpeed
+mhr+mhr
WindWind
SpeedSpeed
-ph-ph
StormStorm
Surge mSurge m
Tropical stormTropical storm #*"#*" ##
TropicalTropical
depressiondepression$*11$*11 #*#./#*#./
11 11/*10$11/*10$ */0*/0 1."*1.01."*1.0
"" 10*110*1 /*11#/*11# 1.!*".1.!*".
$$ 1!*"#/1!*"#/ 111*1$#111*1$# ".*$.".*$.
"1#*"/"1#*"/ 1$1*1001$1*100 .#*0.0.#*0.0
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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Problems with the Saffri Simpson?Problems with the Saffri Simpson?
45 (sing wind speed and storm surge45 (sing wind speed and storm surgelevels 6 what pro7lems could youlevels 6 what pro7lems could you
encounter?encounter?
http8www.nhc.noaa.gova7outsshs.shtmlhttp8www.nhc.noaa.gova7outsshs.shtml
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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' tropical storm has many' tropical storm has many
&riends9&riends95ther phenomena which can "e 3ust as damaging than the wind !reuentl#5ther phenomena which can "e 3ust as damaging than the wind !reuentl#
accompan# tropical stormsaccompan# tropical storms
high seashigh seas8 large waves o! up to 1& metres high are caused "# the strong8 large waves o! up to 1& metres high are caused "# the strongwinds and are ha@ardous to shipping;winds and are ha@ardous to shipping;
storm surgestorm surge8 a surge o! water o! up to several metres can cause eAtensive8 a surge o! water o! up to several metres can cause eAtensive
!looding and damage in coastal regions;!looding and damage in coastal regions;heav rainheav rain8 the tropical c#clone can pick up two "illion tons o! moisture8 the tropical c#clone can pick up two "illion tons o! moistureper da# and release it as rain This also leads to eAtensive !looding 8 o!tenper da# and release it as rain This also leads to eAtensive !looding 8 o!tenwell inland !rom where the tropical revolving storm hit the coast;well inland !rom where the tropical revolving storm hit the coast;
torna!oestorna!oes8 tropical c#clones sometimes spawn man# tornadoes as the# hit8 tropical c#clones sometimes spawn man# tornadoes as the# hit
land which can cause small areas o! eAtreme wind damage Theseland which can cause small areas o! eAtreme wind damage Thesephenomena can cause ma3or destruction, especiall# when the tropicalphenomena can cause ma3or destruction, especiall# when the tropicalc#cloneBs path takes it over land However, a path over land also causes thec#cloneBs path takes it over land However, a path over land also causes thedestruction o! the tropical c#clone itsel! $s it moves over land, its energ#destruction o! the tropical c#clone itsel! $s it moves over land, its energ#source is depleted and !riction across the land sur!ace distorts the air !lowsource is depleted and !riction across the land sur!ace distorts the air !lowThis leads to the e#e !illing with cloud and the tropical c#clone diesThis leads to the e#e !illing with cloud and the tropical c#clone dies
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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$: model o& a Tropical$: model o& a Tropical
StormStorm
Create #our own 7
model / remem"er to
add a ke#D
7/26/2019 Lesson161HowdoTropicalrevolvingStormsform.ppt
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HomeworkHomeworkA"A A2 boo#A"A A2 boo#Eg 6)86 Read and make notesEg 6)86 Read and make notes
isit these we" sites and read around the topic / whatisit these we" sites and read around the topic / whatelse can #ou add to #our notes a"out tropicalelse can #ou add to #our notes a"out tropicalrevolving storm !ormation?revolving storm !ormation?
Waugh Eg (& + *agle Eg 4(1< has eAtra reading, 9pa#Waugh Eg (& + *agle Eg 4(1< has eAtra reading, 9pa#
particular attention to Elaces ) !or Stretch +particular attention to Elaces ) !or Stretch +ChallengeD:ChallengeD:
httpGGwww""ccoukGweatherG!eaturesGunderstandhttpGGwww""ccoukGweatherG!eaturesGunderstand
ingGhurricanec#cleshtmlingGhurricanec#cleshtmlhttpGGwwwmeto!!icegovukGweatherGtropicalc#clonhttpGGwwwmeto!!icegovukGweatherGtropicalc#cloneG!actshtmleG!actshtml
httpGGwwwnhcnoaagovGa"outsshsshtmlhttpGGwwwnhcnoaagovGa"outsshsshtml