Introductory meteorology & climatic change AMET5311 NOTES IGKV
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Aug 29, 2023
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About This Presentation
Meaning and scope of agricultural meteorology; Earth atmosphere- its composition, extent
and structure; Atmospheric weather variables; Atmospheric pressure, its variation with
height, Wind, types of wind, daily and seasonal variation of wind speed, cyclone,
anticyclone, land breeze and sea breeze...
Slide Content
The atmospheric pressure at Earth's surface is 14.7 pounds per square inch (psi). This
lis the weight of all the air above us, and it is called air pressure. High in the atmosphere, air
[pressure decreases, The standard atmospheric pressure at sa level on Earth is 1013.
for about 14.7 pounds per square inch "
ad gin, a ee
[1013.25 fan, arman 14.7 wir sf ta th
lis the weight of all the air above us, and it is called air pressure. High in the atmosphere, air
[pressure decreases, The standard atmospheric pressure at sa level on Earth is 1013.
for about 14.7 pounds per square inch "
ad gin, a ee
[1013.25 fan, arman 14.7 wir sf ta th
Pipes of win
[see winds
Erie ind]
[see winds
Erie ind]
Land and ca tren
Pana sre)
Pana sre)
[Mountain and Valley Breezes}
[Wind speed varies daily ally due to changes in temperature and pressure. A dal
[average may not be sufficient to report wind speed, and a long-term average may be more
prudent. Seasonal winds are caused by global atmospheric circulation patterns, while local winds
[are produced by the sun heating up different parts of the earth's st enly. Seasonal win
fiends to be more constant while local winds are more variabl
13
[Wind speed varies daily ally due to changes in temperature and pressure. A dal
[average may not be sufficient to report wind speed, and a long-term average may be more
prudent. Seasonal winds are caused by global atmospheric circulation patterns, while local winds
[are produced by the sun heating up different parts of the earth's st enly. Seasonal win
fiends to be more constant while local winds are more variabl
13
ructure of the ey
Emmen
Freoricau. CYCLONE]
Sarria apa ad CARA A Mer Breuer arf O at
E AR E
TRA TROPICAL/ TEMPOERATE CY
Freoricau. CYCLONE]
Sarria apa ad CARA A Mer Breuer arf O at
E AR E
TRA TROPICAL/ TEMPOERATE CY
TANT,
LONG WAVE AND THERMAL
RADIATION, NET RADIATION, ALBEDO|
LONG WAVE AND THERMAL
RADIATION, NET RADIATION, ALBEDO|
ET
ges at Far qe Re re re or ur ag Fe Parra,
Her Fa ec are ac ag A te & Fre eer ra fn Frat are fe, we E
lease arf ra a eh aa $
[arco fran quí & args $ are 500 wren wt us fra & era Per an gra wer à dz à
ce 8, shen frre xt ena ew re BH
Ira Pra & our, ware odes: eu à tr Fair a 400 aft 700 CEH Ata ae à, qua
eater a a arar, fre ge Faves 4196 & re Bi ware and eo a wha Pro & Mer,
[ataco ara aes 8:
1. survie (400-490 ©
wu (490-560 wre)
17
ges at Far qe Re re re or ur ag Fe Parra,
Her Fa ec are ac ag A te & Fre eer ra fn Frat are fe, we E
lease arf ra a eh aa $
[arco fran quí & args $ are 500 wren wt us fra & era Per an gra wer à dz à
ce 8, shen frre xt ena ew re BH
Ira Pra & our, ware odes: eu à tr Fair a 400 aft 700 CEH Ata ae à, qua
eater a a arar, fre ge Faves 4196 & re Bi ware and eo a wha Pro & Mer,
[ataco ara aes 8:
1. survie (400-490 ©
wu (490-560 wre)
17
ET
3. sien (560-590 vx)
la. arért=ara (590-700 vaux)
rer re re, Fa at sf ar we ew attache fh aw Ra art
[ira sien, sacs, sai fr rere su var sar $
et xe ara cera arm fhe Peer we sme wae er a re fre, see a
cfr: ae Paco ator & fs Pet are armen te A Bi
Sx
3. sien (560-590 vx)
la. arért=ara (590-700 vaux)
rer re re, Fa at sf ar we ew attache fh aw Ra art
[ira sien, sacs, sai fr rere su var sar $
et xe ara cera arm fhe Peer we sme wae er a re fre, see a
cfr: ae Paco ator & fs Pet are armen te A Bi
Sx
Estas DEWAN
Lens ol
Lens ol
E PROFILE OF TEMPERATURE, ENERGY BALANCE ON]
ere
AUT
m
ST
TEMPERATURE INVERSION]
[A temperature in
sion is layer in the atmosphere in which air temperature increases with height.
[An inversion is present in the lower part ofa cap. Temperature Inversion is also known as thermal
AUT
m
ST
TEMPERATURE INVERSION]
[A temperature in
sion is layer in the atmosphere in which air temperature increases with height.
[An inversion is present in the lower part ofa cap. Temperature Inversion is also known as thermal
[The cap is a layer of relatively warm air aloft (above the inversion). Air parcels rising into this layer
[become cooler than the surrounding environment, which inhibits their ability to ascend,
ere ge arg es rea ea TT er hw aN Fd À go |
‘The reversal ofthe normal behaviour of temperature in the troposphere is known as
temperature inversion.
The troposphere is the lowest region ofthe atmosphere, extending from the earth surface
10 a height of about 6-10 km.
Inversions play an important role in determining visibility, precipitation, and cloud forms.
There will be limited diffusion of air pollutants, smoke and dust
During the day time, the radiation from the sun heats up the land surface and the air gets
mainly heated up when this air gets in touch with the heated land surface.
Diurnal variations in air temperature also affect inversion,
Convective clouds cannot grow high enough to produce showers in regions where a
pronounced low-level inversion is present. This happens due to the accumulation of smoke
and dust particles.
Even in the absence of clouds, visibility may be greatly reduced below the inversion.
Fog is frequently present there, asthe air near the base of an inversion tends to be cool.
‘Through convection and conduction, the heat from the ground gets transferred to the ai.
‘The magnitude of ground inversions is greatly affected by the topography.
‘Temperature inversion is quite common, but it happens for a short duration.
An ideal situation for inversion is stil air, long winter nights with clear skies
Itisa normal ar areas,
aa a
er apta rw fee, ol e em 6-10 Pt Sr re a go
gee, at area wt fer gr fe Po
ang gest qu aft rarer er om
Perdon, Feo fe en eg Ae nl A
ré à sr
re A fe ao fr
ee acer gr ro ge qe go
fh tar gio ro rn a
area aaah, gsr rage
[become cooler than the surrounding environment, which inhibits their ability to ascend,
ere ge arg es rea ea TT er hw aN Fd À go |
‘The reversal ofthe normal behaviour of temperature in the troposphere is known as
temperature inversion.
The troposphere is the lowest region ofthe atmosphere, extending from the earth surface
10 a height of about 6-10 km.
Inversions play an important role in determining visibility, precipitation, and cloud forms.
There will be limited diffusion of air pollutants, smoke and dust
During the day time, the radiation from the sun heats up the land surface and the air gets
mainly heated up when this air gets in touch with the heated land surface.
Diurnal variations in air temperature also affect inversion,
Convective clouds cannot grow high enough to produce showers in regions where a
pronounced low-level inversion is present. This happens due to the accumulation of smoke
and dust particles.
Even in the absence of clouds, visibility may be greatly reduced below the inversion.
Fog is frequently present there, asthe air near the base of an inversion tends to be cool.
‘Through convection and conduction, the heat from the ground gets transferred to the ai.
‘The magnitude of ground inversions is greatly affected by the topography.
‘Temperature inversion is quite common, but it happens for a short duration.
An ideal situation for inversion is stil air, long winter nights with clear skies
Itisa normal ar areas,
aa a
er apta rw fee, ol e em 6-10 Pt Sr re a go
gee, at area wt fer gr fe Po
ang gest qu aft rarer er om
Perdon, Feo fe en eg Ae nl A
ré à sr
re A fe ao fr
ee acer gr ro ge qe go
fh tar gio ro rn a
area aaah, gsr rage
aes ag a À, fa A A we
aes ae ret ee def a ea or
ser à ee fm ge sea
Th positive when the temperature decreases with elevation, 2
Ihe temperature is constant with elevation, and negative when the temperature increases wit
elevation (temperature inversion). The lapse rate of non rising air—commonlyt
referred to as the normal, or environmental, lapse rate—is highly variable, be
jy radiation, convection, and condensation; it ave
ropospher
RER RR SEN a SME wT TT TT
eae ere ar ai rar axe Se QT IH de
serene faye à
Ar er A amet ar hn tres, Ar fern
ear he er a i ae erst ce re se ae eet Pr fi Br
ae are rte pen ae He wn ar q a te ra men Ps
Id Par se trae he a
21
aes ae ret ee def a ea or
ser à ee fm ge sea
Th positive when the temperature decreases with elevation, 2
Ihe temperature is constant with elevation, and negative when the temperature increases wit
elevation (temperature inversion). The lapse rate of non rising air—commonlyt
referred to as the normal, or environmental, lapse rate—is highly variable, be
jy radiation, convection, and condensation; it ave
ropospher
RER RR SEN a SME wT TT TT
eae ere ar ai rar axe Se QT IH de
serene faye à
Ar er A amet ar hn tres, Ar fern
ear he er a i ae erst ce re se ae eet Pr fi Br
ae are rte pen ae He wn ar q a te ra men Ps
Id Par se trae he a
21
Emmen
tes er an A spe ere, Jl era a a TO an ft rs
ree ae Fe ha a em, eg, am
ek er ais fase ge tis at m Fi, sr te et, ae
> tac gia ewe er A ere go,
Anima 14 ae age ee 16 7 a ra ae er dm
eee ee A tee oe er Fai ae ae, ih, oem te fora $
sei ai em an eth i ae fe, le
ven ra saree af a eh ere te ath ace bee
fear 6.5 ea Pet A tte exer eA a ere aH aa GET
site Pion ot reste Fah, te ae er A
ra 75 fr i afte ga A ae a ew a AT ee
veer seh ate ea ar ae 10, hae a ra gE A aE
cra
tes er an A spe ere, Jl era a a TO an ft rs
ree ae Fe ha a em, eg, am
ek er ais fase ge tis at m Fi, sr te et, ae
> tac gia ewe er A ere go,
Anima 14 ae age ee 16 7 a ra ae er dm
eee ee A tee oe er Fai ae ae, ih, oem te fora $
sei ai em an eth i ae fe, le
ven ra saree af a eh ere te ath ace bee
fear 6.5 ea Pet A tte exer eA a ere aH aa GET
site Pion ot reste Fah, te ae er A
ra 75 fr i afte ga A ae a ew a AT ee
veer seh ate ea ar ae 10, hae a ra gE A aE
cra
eee wr et rd mo Ft Set we EE 400 Ft
eft fb srt gins or ee aren eh eH |
‘ae Fete eee rae Fag aa te 1000 sh era ar
saree a fa fi ra arf, |
Sears gt ate deat
TES
at
are reste pi er te reas te ren eet ret see 50 600
Ft ee ew ra a ze da Zah
eft fb srt gins or ee aren eh eH |
‘ae Fete eee rae Fag aa te 1000 sh era ar
saree a fa fi ra arf, |
Sears gt ate deat
TES
at
are reste pi er te reas te ren eet ret see 50 600
Ft ee ew ra a ze da Zah
Emmen
he sg ere ee a fe a Ree te ae Am 296 fra re rx
Io genen ar am aa are ara ere, le, eh arte am, hh
em
mat
¿li Po
free Yah soar era Frc tr ete ora ne
he sg ere ee a fe a Ree te ae Am 296 fra re rx
Io genen ar am aa are ara ere, le, eh arte am, hh
em
mat
¿li Po
free Yah soar era Frc tr ete ora ne
|
El
JONCEPT Ol
El
JONCEPT Ol
Ste, arg seh ar eA ae Ra HAE OS ERT ar AH
von am a5 ag ee, a ree ear et
rg
id ER SEE E SE
A deci dar me Rohr
eres rer ad hr za À, er a a
jan ra er eh, Ts a TAL
ra aah re en
von am a5 ag ee, a ree ear et
rg
id ER SEE E SE
A deci dar me Rohr
eres rer ad hr za À, er a a
jan ra er eh, Ts a TAL
ra aah re en
Emmen
le ta a a RAE AY eT A TY ST PRT MT, MEE
ex ea er ah a ar nie he fo, ses eae ae oT
wea her tr eB wah ee he a BF fr
arr gm, at Pt A cf crm
res br a rere eh ea eh Pt a to
apr car, ae, zara aren
condensation takes p
le ta a a RAE AY eT A TY ST PRT MT, MEE
ex ea er ah a ar nie he fo, ses eae ae oT
wea her tr eB wah ee he a BF fr
arr gm, at Pt A cf crm
res br a rere eh ea eh Pt a to
apr car, ae, zara aren
condensation takes p
sax oca]
> arar te ee fe aa rl, x aT
Ma Bexar ae Be rch aia a à
a sey, de, Seer ren ae Pa a
sie art
[processes of Cooling for Producing Condensation
ON
> art ar y ar, em ref rar
are er ar Fa ra ee a Re fe a ee a ar Pr
arb ef ae ar are
> Refer fier fe, rer a 8 ee a roe gr à
are Sh he ea Bee Fe à, are me a er a à, a
eres ses aa ne he ré er à a arena Ra a
ir, ee er A Pa, We Por ge af TE
A re fe er re io te
ish
> arar te ee fe aa rl, x aT
Ma Bexar ae Be rch aia a à
a sey, de, Seer ren ae Pa a
sie art
[processes of Cooling for Producing Condensation
ON
> art ar y ar, em ref rar
are er ar Fa ra ee a Re fe a ee a ar Pr
arb ef ae ar are
> Refer fier fe, rer a 8 ee a roe gr à
are Sh he ea Bee Fe à, are me a er a à, a
eres ses aa ne he ré er à a arena Ra a
ir, ee er A Pa, We Por ge af TE
A re fe er re io te
ish
ar eo Pr Pe ht gr oa aa a Va
io fag a, Pts nr Fg a cb, gear
ots et la, Ser i ec um a
ae aoe Por À, rer qe wah, be eT, eT
te fo a arr eto
> aaa her ae ee ee ear fa wee ahh oh a oA Se
Aa a ats UH aa seb a a ee rea fea eve Tae, i ea, eT
ses aia hfe ar fe, ares Pig fe
Game an F Rx een far ro ar efi fre a am ar en, sg
eH, ge ae gr Ta AT
io fag a, Pts nr Fg a cb, gear
ots et la, Ser i ec um a
ae aoe Por À, rer qe wah, be eT, eT
te fo a arr eto
> aaa her ae ee ee ear fa wee ahh oh a oA Se
Aa a ats UH aa seb a a ee rea fea eve Tae, i ea, eT
ses aia hfe ar fe, ares Pig fe
Game an F Rx een far ro ar efi fre a am ar en, sg
eH, ge ae gr Ta AT
bus
> a beh rl cam mh ee fe fg (Of A Ha a es ye ig ear Te
“fae ats a aan mr
Pear id, Ree ea arene fi fig ear a ot Hae
> a beh rl cam mh ee fe fg (Of A Ha a es ye ig ear Te
“fae ats a aan mr
Pear id, Ree ea arene fi fig ear a ot Hae
Emmen
nen Fra ea rah arr Pi er Be ata a aa Fr |
ed af er ar ei eh mar aa et ah qu fre
euer, eer a are a een ho en rt er re a a
ets ea aoe re oar Fa re rea rae wa fe
eee ree, gf arg ea rk wr era re eg Tex ET
Reece no hi eg a ai wh er, ee at Ree gr, Pd
seh hoe gra a sg org ee a aa eT e
ara eR rE ag ear ee wT, ae, a re
ra eg ti arg a ree emir enc 0 CA a
sae ar ee eh
SE ST fon ao a gr a
ta eh i Per ra eke ee ge 2 À 3
eee aoa sae gaa ag na fr SO afer ae a CT
5 seme Bra, ra rm 70 sf
38
nen Fra ea rah arr Pi er Be ata a aa Fr |
ed af er ar ei eh mar aa et ah qu fre
euer, eer a are a een ho en rt er re a a
ets ea aoe re oar Fa re rea rae wa fe
eee ree, gf arg ea rk wr era re eg Tex ET
Reece no hi eg a ai wh er, ee at Ree gr, Pd
seh hoe gra a sg org ee a aa eT e
ara eR rE ag ear ee wT, ae, a re
ra eg ti arg a ree emir enc 0 CA a
sae ar ee eh
SE ST fon ao a gr a
ta eh i Per ra eke ee ge 2 À 3
eee aoa sae gaa ag na fr SO afer ae a CT
5 seme Bra, ra rm 70 sf
38
[rescirrano]
A LE
[Processor PRECIPITATION]
EL —
Éswow]
EP
| |
rar]
SNe RQ HF ST a aM HT WU TT NT ME AT UO TEEN TT TET PR
ite se ih ate tao gi ga era re
‘OUD FORMATION]
A LE
[Processor PRECIPITATION]
EL —
Éswow]
EP
| |
rar]
SNe RQ HF ST a aM HT WU TT NT ME AT UO TEEN TT TET PR
ite se ih ate tao gi ga era re
‘OUD FORMATION]
re, arc, ht Ter a ea NC ru a 1
TCE ATCA ESN TE O RT PTB tT A, maT BA FT
fe gere
eee ree Ae ooh TER, a re ee een
ae a zur ct
TCE ATCA ESN TE O RT PTB tT A, maT BA FT
fe gere
eee ree Ae ooh TER, a re ee een
ae a zur ct
vere eae gts Tce eT A AT AT YT TA ais
a, sr re a
ferret arene ann we à qu mg re rr
SN NCE IN
ARDS- DROUGHT, F ODS, FROST.
a, sr re a
ferret arene ann we à qu mg re rr
SN NCE IN
ARDS- DROUGHT, F ODS, FROST.
I, fa ef ar ef arm a, A ae Ma ag a va
er mag ar fy are fai AZ re, ar ra an Gi 6,
cae rebar she ae ra AR ache rc ec ar ae ah a ag ee, dnd |
aaa an an aT a Pr eT ee wa eT at
MECHANISM OF MONSOO!
er mag ar fy are fai AZ re, ar ra an Gi 6,
cae rebar she ae ra AR ache rc ec ar ae ah a ag ee, dnd |
aaa an an aT a Pr eT ee wa eT at
MECHANISM OF MONSOO!
eet ce ep nn rh a ae fg re A
nr ere a 6 ts gr 5 fr cr
a eRe aa ge oT
[roo]
ra ett a AE RS ATTN SES À, ar
tee FB, ca e fr À gt He
rr, fra A a Kt aT act a TH
rec ih rege et or gre à, ree et
"AL CYCLONE]
nr ere a 6 ts gr 5 fr cr
a eRe aa ge oT
[roo]
ra ett a AE RS ATTN SES À, ar
tee FB, ca e fr À gt He
rr, fra A a Kt aT act a TH
rec ih rege et or gre à, ree et
"AL CYCLONE]
ee ETAT CST BT
are aed a
are rer, mt a 219 em rer eee
ea 20 rs 150s a fr, 20 Fa (20 Heya itr re
cee À A À, E E
er ee xe a ex eer aaa eer a ae TT ae
arg Free er a eer er a ag org da
ame
OLD
se grace ite One Bo rm Pro, she et
ra Pt
ND WEATHER RELATIONS; MODIFICATION OF CROP
MATE, CLIMATIC NORMAL FOR CROP AND LIVESTOCK PRODUCTION
are aed a
are rer, mt a 219 em rer eee
ea 20 rs 150s a fr, 20 Fa (20 Heya itr re
cee À A À, E E
er ee xe a ex eer aaa eer a ae TT ae
arg Free er a eer er a ag org da
ame
OLD
se grace ite One Bo rm Pro, she et
ra Pt
ND WEATHER RELATIONS; MODIFICATION OF CROP
MATE, CLIMATIC NORMAL FOR CROP AND LIVESTOCK PRODUCTION
Emmen
eat as ro ae ar rch ar a ea q hr ru Fe
re et aT, ae A a ti see ita da seen TA Y
are a brs sn am 15 Fe A a eB abet me ra A A
sre ie ea hc saat eal ar rm 10-14 we ee ras
rae er dd eT War Meo nd, a Te rm
a tra SCHROTT re ee, 300 et So cr
a e fe a
re re re a sr te eer mg gr
rer fr ar or sa aT à
re 200 Ft teres re re À fr ee rm 100 Bt
are e
ge ere re ares R
10.35 fash een son arr te .10 sen Sea re mm
2500-3000 wf ar fr ere ea go ah eae a
eat as ro ae ar rch ar a ea q hr ru Fe
re et aT, ae A a ti see ita da seen TA Y
are a brs sn am 15 Fe A a eB abet me ra A A
sre ie ea hc saat eal ar rm 10-14 we ee ras
rae er dd eT War Meo nd, a Te rm
a tra SCHROTT re ee, 300 et So cr
a e fe a
re re re a sr te eer mg gr
rer fr ar or sa aT à
re 200 Ft teres re re À fr ee rm 100 Bt
are e
ge ere re ares R
10.35 fash een son arr te .10 sen Sea re mm
2500-3000 wf ar fr ere ea go ah eae a
is fe ame 1 Pa fa a rer 34
tr 19 Fe a see sh re 21 lah Me ae rer Ts,
equ sre rary Re ee eet MT a LA Te RT ae EE A
a, MR STE, aR ZU ro qu eshte DI
eae ft, eit re re mf
tr 19 Fe a see sh re 21 lah Me ae rer Ts,
equ sre rary Re ee eet MT a LA Te RT ae EE A
a, MR STE, aR ZU ro qu eshte DI
eae ft, eit re re mf
Emmen
Be a a m a a m m re me re
a ee arg ea Ham a a Pa, rm A et A
am, un rk mr a ar are cra,
ete, ua te ee ee age nd Far m er,
ta ac re a ga ce cr af hr
fife or a Pme 5
a oo om TT
Sr main A re
ffs, srr a pre io ar tn pa, a fan, Fe,
do ere
qi AA A At
rare hi ma om ro me tir à
ee et ate a or og Frame nd
A mm A m re
rg mer eA, TET rm
si
Be a a m a a m m re me re
a ee arg ea Ham a a Pa, rm A et A
am, un rk mr a ar are cra,
ete, ua te ee ee age nd Far m er,
ta ac re a ga ce cr af hr
fife or a Pme 5
a oo om TT
Sr main A re
ffs, srr a pre io ar tn pa, a fan, Fe,
do ere
qi AA A At
rare hi ma om ro me tir à
ee et ate a or og Frame nd
A mm A m re
rg mer eA, TET rm
si
Estas DEWAN
yd ia 1 |
husbandry
yd ia 1 |
husbandry
TY, GLOBAL WARMING, CAUS
sre arte e oa Bo ate mart
er wa Pr a ger ae HE CUT aA aN
st sta sa ti, et 2 me rt wert A a
ht 2 ee ee re ea ara a
ian: ii à er ea ec ace te
a sh er re air gs at eae an ay, 2
es rash fh ari a a Baa Te Aa A TT,
sre a i rn rs ea eh Ep Fo
hen ars, eA o ar
er wa Pr a ger ae HE CUT aA aN
st sta sa ti, et 2 me rt wert A a
ht 2 ee ee re ea ara a
ian: ii à er ea ec ace te
a sh er re air gs at eae an ay, 2
es rash fh ari a a Baa Te Aa A TT,
sre a i rn rs ea eh Ep Fo
hen ars, eA o ar
IsHAN DEWAN
herzen er are et a cf a ara aT e eses Bgl COD SEA
cre ze rr or en aer ge ea ar 9396 as e er fe, fr FOR gare
aa hese Aue ara a AP, ee for aos gg fresh A
area Fc
est og ep Fr a Por are PTI 3996 SAT fr ER Be Ta
ra ar fi ai hr are ar A na a fe re fr re dr
Er re ro ri er À, a fr ft
atra
ere ae fed E
re) da er ge er o, lc rer R
re, fer re fre, rt eT
herzen er are et a cf a ara aT e eses Bgl COD SEA
cre ze rr or en aer ge ea ar 9396 as e er fe, fr FOR gare
aa hese Aue ara a AP, ee for aos gg fresh A
area Fc
est og ep Fr a Por are PTI 3996 SAT fr ER Be Ta
ra ar fi ai hr are ar A na a fe re fr re dr
Er re ro ri er À, a fr ft
atra
ere ae fed E
re) da er ge er o, lc rer R
re, fer re fre, rt eT
esi af ee tg Oa ee =
cz ese, i age re es ra A m Re
Fas sad ore, ere AN a a CH ara EH TANT aL) TC eT me aT RL
are ea be ma aaa
cz ese, i age re es ra A m Re
Fas sad ore, ere AN a a CH ara EH TANT aL) TC eT me aT RL
are ea be ma aaa
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