climatology vernacular ppt

8/18/2019 Climatology Vernacular Ppt

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Role ofCLIMATE inVernaculararchitecture

SUBMITTED BY:

SHIVAM THUKRAL

SHUBHI KALRA

SHUBHI VERMA

(B.ARH ! SEMERSTER"

NorthernMountainous

Areas.

SUBMITTED T#:

AR.SAHI$ SA%ARAR.EKTA BALI


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VERNACULARARCHITECTURE

VERNACULAR ARCHITECTURE i& a cate'or of architecture

)a&e* on local needs + construction materials an* refecting

local traditions.It ten*& to e,ol,e o,er to re-ect the environmental cultural+

technological economic+ an* historical conte"t in /hich it

e0i&t&.

The ter1 ,ernacular i& *eri,e* fro1 the Latin /or* vernaculus +

1eanin' native.

In architecture+ it refer& to that t e of architecture /hich i&


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M%UNTAIN&

'C%L( CLIMATE)

It i& col* )ecau&e of it& hi'h altitu*e&. Su11erte12erature ran'e )et/een 34 *e'ree& el&iu& to 35*e'ree& el&iu& /hile /inter are fro1 63 *e'ree&el&iu& to 65 *e'ree& el&iu&. The a,era'e2reci2itation i& !4 c1 a ear.


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&ome im#ortant*uestions +

The main differences in climate of mountains are temperature and moisture.

What is the climate on mountains?The temperature on mountains becomes colder the higher the altitude gets.Mountains tend to have much wetter climates than the surrounding flat land.

What is the weather on mountains?Mountain weather conditions can change dramatically from one hour to the next. For example, in just a few minutes a thunder storm can roll in when the sky wasperfectly clear, and in just a few hours the temperatures can drop from extremelyhot temperatures to temperatures that are below freezing.

Why do mountains receive more rainfall?

They receive more rainfall than low lying areas because the temperature on topof mountains is lower than the temperature at sea level.inds carry moist air over the land. hen air reaches the mountain, it risesbecause the mountains are in the way. !s the air rises, it cools, and because coolair can carry less moisture than warm air, there is usually precipitation "rain#.


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Why do we sometimes see snow on the top of mountains? $ou can often see snow on the top of mountains all year round,

because the temperature at the top of mountains is lower than at thebottom. The higher the place is above sea level the colder it will be.%ome mountains reach higher than the clouds. !t this altitude theextreme cold and high winds cause blizzards.

Why does the temperature become colder the higher up aMountain?&enerally the climate on mountains get progressively colder withincreased altitude "the higher up you go#. This happens because asaltitude increases, air becomes thinner and is less able to absorband retain heat. The cooler the temperature the less evaporationthere is, meaning that there is more moisture in the air.!ir pressure decreases with altitude. !s a result of the reduced airpressure, rising air expands and cools.


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IM7#RTA$E #8 LIMATE One of the most significant influences on vernacular

architecture is the macro climate of the area in which the

building is constructed. Buildings in cold climates invariably

have high thermal mass or significant amounts of insulation.They are usually sealed in order to prevent heat loss, and

openings such as windows tend to be small or non-existent..

Buildings for a continental climate must be able to cope with

significant variations in temperature, and may even be altered

by their occupants according to the seasons. Buildings take different forms depending on precipitation

levels in the region – leading to dwellings on stilts in many

regions with freuent flooding or rainy monsoon seasons. !lat

roofs are rare in areas with high levels of precipitation.


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RE&I(ENTIAL ,UIL(IN- Hou&e i& a &2ace inha)ite* ) 2eo2le an* their &torie&.

The character of a Hi1achal ,ernacular+ the &tor unit i& )a&icall a cu)oi*

. The &1alle&t hou&e& are t/o or three laer& &tac9e* in t/o or three le,el&

('roun*+ r&t an* &econ* -oor"

The &i;e of the hou&e increa&e& ) 2lacin' cu)oi*& &i*e ) &i*e an* thene0ten*in' u2 three le,el&.

Each hou&e i& *eter1ine* ) ca2acit. The ca2acit i& not onl the &i;e of

the fa1il )ut al&o the fa1il


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Sin'le cu)oi*,ariant

Dou)le cu)oi*,ariant

Tri2le cu)oi*,ariant


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MATERIALS USED IN CONSTRUCTION


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LITERATUREASE STUDY


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Eects o/ climate on the 0uilding

/ormats in cold mountainous climate The for1at of the )uil*in' ha& an i12ortant e>ect on &o 1anfactor& &uch a& a*?u&tin' the )uil*in' con*ition an* cli1ate a& /ella& 1o*eratin' the tran&1i&&ion of the critical out&i*e /eathercon*ition& to the )uil*in'&. Therefore o2en for1at )uil*in'& or thefor1at& in /hich the &outh6north fronta'e i& len'thier than the/e&t6ea&t fronta'e are not &uita)le. An* it i& )etter for the )uil*in'to )e 1ore co12re&&e* in 1ountainou& col* cli1ate an* their 2lan&houl* )e in four&@uare &ha2e. That /a the can re&i&t the col*.

The cu)ical t/o &tor )uil*in'& are the )e&t 9in* for controllin' theinternal heat in the )uil*in' *urin' /inter.

Direction of )uil*in' con&truction in 1ountainou& col* cli1ate&

Since 'ettin' the 1o&t &unli'ht i& nece&&ar in col* 1ountainou&cli1ate+ therefore )uil*in'& 1u&t locate to/ar* a *irection &o thatthe can recei,e the hi'he&t &un ra*iation. Thu& the 1ain faca*eof )uil*in' 1u&t )e 2lace* to/ar* the &outh in or*er to create the)e&t heat con*ition in&i*e the )uil*in'. So the northern faa*e of)uil*in'& *ecrea&e& to the 1ini1u1 &urface.


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LIVE ASESTUDY


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L#ATI#$ THE H#USE IS L#ATED I$ ITY #8 LAKES $AI$ITAL<

SITUATED BETCEE$ THE BEAUTI8UL VALLEYS #8UTTARAKHA$D.

ITY IS CELL 7#7ULATED AS IT IS A T#URIST 7LAE S#VARI#US #TTA%ES+ RES#RTS+RESTAURE$TS+ H#TELSCERE THEIR A$D THE MATERIAL USED I$ THEM CERE

ST#$ES+MUD+C##D+ BRIKS. M#ST #8 THE H#USES SITUATED AT THE B#TT#M SIDE #8

THE HILLS CERE EAST A$D $#RTH 8AI$% A$D S#MEH#USES CHIH CERE AT THE T#7 CERE S#UTH 8AI$%.

%ABLED R##8 CAS #MM#$ THEIR CITH THE#MBI$ATI#$ #8 #THER SL#7Y R##8S LIKE HI7 R##8.

D#RMERS CERE ALS# VERY #MM#$ #$ THE $#RTH SIDE.

USE #8 ARHES IS VERY #MM#$ I$ MI$ISTRIES A$DADMI$ISTRATIVE BL#KS #8 THE ITY.

$# SU$ BRAKERS CERE USED I$ A$Y BUILDI$%.


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CLIMATE AN( TEM1ERATURE

$ainital ha& te12erate &u11er&+ 1a0i1u1te12erature F (53 F8"G 1ini1u1 te12erature F ( F8" .

In /inter+ $ainital recei,e& &no/fall )et/een

Dece1)er an* 8e)ruar /ith the te12erature&,arin' )et/een a 1a0i1u1 of 3 F (J F8" an*a 1ini1u1 of ! F ( F8".


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SUMMERS

CI$TER

S


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Ma0i1u1 o2enin'& on the &outh/e&t &i*e /a& 'i,en &o that

1a0i1u1 heat coul* tra2 in&i*ethe hou&e.


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S1all /in*o/& at thenorth &i*e at the to2hill&.

#2enin' /a& )loc9e*+

1a )e )ecau&e there&houl* )e le&&o2enin'& &o that there1a )e 1ore ther1alheat in&i*e the hou&e.


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7re&er,ation of,ernacular

1aterial& for futureu&e

Ru))le &tone 1a&onr

0e* /ith 1u* 1ortar.$o o2enin'& e0ce2t the*oor in the north &i*e.


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#$LUSI#$


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DESI%$ RITERIA


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R##8I$% TEH$INUE


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THA$K Y#U

climatology vernacular ppt

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