SlideShare a Scribd company logo
1 of 16
Download to read offline
Aaqib Iqbal
Deccan School of Planning & Architecture
CLIMATOLOGY PROJECT ON
TROPICAL CLIMATE
• Climate is a measure of the average pattern of variation
in temperature, humidity, atmospheric pressure, wind, precipitation,
atmospheric particle count and other meteorological variables in a given
region over long periods of time. Climate is different from weather, in that
weather only describes the short-term conditions of these variables in a
given region
• A region's climate is generated by the climate system, which has five
components: atmosphere, hydrosphere,cryosphere, lithosphere,
and biosphere.
• The climate of a location is affected by its latitude, terrain, and altitude, as
well as nearby water bodies and their currents. Climates can
be classified according to the average and the typical ranges of different
variables, most commonly temperature and precipitation.
CLIMATE
WORLDWIDE CLIMATE CLASSIFICATIONS
• A tropical climate is a climate in
the tropical region. In the Köppen
climate classification it is a non-
arid climate in which all twelve
months have mean temperatures of
at least 18 °C (64 °F).
• Tropical temperature remains
relatively constant throughout the
year and seasonal variations are
dominated by precipitation.
• Tropical Climates are those climates
where heat is dominant problem
where the greater part of year
buildings serve to keep cool for
occupants room rather than warm.
TROPICAL CLIMATE
• The Basis of classification is given by 3 atmospheric factors which
dominantly influence human comfort – air , temperate &
humidity
• The Tropical regions of earth are divided into 3 major climatic
zones & three sub groups
Warm Humid equatorial climate
Hot Dry Desert (or) semi desert climate
Composite or monsoon climate
CLASSIFICATION
• These climates are found in belt near equator extending to about
15ºN & s. Logos,Dar-es-Salam,Colombo,Singapore etc are
examples of this climate. There is very less seasonal variation
throughout the year .Periods of more or less rain & occurrence of
gusty winds & electric storms
Air Temperature – Shades reaches a max during the day of
between 27 & 32ºc but occasionally it may exceed. The mean
minimum varies from 21º & 27ºc
Humidity – Rh(Relative humidity remains high at about 75 % for
most of the time but it may vary from 55 to almost 100 % . Vapor
pressure is steady from 2500 to 3000 N/m2
WARM HUMID CLIMATE
Locations of warm humid climates
 Precipitation – High through out the year. Annual rainfall can vary
from2000 to 5000 mm & may exceed 500 mm .
Sky Condition – Fairly cloudy throughout the year . Cloud cover
varies between 60 & 90 % .Skies are usually bright .
Solar Radiation – is partly reflected & partly scattered by cloud
blanket but strong radiation can cause painful sky glare
Wind Velocities – are typically low, calm periods are forewent but
strong winds can occur during rainfall
Vegetation : Grown quickly due to frequent rains & high temperature
& it is difficult to control the red or brown laterite soils are generally
poor for agriculture .
Special Characteristics – High humidity accelerates mould & algal
growth rusting & rotting .Organic buildings materials tend to decay
rapidly Mosquitoes and other insects abound .The thunder storms are
accompanied by frequent air – to air electrical discharges
These climates occur in two belts at latitudes between
approximately 15 & 30ºnorth & south of the equator . Example's :
Assuan Baghdad,Alice springs & phoenix
Two marked seasons occur :a hot & a somewhat cooler period
Air Temperature : DBT in shade rises quickly after sunrise to day
time mean maximum temperature ranged from 27 to 32ºc . Night
time mean minima between 24 & 30ºc in hot season & between
10 & 18º in cool season .The diurnal range is very great 17 to 22º
Humidity : RH varies from 10 to 55 % as wet depression is large
(rapid evaporation) .Vapor pressure is normally between 750 &
1500 N /m2
HOT DRY DESERT CLIMATE
LOCATIONS OF HOT DRY DESERT CLIMATE
Precipitation : Slight & variable throughout the year, from 50 to 155
mm per annum ,Flash storms may occur over limited areas but
some regions may not have rains for several years .
Sky Conditions : Normally Clear .Clouds are few due to low
humidity of the air . The sky is usually dark blue , with a luminance of
700 to 2500 cd/m2 & further darkened dust or sand storms may
occur
Solar Radiation : Direct & strong during the day , but the absence
of cloud permits easy release of hear stored during day time
Winds : are usually local .Heating of air over hot ground cause a
temperature inversion
Vegetation : is sparse & difficult to maintain humidity . The soil is
usually dusty & very dry. Soils dries quickly after rain & would
generally be fertile if irrigated
• These climates usually occur in large land masses near tropics of
cancer & Capricorn which are sufficiently far from equator to
experience seasonal changes in solar radiation & wind direction
• Examples : Lahore ,Mandalay, New Delhi
• Two seasons occur normally .Approximately 2/3rds of the year is hot
dry & other third is warm humid. Localities further north & south often
have a third season but described as cool dry
Air temperature : in shade as follows
COMPOSITE OR MONSOON CLIMATE
Seasons Hot Dry Warm Humid Cool Dry
Day time 32 -43ºc 27-32ºc Upton 27ºc
Night time 21-27ºc 24-27ºc 4-10ºc
Diurnal mean range 11-22ºc 3-6 11-22ºc
LOCATIONS OF COMPOSITE OR MONSOON CLIMATE
 Humidity i.e. RH : Is low throughout the dry periods at 20 to 55 % with a
vapor pressure of 1300 to 1600 N/m2.Durin wet period it rises to 55 to
95 %
Precipitation : Monsoon rains are intense & continued for a long time
occasionally 25 to 38 mm can fall in an hour. Annual rainfall varies
from 500 to 1300 mm with 200 to 250 mm wettest month. There Is little
rain during dry seasons
Sky conditions :Markedly vary with the seasons .The sky is heavily
overcast & dull during monsoons & clear with dark blue color in dry
seasons
Solar Radiation : Alternated between conditions found in warm humid
& hot dry desert climates
Winds : are hot & dusty during dry period .Monsoon winds are fairly
strong & steady
• Vegetation : Hot dry region has brown & red barren
ground which changes rapidly with the rain .Plants
grow quickly. There is a risk of soil erosion during
monsoon
• Special Characteristics : Seasonal changes in relative
humidity cause rapid weakening of building materials
.Dust & Sand storms may occur
THANK YOU
Aaqib Iqbal| 13131AA001 |THIRD SEM

More Related Content

What's hot (20)

introduce Climatology sem 02 b-arch
introduce Climatology sem 02 b-archintroduce Climatology sem 02 b-arch
introduce Climatology sem 02 b-arch
 
Climatology Arch 302
Climatology Arch 302Climatology Arch 302
Climatology Arch 302
 
climatic zones in india
 climatic zones in india climatic zones in india
climatic zones in india
 
Climatology
ClimatologyClimatology
Climatology
 
Climate
ClimateClimate
Climate
 
Macroclimate microclimate
Macroclimate microclimateMacroclimate microclimate
Macroclimate microclimate
 
Koppen system
Koppen systemKoppen system
Koppen system
 
Lecture 2 climatic zones
Lecture 2   climatic zonesLecture 2   climatic zones
Lecture 2 climatic zones
 
Moderate climatic zone ppt
Moderate climatic zone pptModerate climatic zone ppt
Moderate climatic zone ppt
 
Macro and micro climate
Macro and micro climateMacro and micro climate
Macro and micro climate
 
COLD AND DRY
COLD AND DRYCOLD AND DRY
COLD AND DRY
 
cold climate architecture
cold climate architecturecold climate architecture
cold climate architecture
 
Hot and dry climate
Hot and dry climateHot and dry climate
Hot and dry climate
 
Climate responsive architecture (1)
Climate responsive architecture (1)Climate responsive architecture (1)
Climate responsive architecture (1)
 
Architecture in cold climate
Architecture in cold climateArchitecture in cold climate
Architecture in cold climate
 
Role of climate in architecture
Role of climate in architectureRole of climate in architecture
Role of climate in architecture
 
1. introduction to_climatology
1. introduction to_climatology1. introduction to_climatology
1. introduction to_climatology
 
Shelter for composite climate
Shelter for composite climateShelter for composite climate
Shelter for composite climate
 
Classification of Climate
Classification of ClimateClassification of Climate
Classification of Climate
 
Shelter for warm-humid climate
Shelter for warm-humid climateShelter for warm-humid climate
Shelter for warm-humid climate
 

Similar to Tropical Climate

World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...Azad Uddin (Sojib Ahmed)
 
world climate type n definition
world climate type n definitionworld climate type n definition
world climate type n definitionsalsa moyara
 
Introduction to Tropical Geomorphology
Introduction to Tropical GeomorphologyIntroduction to Tropical Geomorphology
Introduction to Tropical GeomorphologyLalit Thakare
 
G9 Science Q3- Week 4_5- Factors that affect Climate.ppt
G9 Science Q3- Week 4_5- Factors that affect Climate.pptG9 Science Q3- Week 4_5- Factors that affect Climate.ppt
G9 Science Q3- Week 4_5- Factors that affect Climate.pptMAESTRELLAMesa2
 
Climate,climate patterns and biomes
Climate,climate patterns and biomesClimate,climate patterns and biomes
Climate,climate patterns and biomesmanuelvasqs
 
Lec 1 climate & its components
Lec 1 climate & its componentsLec 1 climate & its components
Lec 1 climate & its componentsMahnoor Khawaja
 
Chapter 1 and 2 for students
Chapter 1 and 2 for studentsChapter 1 and 2 for students
Chapter 1 and 2 for studentsMissST
 
Climate
ClimateClimate
ClimateAC
 
Weather elements and factors
Weather elements and factorsWeather elements and factors
Weather elements and factorsShabana Yasmin
 
My presentation (weather)
My presentation (weather)My presentation (weather)
My presentation (weather)092698
 
mypresentationweather-150120021722-conversion-gate02.pdf
mypresentationweather-150120021722-conversion-gate02.pdfmypresentationweather-150120021722-conversion-gate02.pdf
mypresentationweather-150120021722-conversion-gate02.pdfssuserc902fb
 
Weather Systems Revision 2014
Weather Systems Revision 2014Weather Systems Revision 2014
Weather Systems Revision 2014douglasgreig
 

Similar to Tropical Climate (20)

Warm humid climate
Warm humid climateWarm humid climate
Warm humid climate
 
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
World Weather Types: Equatorial, Tropical, Desert, Mediterranean, Temperate a...
 
world climates finale
world climates finaleworld climates finale
world climates finale
 
CLIMATE.pptx
CLIMATE.pptxCLIMATE.pptx
CLIMATE.pptx
 
world climate type n definition
world climate type n definitionworld climate type n definition
world climate type n definition
 
Warm humid island climate
Warm humid island climateWarm humid island climate
Warm humid island climate
 
Introduction to Tropical Geomorphology
Introduction to Tropical GeomorphologyIntroduction to Tropical Geomorphology
Introduction to Tropical Geomorphology
 
G9 Science Q3- Week 4_5- Factors that affect Climate.ppt
G9 Science Q3- Week 4_5- Factors that affect Climate.pptG9 Science Q3- Week 4_5- Factors that affect Climate.ppt
G9 Science Q3- Week 4_5- Factors that affect Climate.ppt
 
Climate,climate patterns and biomes
Climate,climate patterns and biomesClimate,climate patterns and biomes
Climate,climate patterns and biomes
 
Lec 1 climate & its components
Lec 1 climate & its componentsLec 1 climate & its components
Lec 1 climate & its components
 
Chapter 1 and 2 for students
Chapter 1 and 2 for studentsChapter 1 and 2 for students
Chapter 1 and 2 for students
 
Climate
ClimateClimate
Climate
 
Weather elements and factors
Weather elements and factorsWeather elements and factors
Weather elements and factors
 
Climate
ClimateClimate
Climate
 
Climate of Bangladesh
Climate of BangladeshClimate of Bangladesh
Climate of Bangladesh
 
Climate
ClimateClimate
Climate
 
Climate
ClimateClimate
Climate
 
My presentation (weather)
My presentation (weather)My presentation (weather)
My presentation (weather)
 
mypresentationweather-150120021722-conversion-gate02.pdf
mypresentationweather-150120021722-conversion-gate02.pdfmypresentationweather-150120021722-conversion-gate02.pdf
mypresentationweather-150120021722-conversion-gate02.pdf
 
Weather Systems Revision 2014
Weather Systems Revision 2014Weather Systems Revision 2014
Weather Systems Revision 2014
 

More from Aaqib Iqbal

Working drawings
Working drawingsWorking drawings
Working drawingsAaqib Iqbal
 
Semester 4 history
Semester 4   historySemester 4   history
Semester 4 historyAaqib Iqbal
 
Green building(materials)
Green building(materials)Green building(materials)
Green building(materials)Aaqib Iqbal
 
Green building notes
Green building notesGreen building notes
Green building notesAaqib Iqbal
 
Rail nirman nilayam
Rail nirman nilayamRail nirman nilayam
Rail nirman nilayamAaqib Iqbal
 
Cii sohrabji godrej_green_business_centre
Cii sohrabji godrej_green_business_centreCii sohrabji godrej_green_business_centre
Cii sohrabji godrej_green_business_centreAaqib Iqbal
 
Structural systems assignment
Structural systems assignmentStructural systems assignment
Structural systems assignmentAaqib Iqbal
 
Advance structure system Notes 2
Advance structure system Notes 2Advance structure system Notes 2
Advance structure system Notes 2Aaqib Iqbal
 
Structural systems notes
Structural systems notesStructural systems notes
Structural systems notesAaqib Iqbal
 
Acm Space Frames
Acm Space FramesAcm Space Frames
Acm Space FramesAaqib Iqbal
 
Housing Data collection.pdf
Housing Data collection.pdfHousing Data collection.pdf
Housing Data collection.pdfAaqib Iqbal
 
Adv sercvices,structures,green building,housing elective qn papers
Adv sercvices,structures,green building,housing elective qn papersAdv sercvices,structures,green building,housing elective qn papers
Adv sercvices,structures,green building,housing elective qn papersAaqib Iqbal
 

More from Aaqib Iqbal (20)

Working drawings
Working drawingsWorking drawings
Working drawings
 
Semester 4 history
Semester 4   historySemester 4   history
Semester 4 history
 
Green building(materials)
Green building(materials)Green building(materials)
Green building(materials)
 
Green building notes
Green building notesGreen building notes
Green building notes
 
Rail nirman nilayam
Rail nirman nilayamRail nirman nilayam
Rail nirman nilayam
 
Cii sohrabji godrej_green_business_centre
Cii sohrabji godrej_green_business_centreCii sohrabji godrej_green_business_centre
Cii sohrabji godrej_green_business_centre
 
Structural systems assignment
Structural systems assignmentStructural systems assignment
Structural systems assignment
 
Advance structure system Notes 2
Advance structure system Notes 2Advance structure system Notes 2
Advance structure system Notes 2
 
Structural systems notes
Structural systems notesStructural systems notes
Structural systems notes
 
Acm drafting
Acm draftingAcm drafting
Acm drafting
 
Acm assignment
Acm assignmentAcm assignment
Acm assignment
 
Acm Unit v
Acm Unit vAcm Unit v
Acm Unit v
 
Acm Unit 3 2
Acm Unit 3 2Acm Unit 3 2
Acm Unit 3 2
 
Acm Unit 2
Acm Unit 2Acm Unit 2
Acm Unit 2
 
Acm Unit 1
Acm Unit 1Acm Unit 1
Acm Unit 1
 
Curtain walls
Curtain wallsCurtain walls
Curtain walls
 
Acm Space Frames
Acm Space FramesAcm Space Frames
Acm Space Frames
 
Housing Data collection.pdf
Housing Data collection.pdfHousing Data collection.pdf
Housing Data collection.pdf
 
Acm qn papers
Acm qn papersAcm qn papers
Acm qn papers
 
Adv sercvices,structures,green building,housing elective qn papers
Adv sercvices,structures,green building,housing elective qn papersAdv sercvices,structures,green building,housing elective qn papers
Adv sercvices,structures,green building,housing elective qn papers
 

Recently uploaded

PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdf
PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdfPHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdf
PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdfSumit Tiwari
 
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...Nguyen Thanh Tu Collection
 
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in Pharmacy
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in PharmacyASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in Pharmacy
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in PharmacySumit Tiwari
 
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...Nguyen Thanh Tu Collection
 
Metabolism , Metabolic Fate& disorders of cholesterol.pptx
Metabolism , Metabolic Fate& disorders of cholesterol.pptxMetabolism , Metabolic Fate& disorders of cholesterol.pptx
Metabolism , Metabolic Fate& disorders of cholesterol.pptxDr. Santhosh Kumar. N
 
Riti theory by Vamana Indian poetics.pptx
Riti theory by Vamana Indian poetics.pptxRiti theory by Vamana Indian poetics.pptx
Riti theory by Vamana Indian poetics.pptxDhatriParmar
 
EDD8524 The Future of Educational Leader
EDD8524 The Future of Educational LeaderEDD8524 The Future of Educational Leader
EDD8524 The Future of Educational LeaderDr. Bruce A. Johnson
 
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptx
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptxBBA 205 BUSINESS ENVIRONMENT UNIT I.pptx
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptxProf. Kanchan Kumari
 
Awards Presentation 2024 - March 12 2024
Awards Presentation 2024 - March 12 2024Awards Presentation 2024 - March 12 2024
Awards Presentation 2024 - March 12 2024bsellato
 
Dhavni Theory by Anandvardhana Indian Poetics
Dhavni Theory by Anandvardhana Indian PoeticsDhavni Theory by Anandvardhana Indian Poetics
Dhavni Theory by Anandvardhana Indian PoeticsDhatriParmar
 
3.14.24 The Selma March and the Voting Rights Act.pptx
3.14.24 The Selma March and the Voting Rights Act.pptx3.14.24 The Selma March and the Voting Rights Act.pptx
3.14.24 The Selma March and the Voting Rights Act.pptxmary850239
 
Quantitative research methodology and survey design
Quantitative research methodology and survey designQuantitative research methodology and survey design
Quantitative research methodology and survey designBalelaBoru
 
2024.03.16 How to write better quality materials for your learners ELTABB San...
2024.03.16 How to write better quality materials for your learners ELTABB San...2024.03.16 How to write better quality materials for your learners ELTABB San...
2024.03.16 How to write better quality materials for your learners ELTABB San...Sandy Millin
 
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdf
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdfArti Languages Pre Seed Send Ahead Pitchdeck 2024.pdf
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdfwill854175
 
The First National K12 TUG March 6 2024.pdf
The First National K12 TUG March 6 2024.pdfThe First National K12 TUG March 6 2024.pdf
The First National K12 TUG March 6 2024.pdfdogden2
 
LEAD6001 - Introduction to Advanced Stud
LEAD6001 - Introduction to Advanced StudLEAD6001 - Introduction to Advanced Stud
LEAD6001 - Introduction to Advanced StudDr. Bruce A. Johnson
 
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...Subham Panja
 
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.docdieu18
 

Recently uploaded (20)

PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdf
PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdfPHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdf
PHARMACOGNOSY CHAPTER NO 5 CARMINATIVES AND G.pdf
 
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...
BÀI TẬP BỔ TRỢ TIẾNG ANH 11 THEO ĐƠN VỊ BÀI HỌC - CẢ NĂM - CÓ FILE NGHE (FRIE...
 
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in Pharmacy
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in PharmacyASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in Pharmacy
ASTRINGENTS.pdf Pharmacognosy chapter 5 diploma in Pharmacy
 
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...
HỌC TỐT TIẾNG ANH 11 THEO CHƯƠNG TRÌNH GLOBAL SUCCESS ĐÁP ÁN CHI TIẾT - HK2 (...
 
Metabolism , Metabolic Fate& disorders of cholesterol.pptx
Metabolism , Metabolic Fate& disorders of cholesterol.pptxMetabolism , Metabolic Fate& disorders of cholesterol.pptx
Metabolism , Metabolic Fate& disorders of cholesterol.pptx
 
Riti theory by Vamana Indian poetics.pptx
Riti theory by Vamana Indian poetics.pptxRiti theory by Vamana Indian poetics.pptx
Riti theory by Vamana Indian poetics.pptx
 
EDD8524 The Future of Educational Leader
EDD8524 The Future of Educational LeaderEDD8524 The Future of Educational Leader
EDD8524 The Future of Educational Leader
 
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptx
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptxBBA 205 BUSINESS ENVIRONMENT UNIT I.pptx
BBA 205 BUSINESS ENVIRONMENT UNIT I.pptx
 
Awards Presentation 2024 - March 12 2024
Awards Presentation 2024 - March 12 2024Awards Presentation 2024 - March 12 2024
Awards Presentation 2024 - March 12 2024
 
Least Significance Difference:Biostatics and Research Methodology
Least Significance Difference:Biostatics and Research MethodologyLeast Significance Difference:Biostatics and Research Methodology
Least Significance Difference:Biostatics and Research Methodology
 
Dhavni Theory by Anandvardhana Indian Poetics
Dhavni Theory by Anandvardhana Indian PoeticsDhavni Theory by Anandvardhana Indian Poetics
Dhavni Theory by Anandvardhana Indian Poetics
 
3.14.24 The Selma March and the Voting Rights Act.pptx
3.14.24 The Selma March and the Voting Rights Act.pptx3.14.24 The Selma March and the Voting Rights Act.pptx
3.14.24 The Selma March and the Voting Rights Act.pptx
 
Quantitative research methodology and survey design
Quantitative research methodology and survey designQuantitative research methodology and survey design
Quantitative research methodology and survey design
 
2024.03.16 How to write better quality materials for your learners ELTABB San...
2024.03.16 How to write better quality materials for your learners ELTABB San...2024.03.16 How to write better quality materials for your learners ELTABB San...
2024.03.16 How to write better quality materials for your learners ELTABB San...
 
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdf
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdfArti Languages Pre Seed Send Ahead Pitchdeck 2024.pdf
Arti Languages Pre Seed Send Ahead Pitchdeck 2024.pdf
 
The First National K12 TUG March 6 2024.pdf
The First National K12 TUG March 6 2024.pdfThe First National K12 TUG March 6 2024.pdf
The First National K12 TUG March 6 2024.pdf
 
LEAD6001 - Introduction to Advanced Stud
LEAD6001 - Introduction to Advanced StudLEAD6001 - Introduction to Advanced Stud
LEAD6001 - Introduction to Advanced Stud
 
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...
THYROID HORMONE.pptx by Subham Panja,Asst. Professor, Department of B.Sc MLT,...
 
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc
30-de-thi-vao-lop-10-mon-tieng-anh-co-dap-an.doc
 
ANOVA Parametric test: Biostatics and Research Methodology
ANOVA Parametric test: Biostatics and Research MethodologyANOVA Parametric test: Biostatics and Research Methodology
ANOVA Parametric test: Biostatics and Research Methodology
 

Tropical Climate

  • 1. Aaqib Iqbal Deccan School of Planning & Architecture CLIMATOLOGY PROJECT ON TROPICAL CLIMATE
  • 2. • Climate is a measure of the average pattern of variation in temperature, humidity, atmospheric pressure, wind, precipitation, atmospheric particle count and other meteorological variables in a given region over long periods of time. Climate is different from weather, in that weather only describes the short-term conditions of these variables in a given region • A region's climate is generated by the climate system, which has five components: atmosphere, hydrosphere,cryosphere, lithosphere, and biosphere. • The climate of a location is affected by its latitude, terrain, and altitude, as well as nearby water bodies and their currents. Climates can be classified according to the average and the typical ranges of different variables, most commonly temperature and precipitation. CLIMATE
  • 4. • A tropical climate is a climate in the tropical region. In the Köppen climate classification it is a non- arid climate in which all twelve months have mean temperatures of at least 18 °C (64 °F). • Tropical temperature remains relatively constant throughout the year and seasonal variations are dominated by precipitation. • Tropical Climates are those climates where heat is dominant problem where the greater part of year buildings serve to keep cool for occupants room rather than warm. TROPICAL CLIMATE
  • 5. • The Basis of classification is given by 3 atmospheric factors which dominantly influence human comfort – air , temperate & humidity • The Tropical regions of earth are divided into 3 major climatic zones & three sub groups Warm Humid equatorial climate Hot Dry Desert (or) semi desert climate Composite or monsoon climate CLASSIFICATION
  • 6. • These climates are found in belt near equator extending to about 15ºN & s. Logos,Dar-es-Salam,Colombo,Singapore etc are examples of this climate. There is very less seasonal variation throughout the year .Periods of more or less rain & occurrence of gusty winds & electric storms Air Temperature – Shades reaches a max during the day of between 27 & 32ºc but occasionally it may exceed. The mean minimum varies from 21º & 27ºc Humidity – Rh(Relative humidity remains high at about 75 % for most of the time but it may vary from 55 to almost 100 % . Vapor pressure is steady from 2500 to 3000 N/m2 WARM HUMID CLIMATE
  • 7. Locations of warm humid climates
  • 8.  Precipitation – High through out the year. Annual rainfall can vary from2000 to 5000 mm & may exceed 500 mm . Sky Condition – Fairly cloudy throughout the year . Cloud cover varies between 60 & 90 % .Skies are usually bright . Solar Radiation – is partly reflected & partly scattered by cloud blanket but strong radiation can cause painful sky glare Wind Velocities – are typically low, calm periods are forewent but strong winds can occur during rainfall Vegetation : Grown quickly due to frequent rains & high temperature & it is difficult to control the red or brown laterite soils are generally poor for agriculture . Special Characteristics – High humidity accelerates mould & algal growth rusting & rotting .Organic buildings materials tend to decay rapidly Mosquitoes and other insects abound .The thunder storms are accompanied by frequent air – to air electrical discharges
  • 9. These climates occur in two belts at latitudes between approximately 15 & 30ºnorth & south of the equator . Example's : Assuan Baghdad,Alice springs & phoenix Two marked seasons occur :a hot & a somewhat cooler period Air Temperature : DBT in shade rises quickly after sunrise to day time mean maximum temperature ranged from 27 to 32ºc . Night time mean minima between 24 & 30ºc in hot season & between 10 & 18º in cool season .The diurnal range is very great 17 to 22º Humidity : RH varies from 10 to 55 % as wet depression is large (rapid evaporation) .Vapor pressure is normally between 750 & 1500 N /m2 HOT DRY DESERT CLIMATE
  • 10. LOCATIONS OF HOT DRY DESERT CLIMATE
  • 11. Precipitation : Slight & variable throughout the year, from 50 to 155 mm per annum ,Flash storms may occur over limited areas but some regions may not have rains for several years . Sky Conditions : Normally Clear .Clouds are few due to low humidity of the air . The sky is usually dark blue , with a luminance of 700 to 2500 cd/m2 & further darkened dust or sand storms may occur Solar Radiation : Direct & strong during the day , but the absence of cloud permits easy release of hear stored during day time Winds : are usually local .Heating of air over hot ground cause a temperature inversion Vegetation : is sparse & difficult to maintain humidity . The soil is usually dusty & very dry. Soils dries quickly after rain & would generally be fertile if irrigated
  • 12. • These climates usually occur in large land masses near tropics of cancer & Capricorn which are sufficiently far from equator to experience seasonal changes in solar radiation & wind direction • Examples : Lahore ,Mandalay, New Delhi • Two seasons occur normally .Approximately 2/3rds of the year is hot dry & other third is warm humid. Localities further north & south often have a third season but described as cool dry Air temperature : in shade as follows COMPOSITE OR MONSOON CLIMATE Seasons Hot Dry Warm Humid Cool Dry Day time 32 -43ºc 27-32ºc Upton 27ºc Night time 21-27ºc 24-27ºc 4-10ºc Diurnal mean range 11-22ºc 3-6 11-22ºc
  • 13. LOCATIONS OF COMPOSITE OR MONSOON CLIMATE
  • 14.  Humidity i.e. RH : Is low throughout the dry periods at 20 to 55 % with a vapor pressure of 1300 to 1600 N/m2.Durin wet period it rises to 55 to 95 % Precipitation : Monsoon rains are intense & continued for a long time occasionally 25 to 38 mm can fall in an hour. Annual rainfall varies from 500 to 1300 mm with 200 to 250 mm wettest month. There Is little rain during dry seasons Sky conditions :Markedly vary with the seasons .The sky is heavily overcast & dull during monsoons & clear with dark blue color in dry seasons Solar Radiation : Alternated between conditions found in warm humid & hot dry desert climates Winds : are hot & dusty during dry period .Monsoon winds are fairly strong & steady
  • 15. • Vegetation : Hot dry region has brown & red barren ground which changes rapidly with the rain .Plants grow quickly. There is a risk of soil erosion during monsoon • Special Characteristics : Seasonal changes in relative humidity cause rapid weakening of building materials .Dust & Sand storms may occur
  • 16. THANK YOU Aaqib Iqbal| 13131AA001 |THIRD SEM

Editor's Notes

  1. Insert a map of your country.
  2. Insert a picture of one of the geographic features of your country.
  3. Insert a picture illustrating a season in your country.
  4. Insert a picture of an animal and or plant found in your country.
  5. Insert a picture illustrating a custom or tradition here.
  6. Insert a picture of the head leader of your country.
  7. Insert a picture that illustrates some part of your country’s economy.
  8. Insert a picture of one of the points of interest for your country.