SlideShare a Scribd company logo
Geographic
Coordinate
System
By Mahnoor Bukhari
Shape of the Earth
• Geodesy studies Earth’s shape, orientation, and positions for the past,
present, and future.
• It also studies where things are and where things are going to with extreme
accuracy.
• Models of Earth:
i. Spheroid
ii. Ellipsoid
iii. Geoid (true 3-D shape of Earth considered as a mean sea level extended continuously
through the continents)
• Geodesists have adopted an Ellipsoid model to determine Latitude and
Longitude coordinates.
a figure resembling a sphere. also : an object of approximately spherical shape.
Ellipsoid
• The Earth is an Ellipsoid.
• Because of the "bulging" caused by the Earth spinning, the Earth is not
completely round, thus, is not a sphere. Instead, we use the term
"oblate spheroid," or "ellipsoid."
• Earth Bulges at the Equator.
• We say Earth is a sphere… But it’s not exactly a perfect one.
• It’s an oblate spheroid that bulges at the equator and is somewhat
squashed at the poles.
Geoid and Ellipsoid Example
Earth’s Geographical
Coordinates
• Latitude and longitude, together forms Earth’s
geographical coordinates, and represents the
angular distance of any location from the center of
the Earth.
• A grid of parallels and meridians shown as lines
on a map is called a ‘graticule’.
Latitudes
• Any circle that runs east and west around Earth and that is parallel to
the equator is called ‘parallel’ or a ‘line of latitude’.
• All parallels (lines of latitude) except equator get smaller as you get
near the pole.
• Parallel but not equal.
• Five Important Latitudes:
• Arctic circle -----------------→ 66 1/2° N
• Tropic of cancer -----------------→ 23 1/2° N
• Equator -----------------→ 0°
• Tropic of Capricorn -------------→ 23 1/2° S
• Antarctic circle -----------------→ 66 1/2° S
Longitudes
(earth)
• Any semi-circle that runs north and south around Earth from the
geographic north pole to geographic south pole is called ‘meridian’ or
‘line of longitude’.
• The distance between longitudes reaches zero at the poles as the lines
of meridian converge at that point.
• Not parallel but equal.
And on the other hand, lines of
longitude have X-coordinates
between -180 and +180 degrees.
As shown in the image, lines of
latitudes have Y-values that are
between -90 and +90 degrees.
Explanation of Coordinate System
• When you put two coordinates together as a pair (X, Y), you can locate anything on Earth.
• Latitude and longitude form our coordinate system grid.
• Thanks to our geographic coordinate, you can pinpoint any point on Earth such as GPS
receivers.
• Cartographers write latitudes and longitudes in degrees-minutes-seconds (DMS) and
decimal degrees. For degrees-minutes-seconds, minutes range from 0 to 60. For example, the
geographic coordinate expressed in degrees-minutes-seconds for New York City is:
• Latitude: 40 degrees, 42 minutes, 51 seconds N
• Longitude: 74 degrees, 0 minutes, 21 seconds W
• You can also express geographic coordinates in decimal degrees. It’s just another way to
represent that same location in a different format. For example, here is New York City in
decimal degrees:
• Latitude: 40.714 N
• Longitude: -74.006 W
GPS Coordinates Pakistan
• Pakistan lies in the North-East part of the world
• 23 degrees 35 minutes to 37 degrees 05 minutes North (latitude)
• 60 degrees 50 minutes to 77 degrees 50 minutes East (longitude)
World Time Zones
UTC vs. GMT: History
• You'll often see UTC (Coordinated Universal Time) and GMT (Greenwich Mean Time) used
interchangeably, and while doing so can be suitable for informal use, they are not technically the same.
• GMT, or Greenwich Mean Time, is a time zone located along the prime meridian. It was established as
an international standard in 1884 at the International Meridian Conference, where many nations got
together to decide what the prime meridian of the Earth would be. Prior to this, time varied wildly in
different areas.
• The prime meridian selected at that conference runs through the Royal Observatory in Greenwich,
giving the time zone its name. From 1884 until the 1950s, GMT was used as the time standard.
• However, as atomic clocks were invented in the 1950s, there were more accurate ways of keeping time.
The new standard for coordinated time was first used at the beginning of 1960, but it didn't become an
official term until 1967 and replaced GMT a few years later.
• So, GMT is a time zone, while UTC is a time standard. You can consider UTC the successor to GMT, as
it's more accurate.
UTC or Coordinated Universal Time
• What Is UTC?
• UTC is the standard of time used all around the world to regulate clocks. It is
effectively the "center" of our timekeeping, with all time zones referenced in relation to
how far ahead of, or far behind, UTC they are.
• The full name for UTC is Coordinated Universal Time, and its initialism was reached
as a compromise. English speakers wanted to use CUT (for "Coordinated Universal
Time"), while French speakers advocated for TUC (short for "temps universel
coordonné"). Ultimately, UTC was chosen.
Time Zones Explained
• What are the Time Zones?
• Time Zones are a geographical division of the terrestrial globe into 24
longitudinal sections. The distance between two consecutive time zones is
approximately 15°. Each such time zone observes a uniform standard time.
• We have 24 different time zones in the world. Because the Earth rotates
360° every 24 hours, each time zone is 15° longitude apart from the other.
(360÷24=15)
• The Prime Meridian (Greenwich Meridian) defines the center of the first
time zone in the world
Irregular Time Zone Boundaries
• No time zone in the world runs a perfect north-south line. Instead, they
are jagged and adapt to the political boundaries of countries. Also,
there can be “irregular square” time zones similar to islands.
Geographic Coordinate System.pdf
Name Description Relative to GMT
GMT Greenwich Mean Time GMT
UTC Universal Coordinated Time GMT
ECT European Central Time GMT+1:00
EET Eastern European Time GMT+2:00
ART (Arabic) Egypt Standard Time GMT+2:00
EAT Eastern African Time GMT+3:00
MET Middle East Time GMT+3:30
NET Near East Time GMT+4:00
PKT Pakistan Standard Time GMT+5:00
IST India Standard Time GMT+5:30
BST Bangladesh Standard Time GMT+6:00
Why do countries need different time zones?
• Maintaining different time zones for any country is not an easy choice.
From commercial and business transactions to transportation and
communication, everything is dependent on time. Thus, most countries
of the world have opted for one standard time zone. Some countries,
with comparatively larger areas or territories scattered around the
world, do opt for multiple time zones. For example, the USA, Russia
and Canada have multiple time zones within the country.
Geographic Coordinate System.pdf
What is UTC Offset?
• UTC Offset is the time difference of a particular place from UTC. It is
measured in hours and minutes.
• For a place ahead of UTC (east of UTC), a positive sign is used.
Similarly, for a place which is located behind the UTC (west of UTC),
a negative sign is used.
• Example
• The time zone in Toronto (Canada) is UTC-4 while the time zone in
Beijing (China) is UTC+8.
Pakistan Time Zone
• Pakistan Standard Time (abbreviated as PKT) is UTC+05:00 hours
ahead of Coordinated Universal Time.
International Date Line
• The International Date Line is a north-south line in the Pacific Ocean
where you turn your calendar back or ahead one day. The center of the
time zone roughly follows 180° longitude without crossing any
landmass.
• When you cross the International Date Line moving toward the east,
you turn your calendar back one day. Whereas when you go from the
west across the International Date Line, you turn your calendar ahead
one day.
Thanks.

More Related Content

PPTX
Coordinate system Geographical coordinate system
PPTX
PDF
PPTX
Scope and content of population geography
PPT
projection
PPTX
Geometry and types of aerial photographs
PPTX
Distribution of maps
PPTX
Geological Structures
Coordinate system Geographical coordinate system
Scope and content of population geography
projection
Geometry and types of aerial photographs
Distribution of maps
Geological Structures

What's hot (20)

PPT
Distribution maps
PPSX
Drainage basin morphometry
PPTX
Fluvial process
PPT
Map Reading
PPT
Drainage Basins
PPT
Topography powerpoint
PPTX
Aquifer
PPTX
morphometry of drainage basin.pptx
PPTX
Morphometric Analysis of Drainage Basin.pptx
PPTX
Soil formation
PPT
Map scale and projection
PDF
georeference
PPT
Elements of a map
PPTX
Aerial photography.pptx
PPT
Digital Cartography
PPTX
Fluvial landforms
PPTX
Maps and map reading
PPTX
Types of Aquifers
PPTX
Basic coordinate system
PDF
Drainage pattern
Distribution maps
Drainage basin morphometry
Fluvial process
Map Reading
Drainage Basins
Topography powerpoint
Aquifer
morphometry of drainage basin.pptx
Morphometric Analysis of Drainage Basin.pptx
Soil formation
Map scale and projection
georeference
Elements of a map
Aerial photography.pptx
Digital Cartography
Fluvial landforms
Maps and map reading
Types of Aquifers
Basic coordinate system
Drainage pattern
Ad

Similar to Geographic Coordinate System.pdf (20)

PPT
Role of Geography in Tourism
PPT
Geography five lab one
PPT
Geography five lab one
PPT
Lab two location and time
PPTX
Travel Agency and Tour Operation Management -Geography of Tourism
PDF
QUICK GEOGRAPHY (1).pdf
PPTX
Geographic grid latitudes and longitudes made by Ravi Bharti
PPTX
3 lengte en breetelyne
PPTX
UNDERSTANDING TIME & DATE MERIDIAN
PPTX
FINAL globe latitudes and longitudes (1).pptx
PPTX
earth living planet.pptx
PPT
lat_and_lon_poewrpoint1_teacher_copy.ppt
PPTX
6 latitude an longitude ..pptx
PPTX
9. Time
PPT
Time zones and international date line (idl
PPT
Location and time
PPTX
4 atlas en kaartskale
PPTX
Planet earth
PDF
GLOBE.pdf
Role of Geography in Tourism
Geography five lab one
Geography five lab one
Lab two location and time
Travel Agency and Tour Operation Management -Geography of Tourism
QUICK GEOGRAPHY (1).pdf
Geographic grid latitudes and longitudes made by Ravi Bharti
3 lengte en breetelyne
UNDERSTANDING TIME & DATE MERIDIAN
FINAL globe latitudes and longitudes (1).pptx
earth living planet.pptx
lat_and_lon_poewrpoint1_teacher_copy.ppt
6 latitude an longitude ..pptx
9. Time
Time zones and international date line (idl
Location and time
4 atlas en kaartskale
Planet earth
GLOBE.pdf
Ad

Recently uploaded (20)

PPTX
Onco Emergencies - Spinal cord compression Superior vena cava syndrome Febr...
PPTX
Chinmaya Tiranga Azadi Quiz (Class 7-8 )
PDF
SOIL: Factor, Horizon, Process, Classification, Degradation, Conservation
DOC
Soft-furnishing-By-Architect-A.F.M.Mohiuddin-Akhand.doc
PDF
OBE - B.A.(HON'S) IN INTERIOR ARCHITECTURE -Ar.MOHIUDDIN.pdf
PPTX
Tissue processing ( HISTOPATHOLOGICAL TECHNIQUE
PDF
Black Hat USA 2025 - Micro ICS Summit - ICS/OT Threat Landscape
PPTX
UNIT III MENTAL HEALTH NURSING ASSESSMENT
PDF
LNK 2025 (2).pdf MWEHEHEHEHEHEHEHEHEHEHE
PDF
Supply Chain Operations Speaking Notes -ICLT Program
PDF
Trump Administration's workforce development strategy
PDF
Empowerment Technology for Senior High School Guide
PDF
Chinmaya Tiranga quiz Grand Finale.pdf
PPTX
CHAPTER IV. MAN AND BIOSPHERE AND ITS TOTALITY.pptx
PDF
A GUIDE TO GENETICS FOR UNDERGRADUATE MEDICAL STUDENTS
PDF
What if we spent less time fighting change, and more time building what’s rig...
PDF
A systematic review of self-coping strategies used by university students to ...
PDF
medical_surgical_nursing_10th_edition_ignatavicius_TEST_BANK_pdf.pdf
PPTX
UV-Visible spectroscopy..pptx UV-Visible Spectroscopy – Electronic Transition...
PDF
ChatGPT for Dummies - Pam Baker Ccesa007.pdf
Onco Emergencies - Spinal cord compression Superior vena cava syndrome Febr...
Chinmaya Tiranga Azadi Quiz (Class 7-8 )
SOIL: Factor, Horizon, Process, Classification, Degradation, Conservation
Soft-furnishing-By-Architect-A.F.M.Mohiuddin-Akhand.doc
OBE - B.A.(HON'S) IN INTERIOR ARCHITECTURE -Ar.MOHIUDDIN.pdf
Tissue processing ( HISTOPATHOLOGICAL TECHNIQUE
Black Hat USA 2025 - Micro ICS Summit - ICS/OT Threat Landscape
UNIT III MENTAL HEALTH NURSING ASSESSMENT
LNK 2025 (2).pdf MWEHEHEHEHEHEHEHEHEHEHE
Supply Chain Operations Speaking Notes -ICLT Program
Trump Administration's workforce development strategy
Empowerment Technology for Senior High School Guide
Chinmaya Tiranga quiz Grand Finale.pdf
CHAPTER IV. MAN AND BIOSPHERE AND ITS TOTALITY.pptx
A GUIDE TO GENETICS FOR UNDERGRADUATE MEDICAL STUDENTS
What if we spent less time fighting change, and more time building what’s rig...
A systematic review of self-coping strategies used by university students to ...
medical_surgical_nursing_10th_edition_ignatavicius_TEST_BANK_pdf.pdf
UV-Visible spectroscopy..pptx UV-Visible Spectroscopy – Electronic Transition...
ChatGPT for Dummies - Pam Baker Ccesa007.pdf

Geographic Coordinate System.pdf

  • 2. Shape of the Earth • Geodesy studies Earth’s shape, orientation, and positions for the past, present, and future. • It also studies where things are and where things are going to with extreme accuracy. • Models of Earth: i. Spheroid ii. Ellipsoid iii. Geoid (true 3-D shape of Earth considered as a mean sea level extended continuously through the continents) • Geodesists have adopted an Ellipsoid model to determine Latitude and Longitude coordinates. a figure resembling a sphere. also : an object of approximately spherical shape.
  • 3. Ellipsoid • The Earth is an Ellipsoid. • Because of the "bulging" caused by the Earth spinning, the Earth is not completely round, thus, is not a sphere. Instead, we use the term "oblate spheroid," or "ellipsoid." • Earth Bulges at the Equator. • We say Earth is a sphere… But it’s not exactly a perfect one. • It’s an oblate spheroid that bulges at the equator and is somewhat squashed at the poles.
  • 5. Earth’s Geographical Coordinates • Latitude and longitude, together forms Earth’s geographical coordinates, and represents the angular distance of any location from the center of the Earth. • A grid of parallels and meridians shown as lines on a map is called a ‘graticule’.
  • 7. • Any circle that runs east and west around Earth and that is parallel to the equator is called ‘parallel’ or a ‘line of latitude’. • All parallels (lines of latitude) except equator get smaller as you get near the pole. • Parallel but not equal. • Five Important Latitudes: • Arctic circle -----------------→ 66 1/2° N • Tropic of cancer -----------------→ 23 1/2° N • Equator -----------------→ 0° • Tropic of Capricorn -------------→ 23 1/2° S • Antarctic circle -----------------→ 66 1/2° S
  • 9. • Any semi-circle that runs north and south around Earth from the geographic north pole to geographic south pole is called ‘meridian’ or ‘line of longitude’. • The distance between longitudes reaches zero at the poles as the lines of meridian converge at that point. • Not parallel but equal.
  • 10. And on the other hand, lines of longitude have X-coordinates between -180 and +180 degrees. As shown in the image, lines of latitudes have Y-values that are between -90 and +90 degrees.
  • 11. Explanation of Coordinate System • When you put two coordinates together as a pair (X, Y), you can locate anything on Earth. • Latitude and longitude form our coordinate system grid. • Thanks to our geographic coordinate, you can pinpoint any point on Earth such as GPS receivers. • Cartographers write latitudes and longitudes in degrees-minutes-seconds (DMS) and decimal degrees. For degrees-minutes-seconds, minutes range from 0 to 60. For example, the geographic coordinate expressed in degrees-minutes-seconds for New York City is: • Latitude: 40 degrees, 42 minutes, 51 seconds N • Longitude: 74 degrees, 0 minutes, 21 seconds W • You can also express geographic coordinates in decimal degrees. It’s just another way to represent that same location in a different format. For example, here is New York City in decimal degrees: • Latitude: 40.714 N • Longitude: -74.006 W
  • 12. GPS Coordinates Pakistan • Pakistan lies in the North-East part of the world • 23 degrees 35 minutes to 37 degrees 05 minutes North (latitude) • 60 degrees 50 minutes to 77 degrees 50 minutes East (longitude)
  • 14. UTC vs. GMT: History • You'll often see UTC (Coordinated Universal Time) and GMT (Greenwich Mean Time) used interchangeably, and while doing so can be suitable for informal use, they are not technically the same. • GMT, or Greenwich Mean Time, is a time zone located along the prime meridian. It was established as an international standard in 1884 at the International Meridian Conference, where many nations got together to decide what the prime meridian of the Earth would be. Prior to this, time varied wildly in different areas. • The prime meridian selected at that conference runs through the Royal Observatory in Greenwich, giving the time zone its name. From 1884 until the 1950s, GMT was used as the time standard. • However, as atomic clocks were invented in the 1950s, there were more accurate ways of keeping time. The new standard for coordinated time was first used at the beginning of 1960, but it didn't become an official term until 1967 and replaced GMT a few years later. • So, GMT is a time zone, while UTC is a time standard. You can consider UTC the successor to GMT, as it's more accurate.
  • 15. UTC or Coordinated Universal Time • What Is UTC? • UTC is the standard of time used all around the world to regulate clocks. It is effectively the "center" of our timekeeping, with all time zones referenced in relation to how far ahead of, or far behind, UTC they are. • The full name for UTC is Coordinated Universal Time, and its initialism was reached as a compromise. English speakers wanted to use CUT (for "Coordinated Universal Time"), while French speakers advocated for TUC (short for "temps universel coordonné"). Ultimately, UTC was chosen.
  • 16. Time Zones Explained • What are the Time Zones? • Time Zones are a geographical division of the terrestrial globe into 24 longitudinal sections. The distance between two consecutive time zones is approximately 15°. Each such time zone observes a uniform standard time. • We have 24 different time zones in the world. Because the Earth rotates 360° every 24 hours, each time zone is 15° longitude apart from the other. (360÷24=15) • The Prime Meridian (Greenwich Meridian) defines the center of the first time zone in the world
  • 17. Irregular Time Zone Boundaries • No time zone in the world runs a perfect north-south line. Instead, they are jagged and adapt to the political boundaries of countries. Also, there can be “irregular square” time zones similar to islands.
  • 19. Name Description Relative to GMT GMT Greenwich Mean Time GMT UTC Universal Coordinated Time GMT ECT European Central Time GMT+1:00 EET Eastern European Time GMT+2:00 ART (Arabic) Egypt Standard Time GMT+2:00 EAT Eastern African Time GMT+3:00 MET Middle East Time GMT+3:30 NET Near East Time GMT+4:00 PKT Pakistan Standard Time GMT+5:00 IST India Standard Time GMT+5:30 BST Bangladesh Standard Time GMT+6:00
  • 20. Why do countries need different time zones? • Maintaining different time zones for any country is not an easy choice. From commercial and business transactions to transportation and communication, everything is dependent on time. Thus, most countries of the world have opted for one standard time zone. Some countries, with comparatively larger areas or territories scattered around the world, do opt for multiple time zones. For example, the USA, Russia and Canada have multiple time zones within the country.
  • 22. What is UTC Offset? • UTC Offset is the time difference of a particular place from UTC. It is measured in hours and minutes. • For a place ahead of UTC (east of UTC), a positive sign is used. Similarly, for a place which is located behind the UTC (west of UTC), a negative sign is used. • Example • The time zone in Toronto (Canada) is UTC-4 while the time zone in Beijing (China) is UTC+8.
  • 23. Pakistan Time Zone • Pakistan Standard Time (abbreviated as PKT) is UTC+05:00 hours ahead of Coordinated Universal Time.
  • 24. International Date Line • The International Date Line is a north-south line in the Pacific Ocean where you turn your calendar back or ahead one day. The center of the time zone roughly follows 180° longitude without crossing any landmass. • When you cross the International Date Line moving toward the east, you turn your calendar back one day. Whereas when you go from the west across the International Date Line, you turn your calendar ahead one day.