LATITUDE AND LONGITUDE INCLUDING IMPORTANT PARALLELS AND MERIDIANS

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LATITUDE AND LONGITUDE INCLUDING IMPORTANT PARALLELS AND MERIDIANS

 
 
 
 
Latitude and longitude are the fundamental tools used to pinpoint locations on Earth, forming a geographical grid system. Understanding these, along with important parallels and meridians, is essential for navigation, mapmaking, and comprehending various geographical phenomena.
 
 
1. Latitude
 
Latitude is measured in degrees, ranging from 0° at the equator to 90° north and 90° south. Each degree can be further subdivided into minutes and seconds for greater precision. The Earth's circumference is approximately 40,007 kilometres (24,901 miles) at the equator. Therefore, one degree of latitude corresponds to roughly 111 kilometres (69 miles). This distance decreases slightly as you move away from the equator due to the Earth's slightly oblate shape.

Importance of Latitude

  • Climate and Weather: Latitude plays a crucial role in determining climate and weather patterns. Regions closer to the equator experience direct sunlight throughout the year, leading to warmer temperatures and tropical climates. Conversely, polar regions receive less sunlight, resulting in colder temperatures and distinct seasons.
  • Daylight Hours: The number of daylight hours varies depending on latitude. At the poles, the sun doesn't rise or set for extended periods during summer and winter solstices, respectively. This phenomenon, known as polar day and polar night, is directly linked to the tilt of Earth's axis and its rotation around the sun.
  • Navigation and Mapping: Latitude, along with longitude, forms the foundation of the global coordinate system. This system allows for precise location identification, navigation, and mapmaking. Knowing the latitude of a specific location allows us to determine its approximate distance from the equator and its position within one of the five major climate zones: tropical, subtropical, temperate, subarctic, and arctic.
  • Biogeography and Ecosystems: Latitude influences the distribution of plant and animal life on Earth. Different latitudes support diverse ecosystems adapted to specific temperatures, precipitation, and sunlight patterns. Studying the variations in biogeography across latitudes helps us understand the intricate relationship between life and its environment.

 

1.1. Important Parallels

 
Tropic of Cancer (23.5° N)
 
 
The Tropic of Cancer is the most northerly circle of latitude on Earth at which the Sun can be directly overhead. This occurs on the June solstice when the Northern Hemisphere is tilted toward the Sun to its maximum extent. It also reaches 90 degrees below the horizon at solar midnight on the December Solstice. Using a continuously updated formula, the circle is currently 23°26′10.2″ (or 23.43616°) north of the Equator.
Image of Tropic of Cancer on the globe
  • The Tropic of Cancer passes through 23 countries and territories: Mexico, The Bahamas, Western Sahara, Mauritania, Mali, Niger, Algeria, Libya, Chad, Egypt, Saudi Arabia, United Arab Emirates, Oman, India, Bangladesh, Myanmar, China, Taiwan, Mexico, and the United States.
  • The Tropic of Cancer marks the boundary between the tropics and the subtropical zones. The tropics are the region between the Tropic of Cancer and the Tropic of Capricorn, and they are characterized by hot, humid weather year-round. The subtropical zones are located north and south of the tropics, and they have warm to hot summers and mild winters.
  • The Tropic of Cancer is an important cultural and religious symbol in many parts of the world. In India, for example, it is known as the Uttarayan, and it is celebrated as a festival of the Sun's northward journey.
 
 
Tropic of Capricorn (23.5° S)
 
 

The Tropic of Capricorn is the most southerly circle of latitude on Earth where the Sun can be directly overhead. This occurs on the December solstice, when the Southern Hemisphere is tilted towards the Sun to its maximum extent. It also reaches 90 degrees below the horizon at solar midnight on the June Solstice. Its current latitude is 23°26′10.2″ (or 23.43616°) south of the Equator, as calculated using a continuously updated formula.

Image of Tropic of Capricorn on a globe
  • Countries and Territories Crossed: The Tropic of Capricorn passes through 26 countries and territories: Namibia, Botswana, South Africa, Mozambique, Zimbabwe, Madagascar, Malawi, Zambia, Mozambique Channel, Paraguay, Brazil, Argentina, Chile, Bolivia, French Polynesia, Pitcairn Islands, Australia, Southern Ocean, Tonga, Niue, Cook Islands, French Southern and Antarctic Lands, and South Georgia and the South Sandwich Islands.
  • Climate Zones: The Tropic of Capricorn marks the boundary between the tropics and the subtropical zones. The tropics, located between the Tropic of Capricorn and the Tropic of Cancer, are characterized by hot, humid weather year-round. The subtropical zones, located north and south of the tropics, have warm to hot summers and mild winters.
  • Cultural and Religious Significance: The Tropic of Capricorn is an important cultural and religious symbol in many parts of the world. In Argentina, for example, it is known as the Trópico de Capricornio and is associated with themes of new beginnings and transformation.
 
 
Arctic Circle (66.5° N)
 
 
The Arctic Circle is a parallel of latitude located at approximately 66° 33′ 48″ north of the Equator. It marks the southernmost boundary of the Arctic, a region characterized by polar climates and long periods of darkness and sunlight depending on the season.
  • Unique Phenomenon: Due to the Earth's tilt on its axis, the Arctic Circle experiences polar day and polar night. During the summer solstice (around June 21st), the sun stays above the horizon for at least 24 hours continuously, while during the winter solstice (around December 21st), the sun stays below the horizon for at least 24 hours continuously. The length of these periods of continuous daylight and darkness increases the farther north you travel within the Arctic Circle, culminating in six months of daylight and six months of darkness at the North Pole.
  • Countries and Territories Crossed: The Arctic Circle passes through eight countries and territories: Canada, Denmark (Greenland), Finland, Iceland, Norway, Russia, Sweden, and the United States (Alaska).
Image of Arctic Circle map
  • Climate and Geography: The Arctic is characterized by cold, dry winters and cool, short summers. The landscape is dominated by tundra, a vast treeless plain with permafrost (permanently frozen ground), and glaciers. The Arctic Ocean covers much of the region, and sea ice plays a crucial role in the Arctic ecosystem.
  • Cultural and Environmental Significance: The Arctic is home to diverse indigenous cultures that have adapted to the challenging environment for centuries. However, the region is also facing significant challenges due to climate change, which is causing rising temperatures, melting glaciers, and sea ice loss.
 
Antarctic Circle (66.5° S)
 

The Antarctic Circle, a parallel of latitude at 66.5° South, serves as the gateway to the vast and mysterious continent of Antarctica. 

  • Midnight Sun and Polar Night: Similar to the Arctic Circle, the Antarctic Circle experiences the captivating phenomena of midnight sun and polar night. For at least one day during summer (around December 22nd), the sun remains continuously above the horizon, while for at least one day during winter (around June 21st), it stays completely below the horizon.
  • Impact on Climate and Geography: The Antarctic Circle influences the region's frigid climate. Areas further south experience even colder temperatures due to minimal direct sunlight. This, along with the polar day and night, shapes the unique landscape dominated by glaciers, ice shelves, and minimal vegetation.
  • Countries and Territories: Unlike the Arctic Circle, the Antarctic Circle doesn't pass through any sovereign land. Instead, it traverses the territorial claims of several countries, including Argentina, Australia, Chile, France, New Zealand, Norway, the United Kingdom and the United States.
  • Scientific and Exploration Hub: The Antarctic Circle serves as a crucial access point for numerous research stations and scientific expeditions. These endeavours aim to understand the continent's climate, geology, and unique ecosystems, providing valuable insights into global processes and the potential impacts of climate change.
  • Conservation Challenges: Antarctica faces various environmental threats, including rising sea levels, melting glaciers, and potential resource exploitation. Protecting this fragile ecosystem and its diverse wildlife requires international cooperation and effective conservation measures.
 
2. Longitude
 

Longitude, the measurement of east or west distance from the Prime Meridian, plays a crucial role in pinpointing locations on Earth alongside its partner, latitude. Measured in degrees (0° to 180°), east or west of the Prime Meridian. The Prime Meridian (0°) runs through Greenwich, England, serving as the reference point. Earth is divided into eastern and western hemispheres by the Prime Meridian.

 

2.1. Important Meridians

 
International Date Line (180°)
 

The International Date Line (IDL) is an imaginary line that runs along the 180th meridian in the Pacific Ocean. It serves as the demarcation line for calendar days, and crossing it results in a change of date.

  • Location: The IDL is located at 180 degrees longitude, halfway around the world from the prime meridian, which is at 0 degrees longitude and passes through Greenwich, London.
  • Direction: The IDL is not a straight line but deviates to accommodate political and economic considerations. It zigzags around certain regions and islands to avoid splitting them into two different days.
  • Date Change: When crossing the IDL from west to east, a day is subtracted, advancing the calendar by one day. Conversely, when crossing from east to west, a day is added, moving the calendar back by one day.
  • Time Zone Conventions: To the west of the IDL, the time is earlier, and to the east, the time is later. The time difference across the IDL is typically 24 hours, but variations exist due to deviations in the line's path.
  • Pacific Region Significance: The IDL is most relevant in the Pacific region, where it passes through various island nations and territories. Some notable locations affected by the IDL include Fiji, Tonga, Samoa, and the Chatham Islands of New Zealand.
  • IDL Adjustments: Some regions near the IDL have made adjustments to their time zone to be on the same side as their trading partners or cultural influences. For example, Samoa moved from the west side to the east side of the IDL in 2011, skipping December 30, 2011, and going straight to December 31, 2011.
  • Chatham Islands Anomaly: The Chatham Islands, an archipelago off the east coast of New Zealand, observe a time zone that is 45 minutes ahead of New Zealand Standard Time, creating a unique time difference.
  • Deviations Around Islands: The IDL deviates around certain islands to avoid splitting them into different days. One example is the deviation around the Russian-controlled Big Diomede and Little Diomede islands in the Bering Strait.
The International Date Line is a critical concept for international travellers, businesses, and global communication, as it helps regulate the measurement of time and dates across different regions of the world. Its design considers both practical and political considerations to ensure smooth coordination of time and date changes.
 
 
Standard Meridians
 

Standard meridians are specific lines of longitude used as reference points for defining time zones. These meridians are multiples of 15 degrees and typically correspond to the centre of each time zone. The use of standard meridians helps organize the world into distinct time zones, allowing for a standardized measurement of time across different regions.

  • Time Zones: The Earth is divided into 24 time zones, each representing one hour. These time zones are centred around standard meridians, which are multiples of 15 degrees.
  • Prime Meridian (0°): The prime meridian, located at 0 degrees longitude, is the reference line for Greenwich Mean Time (GMT) or Coordinated Universal Time (UTC). It serves as the starting point for measuring time zones.
  • Standard Time Zones: Standard meridians are usually set at intervals of 15 degrees east or west of the prime meridian. The central meridian for each time zone is typically used to determine the standard time for that zone.
  • Longitude and Time Relationship: Every 15-degree increment in longitude corresponds to a one-hour difference in time. As one moves eastward or westward from the prime meridian, the time increases or decreases by one hour, respectively.
  • UTC Offset: The standard meridian for a particular time zone is associated with a specific UTC offset, indicating the number of hours ahead or behind Coordinated Universal Time (UTC). For example, a location with a standard meridian at 75 degrees west may have a UTC offset of UTC-5.
  • International Date Line (IDL): The International Date Line (IDL), located at 180 degrees longitude, serves as the transition point between calendar days. Crossing the IDL results in a change of date.
  • Deviations: While standard meridians are generally set at 15-degree intervals, there are deviations to accommodate political and economic considerations. Some time zone boundaries deviate from these intervals to include or exclude certain regions.
  • Time Zone Map: The organization of standard meridians into time zones is depicted on a time zone map, which illustrates the division of the world into regions with consistent timekeeping.

Understanding standard meridians and time zones is crucial for coordinating activities, travel planning, and maintaining a standardized measurement of time across the globe. The use of standard meridians helps facilitate global communication and ensures that time is uniformly measured, making it easier to schedule events and activities on an international scale.

 
Previous Year Questions
 

1. In the South Atlantic and South-Eastern Pacific regions in tropical latitudes, cyclone does not originate. What is the reason? (upsc 2015)

(a) Sea surface temperatures are low

(b) Inter-Tropical Convergence Zone seldom occurs

(c) Coriolis force is too weak

(d) Absence of land in those regions

Answer: B

2. Among the following cities, which one lies on a longitude closest to that of Delhi? (UPSC 2018)

(a) Bengaluru

(b) Hyderabad

(c) Nagpur

(d) Pune

 Answer: A

3. On 21st June, the Sun (UPSC 2019)

(a) does not set below the horizon at the Arctic Circle

(b) does not set below the horizon at Antarctic Circle

(c) shines vertically overhead at noon on the Equator

(d) shines vertically overhead at the Tropic of Capricorn

Answer: A

Mains

1. Major hot deserts in northern hemisphere are located between 20-30 deg N latitudes and on the western side of the continents. Why? (UPSC 2013)

 

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