Saturday, 26 July 2025

The Sun

                                                                                                                                                                                                                           

             The Sun is the star at the centre of the Solar System. It is a massive, nearly perfect sphere of hot plasma, heated to incandescence by nuclear fusion reactions in its core, radiating the energy from its surface mainly as visible light and infrared radiation with 10% at ultraviolet energies. It is by far the most important source of energy for life on Earth. The Sun has been an object of veneration in many cultures. It has been a central subject for astronomical research since antiquity.

The Sun orbits the Galactic Center at a distance of 24,000 to 28,000 light-years. Its distance from Earth defines the astronomical unit, which is about 1.496×108 kilometres or about 8 light-minutesIts diameter is about 1,391,400 km (864,600 mi), 109 times that of Earth. The Sun's mass is about 330,000 times that of Earth, making up about 99.86% of the total mass of the Solar System. The mass of outer layer of the Sun's atmosphere, its photosphere, consists mostly of hydrogen (~73%) and helium (~25%), with much smaller quantities of heavier elements, including oxygencarbonneon, and iron.

The Sun is a G-type main-sequence star (G2V), informally called a yellow dwarf, though its light is actually white. It formed approximately 4.6 billion[a] years ago from the gravitational collapse of matter within a region of a large molecular cloud. Most of this matter gathered in the centre; the rest flattened into an orbiting disk that became the Solar System. The central mass became so hot and dense that it eventually initiated nuclear fusion in its core. Every second, the Sun's core fuses about 600 billion kilograms (kg) of hydrogen into helium and converts 4 billion kg of matter into energy.

About 4 to 7 billion years from now, when hydrogen fusion in the Sun's core diminishes to the point where the Sun is no longer in hydrostatic equilibrium, its core will undergo a marked increase in density and temperature which will cause its outer layers to expand, eventually transforming the Sun into a red giant. After the red giant phase, models suggest the Sun will shed its outer layers and become a dense type of cooling star (a white dwarf), and no longer produce energy by fusion, but will still glow and give off heat from its previous fusion for perhaps trillions of years. After that, it is theorised to become a super dense black dwarf, giving off negligible energy.

              Rotation

The Sun rotates faster at its equator than at its poles. This differential rotation is caused by convective motion due to heat transport and the Coriolis force due to the Sun's rotation. In a frame of reference defined by the stars, the rotational period is approximately 25.6 days at the equator and 33.5 days at the poles. Viewed from Earth as it orbits the Sun, the apparent rotational period of the Sun at its equator is about 28 days.[47] Viewed from a vantage point above its north pole, the Sun rotates counterclockwise around its axis of spin.[d][48]

A survey of solar analogues suggests the early Sun was rotating up to ten times faster than it does today. This would have made the surface much more active, with greater X-ray and UV emission. Sunspots would have covered 5–30% of the surface.[49] The rotation rate was gradually slowed by magnetic braking, as the Sun's magnetic field interacted with the outflowing solar wind.[50] A vestige of this rapid primordial rotation still survives at the Sun's core, which rotates at a rate of once per week; four times the mean surface                                                                         

Composition

The Sun consists mainly of the elements hydrogen and helium. At this time in the Sun's life, they account for 74.9% and 23.8%, respectively, of the mass of the Sun in the photosphere.[53] All heavier elements, called metals in astronomy, account for less than 2% of the mass, with oxygen (roughly 1% of the Sun's mass), carbon (0.3%), neon (0.2%), and iron (0.2%) being the most abundant.[54]

The Sun's original chemical composition was inherited from the interstellar medium out of which it formed. Originally it would have been about 71.1% hydrogen, 27.4% helium, and 1.5% heavier elements.[53] The hydrogen and most of the helium in the Sun would have been produced by Big Bang nucleosynthesis in the first 20 minutes of the universe, and the heavier elements were produced by previous generations of stars before the Sun was formed, and spread into the interstellar medium during the final stages of stellar life and by events such as supernovae.[55]

Since the Sun formed, the main fusion process has involved fusing hydrogen into helium. Over the past 4.6 billion years, the amount of helium and its location within the Sun has gradually changed. The proportion of helium within the core has increased from about 24% to about 60% due to fusion, and some of the helium and heavy elements have settled from the photosphere toward the centre of the Sun because of gravity. The proportions of heavier elements are unchanged. Heat is transferred outward from the Sun's core by radiation rather than by convection (see Radiative zone below), so the fusion products are not lifted outward by heat; they remain in the core,[56] and gradually an inner core of helium has begun to form that cannot be fused because presently the Sun's core is not hot or dense enough to fuse helium. In the current photosphere, the helium fraction is reduced, and the metallicity is only 84% of what it was in the protostellar phase (before nuclear fusion in the core started). In the future, helium will continue to accumulate in the core, and in about 5 billion years this gradual build-up will eventually cause the Sun to exit the main sequence and become a red giant.[57]

The chemical composition of the photosphere is normally considered representative of the composition of the primordial Solar System.[58] Typically, the solar heavy-element abundances described above are measured both by using spectroscopy of the Sun's photosphere and by measuring abundances in meteorites that have never been heated to melting temperatures. These meteorites are thought to retain the composition of the protostellar Sun and are thus not affected by the settling of heavy elements. The two

  

Core

The core of the Sun extends from the centre to about 20–25% of the solar radius.[60] It has a density of up to 150 g/cm3[61][62] (about 150 times the density of water) and a temperature of close to 15.7 million kelvin (K).[62] By contrast, the Sun's surface temperature is about 5800 K. Recent analysis of SOHO mission data favours the idea that the core is rotating faster than the radiative zone outside it.[60] Through most of the Sun's life, energy has been produced by nuclear fusion in the core region through the proton–proton chain; this process converts hydrogen into helium.[63] Currently, 0.8% of the energy generated in the Sun comes from another sequence of fusion reactions called the CNO cycle; the proportion coming from the CNO cycle is expected to increase as the Sun becomes older and more luminous.[64][65]

The core is the only region of the Sun that produces an appreciable amount of thermal energy through fusion; 99% of the Sun's power is generated in the innermost 24% of its radius, and almost no fusion occurs beyond 30% of the radius. The rest of the Sun is heated by this energy as it is transferred outward through many successive layers, finally to the solar photosphere where it escapes into space through radiation (photons) or advection (massive particles).[66][67] 
                                                                                 

                      

Friday, 11 July 2025

GLOBE AND MAPS


 

                                                                                                                       

MAPS

Representation of Earth or its regions in –

  • Three Dimensions         – Globe
  • Two Dimensions             – Maps
    • Collection of Maps - Atlas
    • Art of making Maps – Cartography

 

Elements of Maps – Represent different information about the area on map.

  • Direction – Compass on map to show direction or Top of the map is North.
  • Colour – Represent physical attributes of the area
    • Brown (Mountains),
    • Yellow (Plateau),
    • Light Blue (Shallow water bodies),
    • Dark Blue (Deep water bodies),
    • Green (Plains).
  • Symbol - Represent specific landmarks in the area.
    • PO (Post Office),
    • PS (Police Station),
    • Cross (Church)
    • Single Line (Regular Road),
    • Two Parallel Lines (National Highway)
    • Single Blue Line (River),
    • Broken Line (Sea Route).
    • Red Cross (Hospital),
    • Pair of students (School)
  • Scale - Ratio between the size of the map and the area shown. 1 cm:100 km means 1 cm on map is equivalent to 100km in actual distance.

 

Types of Maps

  • Political Maps - Shows the boundaries and locations of countries, states, cities, towns. These boundaries and locations are determined by governments rather than nature.
  • Physical Maps - Shows landforms, bodies of water and other geographical features.
  • Road Map - Displays roads and transport links.
  • Thematic Maps - Shows a particular theme connected with a specific geographic area e.g. percentage population change.

 

GLOBE

The Earth’s entire surface is marked by a crisscross of horizontal lines and vertical lines forming a grid.

 

Horizontal Lines (Latitudes or Parallels):-

  • Latitudes are horizontal lines drawn on the globe or map that go round the Earth and run parallel to each other and therefore referred as Parallels.
  • The Latitude at biggest circumference of the Earth is called Equator and is measured as 0 degree.
  • There are 90 degrees of latitude to the North of the Equator called the Northern Hemisphere and 90 degrees of latitude to the South of the Equator called the Southern Hemisphere.
  • There are 181 degrees of latitudes in all. There are 90 degrees in North, 90 degrees in South, and there is the 0°latitude, which is the Equator.
  • The North Pole is the northern-most point on the Earth. It is located in the middle of the Arctic Ocean. The latitude of North Pole is 90°N or north and one end of all the longitude lines meet at the North Pole.
  • The South Pole is the southern-most point on the surface of the Earth. It is situated on the continent of Antarctica. The latitude of South Pole is 90°S or south and another end of all longitude lines meet at the South Pole.
  • North Pole and South Pole lie diametrically opposite each other.
  • The Tropic of Cancer is a line of latitude circling the Earth at 23½° N or north of the Equator.
  • The Tropic of Capricorn is a line of latitude circling the Earth at 23½°S or south of Equator.
  • Arctic Circle is a line of latitude circling the Earth at 66½° N or north of equator.
  • Antarctic Circle is a line of latitude circling the Earth at 66½° S or south of equator.

 

 

Vertical Lines (Longitudes or Meridians):-

  • Longitudes are vertical lines drawn on the globe or map. They form semicircles that run from the North Pole to the South Pole and are also called Meridians.
  • The Longitude running through the Old Royal Observatory at Greenwich near London is marked 0°. It is called the Prime Meridian.
  • There are 180 degrees of longitudes to the East of the Prime Meridian called the Eastern Hemisphere and 180 degrees of longitudes to the West of the Prime Meridian called the Western Hemisphere.
  • There are 360 degrees of longitudes in all. There are 180 degrees in East, 180 degrees in West, and there is the 0°longitude, which is Prime Meridian minus 1 Longitude because the 180°E and 180°W is the same longitude.
  • The 180° East and 180°west longitudes meet and form a single line, in the Pacific Ocean, which is on the opposite side of the Prime Meridian is called the International Date Line.

 

Rotation and Revolution of Earth

Rotation of Earth:-

  • The Earth is tilted at an angle of 23½° from the vertical plane. Axis of the Earth passes through the centre of the Earth from North Pole to the South Pole.
  • The Earth spins on its axis once in 24 hours from west to east thereby causing the Sun to rise in east. This movement is known as rotation.
  • Rotation of the Earth on its axis causes day and night. As the Earth rotates, the side facing the Sun has day and other part facing away from the Sun has night.
  • Rotation of the Earth on its axis causes Tides, which is a rhythmic rise and fall of ocean water twice a day.

 

Revolution of Earth:-

  • While Earth is rotating on its axis, it is also revolving around the Sun. The Earth follows a fixed path called orbit to move around the Sun. This movement is known as revolution.
  • The Earth completes one revolution around the Sun in 365 ¼ days or one year.
  • Leap year has 366 days and its February has 29 days. It falls every 4th year to cover the ¼ day of the previous 3 years so that the revolution of the Earth matches the completion of our calendar year.
  • Revolution of the Earth around the Sun and its tilted axis causes seasons.
  • The hemisphere of the Earth that is tilted towards the Sun gets longer hours of sunlight and has summer season.
  • The hemisphere of the Earth that is tilted away from the Sun has lesser hours of sunlight and has winter season.
  • 21 March and 23 September - The sun is directly overhead the equator and Earth experiences equinox on these two days. 'Equi' means equal and 'nox' means night, so equinox means equal day and night.
  • In March, both the poles are at an equal distance from the Sun. The Northern Hemisphere emerges from winter and has spring and the Southern Hemisphere leaves the summer behind and has autumn.
  • In September, both the poles are at an equal distance from the Sun. The Northern Hemisphere leaves the summer behind and has autumn and the Southern Hemisphere emerges from winter and has spring.
  • 21 June - The Sun is shining directly overhead the Tropic of Cancer and the northern hemisphere is tilted towards the Sun to experience summer solstice in the northern hemisphere. During this time the southern hemisphere experiences winter solstice. This is the longest day in northern hemisphere and the shortest day in the southern hemisphere.
  • 22nd December - The Sun is directly over the Tropic of Capricorn in Southern Hemisphere and tilt of the axis brings the southern Hemisphere closer to the sun to experience summer solstice in the southern hemisphere. During this time the northern hemisphere experiences winter solstice. This is the longest day in southern hemisphere and the shortest day in the northern hemisphere.

 

 

Continents and Oceans

Order of Continents from Largest to Smallest

            Asia

            Africa

            North America

            South America

            Antarctica

            Europe

            Australia

 

Order of Oceans from Largest to Smallest

            Pacific Ocean

            Atlantic Ocean

            Indian Ocean

            Southern Ocean

            Arctic Ocean

 

INTERESTING FACTS

 

The Suez Canal, situated at the coast of Egypt, connects the Mediterranean Sea to the Red Sea saving a sea route of about 9,000Km.

 

North America and South America are joined by the Isthmus of Panama through which the Panama Canal is made saving a sea route of about 15,000 Km.

 

Landlocked seas:-

  • Aral sea is located with boundaries with Uzbekistan, Turkmenistan, Kyrgyzstan and Afganistan.

 

  • Caspian sea is located between Asia and Europe with boundaries with Russia, Iran and Azerbaijan.

 

  • Dead sea is located between Israel, Jordan, Syria and Lebanon.

 

The Sun

                                                                                                                                            ...