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    Home»Geography»GEOGRAPHY: FORM ONE: Topic 2 – THE SOLAR SYSTEM
    Geography

    GEOGRAPHY: FORM ONE: Topic 2 – THE SOLAR SYSTEM

    March 30, 201832 Mins Read
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    TOPIC 2
    THE
    SOLAR SYSTEM
    Solar System is the arrangement of sun, planets and
    other solid objects in the space in relation to the position of the sun. The planets are not arranged in a single
    line from the sun, they are scattered in the space.

    Components of the Solar System

    The
    solar system is made up of the sun, planets, moons, natural satellites,
    asteroids, meteors, comets, dust, ice, and interplanetary space (it contains
    interplanetary dust and interplanetary gas). All planets and other bodies
    revolve around the sun. The sun is the central body of the solar system, and it
    is the only body that generates its own heat. Bodies that revolve around the
    sun are kept in their orbits (paths) by the sun’s powerful force of gravity.

    There
    are eight known planets in the solar system. The planets, starting from the one
    closest to the sun are: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus,
    and Neptune.

    The
    four innermost planets in the solar system, Mercury, Venus, Earth and Mars are
    also called terrestrial planets. They are called terrestrial because they have
    a compact, rocky surface like the Earth’s.

    Jupiter,
    Saturn, Uranus, and Neptune are known as the Jovian (Jupiter-like) planets,
    because they are all gigantic compared with Earth, and they have a gaseous
    nature like Jupiter’s. The Jovian planets are also referred to as the gas
    giants, although some or all of them might have small solid cores.

    Solar System


    Importance of the
    Components of Solar System

    Though
    the solar system has many components, the two most important components of the
    solar system are the Earth and the sun. The Earth sustains lives of a diversity
    of living organisms (plants and animals). The Earth contains numerous resources
    that enable living organisms to thrive in it. The Earth’s atmosphere contains
    water and air (a mixture of several gases that are used by living organisms for
    survival). In general, the Earth is the only planet known to sustain life.
    1.   Mercury
    = 57600,000km
    2.   Venus
    = 107,200,000 km
    3.   Earth
    = 148,800,000km
    4.   Mars
    = 227.200,000km
    5.   Jupiter
    = 772,800,000 km
    6.    Saturn
    = 1,417,600,000km
    7.   Uranus
    = 2,854,400,000 km
    8.   Neptune
    = 4,468,800,000 km


    A. SUN
    Sun is
    the star. It is one among the millions of stars that one sees at night except
    that it looks much bigger because it is closer to the earth than other distant
    stars. The sun is much larger than other distant stars from the earth. In fact
    much larger than all the planets put together. Its diameter is approximately 14
    million kilometers and its mass is approximately 330,000 times greater than
    that of the earth. The elements that form the material of the sun are also in
    different proportion from those of the earth: The sun is composed of
    approximately;
    ·       
    75%
    hydrogen
    ·       
    23% helium
    ·       
    3% of other elements

    The
    earth is relatively cold body but the sun is so hot that nearly all molecules
    are broken into their separate atoms and all are mixed together into a single
    hot gas. Its average surface temperature is about 6000°c, it is much hotter in
    the interior where it is about 14,000,000°c.  



    The sun is the source of all energy that
    supports life on Earth. The sun is responsible for water cycle and it is
    responsible for weather conditions and climate. The moon lights the Earth on
    some days of the month, though it gets its light from the sun.


    The Importance of the Sun

    1. The sun is very important in the plants’
    growth. The sun helps the plants to make their own food by the photosynthesis
    process.

    2. The sun is very necessary for the
    other living organisms, that is, it provides us with light for the vision and
    to do our work.

    3. The sun provides us with the heat to
    warm our bodies.

    4. The sun provides some animals and
    humans (that feed on plants) with food as it helps the plants to make its own
    food by the photosynthesis process.

    5. The sun is used in heating water and
    warming houses by the solar heater which changes the solar energy of the sun
    into the heat energy. The heat energy is used in warming houses and heating
    water.

    6. The sun is very important in the
    formation of the clouds, rain, and winds. The sun evaporates the water in the
    seas, lakes and oceans into water vapour. When the water vapour rises in the
    sky, it cools and condenses forming the clouds, which eventually forms rain.


    B. SOLAR ENERGY

    The sun is the source
    of all energy in the earth. This is called solar energy. Solar energy is the energy produced by the sun

    Uses
    of Solar Energy

    1.  In drying clothes, grains, fruits
    and meat.

    2. Growing plants: – when plants grow they use energy from the sun to manufacture their
    food
    through the process known as
    photosynthesis

    3. Solar energy captured in solar panels and stored in batteries provides electricity used
    in
    generating industrial and home appliances like television,
    refrigerator,
    Oven, electric iron
    and
    cooker.

    4. Many
    everyday items such
    as calculators and other low power consuming devices can be powered by solar energy effectively

    5. Is
    used as a source of
    vitamin D for human being

    6. It
    is used for evaporation of water from
    water bodies which is necessary for rain formation

    Coal
    energy
    is the solar energy
    stored in the bodies of plants grew thousands of years ago which after being barred under the earth for a very long time turned into coal similarly gas and oil formed from died bodies of organic matters which lived thousands of years ago.


    How the use of solar energy promotes
    environmental conservation

    1. Solar
    energy is used by plant during manufacturing its food through the
    photosynthesis. In this process plants take up carbon dioxide from the
    atmosphere and releasing oxygen. In dome so carbon dioxide is removed from the
    atmosphere making the ozone layer safe and more oxygen to be used in
    troposphere by other living organisms.

    2. Moreover,
    Solar energy is clean and safe type of energy suitable for heating and lighting
    this is due to the fact that it does not release soot.

    3. The
    use of solar energy in household’s helps to promote and conceive environment in
    the sense that it would reduce the need for firewood and charcoal, where by
    both once extracted pollute and destroy forest.

    4. The
    use of solar energy also reduces the use of fuel like kerosene as a result it
    helps to reduce environmental pollution caused by smoke from burning fuel.

    5. Formation
    of coal and oil
    :
    Coal is solar energy stored in the bodies of plants that grew thousands of
    years ago, and which after being buried under the Earth for a very long period,
    turned into coal. Similarly, oil was formed from dead bodies of organisms.

    6. Formation
    of rainfall
    :
    Evaporation of water which is necessary for cloud and finally rainfall
    formation also uses solar energy.


    Solar energy in relation to the emancipation of women
    (how solar energy contribute to the emancipation of women)

    1. Helps to reduce the time would
    be consumed used by the women searching firewood from forest.

    2. The use of solar energy
    equipments on cooking makes them to have more time to be involved in money
    making activities such as business or farming.

    3. Through the use of solar
    energy equipments in cooking and other domestic’s tasks, young girls get time
    to go to school and private study as it was to the boys.


    C. PLANETS

    The planets are bodies
    that revolve around the sun.  
    Planets revolve around the sun in
    anticlockwise direction following paths called orbits.
    As they revolve around the sun, they appear to move among the stars. This is
    the reason why the Greeks called them the planets, which in their
    language means “wandering stars”.

    All the light and
    the heat of the planets come from the sun. Hence, the temperatures on the
    planets depend on their relative distances from the sun. All planets revolve
    around the sun in the same direction in orbits that are elliptical and nearly
    in the same plane.

    They
    include:
    1.   Mercury
    2.   Venus
    3.   Earth
    4.   Mars
    5.   Jupiter
    6.   Saturn
    7.   Uranus
    8.   Neptune

    As
    they revolve around the sun they appear to move around the star. That is why
    the Greeks called them planets
    means “Wandering stars”. All planets
    revolve around the sun in the same orbit that are elliptical and nearly the
    same plane.

    The
    time taken to complete an orbit round the sun depends on the distance of the
    planet from the sun. All the light and heat of the planets come from the sun.
    Hence the temperatures on the planet depend on their relative distances from
    the sun.  However, Pluto is not a planet
    because an object to be a planet, it needs to meet these requirements
    (criteria) defined by the International Astronomical Union (IAU) as follows:
    i)            
    It needs to be in orbit around
    the sun
    ii)           
    It needs to have enough to
    pull itself in a spherical shape
    iii)         
    It needs to have “Cleared
    neighborhood of its orbit”

    Note: Any
    object that doesn’t meet these 3 criteria is considered a
    dwarf planet. And so, Pluto is a dwarf
    planet is not a planet.

    PLANETS
    POSITION AND CHARACTERISTICS
    D. COMETS
    Sometimes
    at night one sees objects with leading heads and right
    tail at the sky. These are
    called comets. At present
    many scientists believe that comets are
    composed of ice crystals and fragment matters. Comets revolve around the sun far beyond the limits of
    Pluto. They can be seen from the earth only when they come close to the sun.

    Comet


    E. ASTEROIDS
    Asteroids
    are solid heavenly bodies revolving around the sun mostly between
    the orbits of Mars and Jupiter There are thousands of these, the largest having diameter of less than 800km. These bodies cannot be
    seen without a telescope because they are very far away.

    Asteroid
    F. METEORS
    Meteors
    are process of hard matter falling from
    outer space become visible between
    110 and 145 km above the earth’s
    surface, where as a result of friction with
    the atmosphere become hot and usually
    disintegrate. When they do completely
    disintegrate as they pass through the
    atmosphere reach the earth’s surface and are known as meteorites.

    Meteor and Meteorite


    Meteorites are usually made of nickel, iron or silica
    fragments of disintegrated comets. There are two known meteorites
    in Tanzania one is found in Mbozi District and the other fell at Malampaka in Kwimba District in 1930. Sometimes meteors reach the earth’s surface with such force, hence they make
    large holes or craters. An
    example of such craters in the world is the great meteor crater in
    Arizona desert in United States of America which is 150 meters deep and
    about 1 kilometer width.

    G. SATELLITES
    Satellites are moons of the planets. The number of satellites depends on the nature and size of planet
    up to the moment space researches has proved that only seven planets have satellites.

    H. THE EARTH
    The Earth is the
    third planet from the sun. It is the only planet known to have an atmosphere
    containing free oxygen, oceans of liquid water on its surface, and supports
    life. Earth is the fifth largest of the planets in the solar system, smaller
    than the four gas giants namely Jupiter, Saturn, Uranus and Neptune, but larger
    than the three other rocky planets, Mercury, Mars and Venus.
    We
    live on the planet earth. The Earth
    is made of the;
    ·       
    Atmosphere (air)
    ·       
    Hydrosphere (water bodies)
    ·       
    The crust solid
    ·       
    Molten material
    ·       
    Biosphere (living things)

    About 3/4
    of the earth’s surface is covered by water. In fact no other planet in the
    solar system is known to have water bodies, the shape of the earth is a
    flattened sphere This flattening is very slight as indicated by measurements in
    diameters through poles and at the equator. The diameter through the poles is
    12,713 km while at the equator it is 12,757 km. 

    The Shape of the Earth and
    its Evidence

    The
    Earth is not perfectly round. Its shape is an oblate
    spheroid
    which is a flattened sphere. The flattening is very slight
    at the poles than at the equator.
    There are some several
    evidences, which are used to prove that the earth is sphere like structure,
    some of them are shown in the following: 

    (i) SUNRISE AND
    SUNSET
    The
    sunrise and sunset at different places of the earth, people in the east see the
    sun earlier than the people in the west due to earth’s rotation from west to
    east. If the earth was flat the whole world would have sunrise and sunset at
    the same time. 
    Spherical earth and Flat
    earth

    (ii)
    CIRCUMNAVIGATION OF THE EARTH
    If
    traveling from a certain point of the earth and you go straight around the
    earth you will come to the point of origin. The first traveler around the world
    named Magellan in 1519 – 1522 proved this; image did not encounter abrupt edge
    over the world in his voyage. 

    Circumnavigation of the Earth 
    (iii)
    AERIAL PHOTOGRAPHS
    Photographs
    taken by satellites or aeroplane from the air show that the earth has a curved
    or round shape

    Aerial Photographs 

    (iv)
    SHIP’S VISIBILITY
    If you
    are in the coast viewing a ship which is very far you will see the soot, then the pipe and eventually the whole ship
    gradually appears. If the earth were flat the ship would have been seen all at once 

    Spherical Earth and Flat Earth


    (v) LUNAR ECLIPSE

    The
    shadow of the earth thrown to the moon during lunar eclipse is always round.
    Only a spherical object can give a circular shadow.  
     

    lunar eclipse


    THE MOON
    The
    moon is a natural satellite of the earth It has a solid spherical body with a
    diameter of 3456 kilometers. The distance from the earth to the moon is a
    384,403 kilometers. The moon takes 129 ½ days to make a complete revolution
    around the earth.

    The
    moon appears to rise in the east and set in the west because the earth spins
    from west to
    east.  Among all planets only the
    earth sustains life due to its position from the sun. It is not very close or
    very far from the sun. Other body such as Pluto which is very far from the sun
    does not sustain life because it is very cold. Likewise Mercury which is very close
    to the sun does not sustain life because it is very hot.


    EARTH’S MOVEMENT
    The earth is in motion all the time. One does not feel this motion because one moves with it, like all other planets, the earth has two motions known as: –
    (a) Rotation
    (b) Revolution

    ROTATION
    Rotation refers to the spinning of a body on
    its axis. The Earth rotates or spins on its axis in an anti-clockwise
    direction, from West to East through 360 degrees. It makes one complete
    rotation in 24 hours. Thus, for every 15 degrees of rotation, the Earth takes
    one hour which is the same as four minutes for every 1 degree.

    An axis is an imaginary line joining the N
    (North) and S (South) poles through the centre of the Earth.


    The
    rotation of the Earth is very rapid although it is difficult to feel its
    motion. At the equator, every point of the Earth’s surface is travelling
    eastwards at about 1600 km per hour. At latitude 40 degrees, the speed is about
    1280 km per hr. The Earth’s axis makes an angle of 66 ½ degrees with the plane
    of its orbit. In other words, the axis is tilted 23 ½ degrees from the
    perpendicular.

    Rotation of the Earth

    It
    makes one complete rotation after every twenty four hours or one day.

    The
    following observations illustrates the earth’s rotation from west to east.

    1. When
    traveling in a fast moving vehicle we notice trees and other objects on both
    sides of the road moving in the opposite direction. This observation is similar
    to the movement of the earth’s rotation to the sun.

    2. At
    night most of the stars appear to move across the sky from east to west. This
    shows that the earth is moving from west to east.

    3. Sunrise and sunset: the sun rises
    over the eastern horizon in the morning and sets over the western horizon in the
    evening. But since the sun is in the centre of the solar system and the fact
    that it does not move, this shows that the point of observation (the Earth) is
    moving by rotation from West to East.

    4. Day and Night: During the Earth’s
    rotations some regions face the sun while others do not face it. The regions
    facing the sun experience day time whereas the regions which are not facing the
    sun are in darkness (night). If the Earth was not rotating, one half of the
    Earth would be having daylight while the other half would be in total darkness
    forever. The occurrence of day and night proves that the Earth is rotating.

    5. Photographs of the Earth taken from
    the satellite at different times of the day show that different parts of the
    Earth experience daylight at different times. If the Earth was not rotating,
    different photographs taken at any time of the day would all look alike.

    Day
    and night

    Significances of Earth’s Rotation

    The
    rotation of the Earth is very important because it causes the following
    phenomena:

    1. Alternation of day and night: Rotation of the Earth causes the
    side of the Earth which face the sun to experience daylight which is the day,
    whereas the side that is not facing the sun at that time will be in darkness
    (night). This ensures that, at any time of the day, one half of the Earth is in
    darkness and the other is in daylight. If the Earth did not rotate then its one
    half would be in daylight while the other half would be in darkness all the
    year round.

    2. Occurrence of tides: Tides are the periodic rise and
    fall of sea levels caused by the combined effects of the gravitational forces
    exerted by the moon and the sun on the rotating Earth.

    3. Deflection of winds and ocean currents: As the Earth rotates on its axis
    from West to East, winds and ocean currents flowing over the Earth’s surface
    are deflected. The anticlockwise rotation of the Earth deflects prevailing
    winds to the right in the northern hemisphere and to the left in the southern
    hemisphere.

    4. Time difference between longitudes: The rotation is responsible for the
    difference in time between different places on Earth. It causes the difference
    of one hour in every 15 degree interval between longitudes, which is equivalent
    to 4 minutes for each degree of longitude.

    Deflection of winds and ocean
    currents

    REVOLUTION
    Is the movement of one body around another.
    Earth’s revolution:–
    ·       
    Is
    the
    movement of the earth around the
    sun
    ·       
    The
    earth
    takes 365
    1/4 days for a complete revolution
    ·       When the earth takes 366 days
    to accomplish one revolution is
    called a Leap year
    ·       
    The
    earth
    revolution revolve around the sun in
    an elliptical
    ·       Due to the shape of the earth’s orbit, the earth is very closer
    to the sun one point of the year
    than at another


    APHELION AND PERIHELION

    Aphelion is
    the furthest position of the
    earth’s orbit from the sun
    – The earth is at Aphelion each
    year on
    4th July when
    it is in 152 million kilometers from the sun.

    Perihelion is the nearest position
    of the earth from the sun
    – The earth is at perihelion
    each rear on 3
    rd January when it is 147.3 million kilometers from
    the sun.
    Therefore the speed of
    revolution is about 29.66 km per second. 
                             Earth Revolution
    The Effects
    of Earth’s R
    evolution

    The revolution of
    the Earth around the sun and the inclination (tilting) of its axis results in
    the following:

    1. The
    four seasons of the year, namely summer, autumn, winter and spring. A season is
    one of the distinct periods into which the year may be divided.

    2. Change
    in the altitude of the midday sun at different times of the year at any place.

    3. Varying
    lengths of the day and night at different times of the year. The axis of the
    Earth is inclined to its elliptical plane at an angle of 66.5 degrees. If the
    axis of the Earth was vertical, the sun rays would always be overhead at the
    Equator, thus all places on the Earth would always experience 12 hours of
    daylight (day) and 12 hours of darkness (night).

    4. The
    eclipses (eclipse of the sun and eclipse of the moon).


    SEASONS

    Season
    is one of the four periods of the
    year separated from each other by different
    temperature conditions The seasons are
    summer, autumn, winter and spring They are more pronounced between 23°c and 66°c of latitudes At the equator the year
    is divided between hot and wet seasons while at the poles is very cold all the year around and the season cannot
    be identified easily.

    The
    Northern hemisphere summer months are May, June and July. Autumn months are August,
    September and October; Winter Months are November, December and January while spring months are February, March and April. In the Southern Hemisphere
    summer months are November, December and January, autumn months are February, March and April Winter has May, June and July while spring
    months
    are August, September and
    October.

    CAUSE
    OF SEASONS
    Seasons
    are caused by inclination of the earth’s
    axis and the earth’s revolution around the sun The earth’s axis is tilted at an angle of 660 to the earth’s
    orbital plane and it is always pointing
    to the
    same direction in space.
    In its
    revolution around the sun
    one of the hemispheres is inclined towards the sun to one period of the year
    and away from it at another period of the year.
    Seasons of the year
    ECLIPSE

    This is the movement
    of one heavily body between the two others, such that it casts shadow over the other. The eclipse involves three heavily bodies namely; the Sun, the Earth and the Moon. So long as the sun is the central both- of the solar system, it never moves, only the earth and the moon are in the motion all the time.

    An eclipse is said to be total eclipse when the
    whole body is
    obscured i.e completely blocked from the sunlight and it is described as a partial eclipse when the only part of the body becomes obscured. At any place an eclipse will last short time,
    hardly seven minutes because both the earth
    and the moon are in motion.

    Types of Eclipse
    There
    are two types of eclipse
    i.e Lunar
    eclipse and solar eclipse

    1. LUNAR ECLIPSE (ECLIPSE OF THE MOON)
    This
    occurs when the earth moves between the sun and the moon, this casting its shadow over the moon. 

    Lunar Eclipse
    2. THE SOLAR ECLIPSE
    The solar eclipse is also known as
    the eclipse of the
    sun.
    This occurs
    when the moon passes between the
    earth and the sun casting its shadow over the earth.

    Solar Eclipse

    – Umbra or total
    eclipse is when the whole body is obscured i.e completely blocked from the
    sun’s light.
    – Penumbra or partial eclipse is when only part of the body becomes obscured.


    THE APPARENT MOVEMENT OF THE OVERHEAD SUN

    The apparent movement
    of the overhead sun is related to the different positions of the earth
    on its movement as it revolves around the sun. The overhead
    sun appears to move northwards and
    south wards in an osculating
    (swinging) manner.

    However
    the overhead sun’s northward limit is latitude 23°N People beyond this latitude never see the sun vertically above their head.
    The latitudes 23°N is known as Tropical
    of cancer.
    Similarly the overhead sun ends
    23°S in its apparent Southward movement. This latitude is known as the Tropic of Capricorn on 2l June the sun is vertically
    overhead on the Tropical of cancer.
    This is known as the summer
    solstice in the Northern hemisphere.

    On 22nd December the sun is vertically
    overhead on the Tropic of Capricorn this is the winter solstice in the Northern Hemisphere.

    Solstice means equal night or
    is when the sun on these days appears to stand still between its northward and
    southward journeys.                  



    THE SOLSTICES
    The sun is overhead twice a year
    at the equators 21st March
    and 23rd September. 21st March is known as the spring equinox and
    23rd September is known as
    the autumn equinox in the Northern Hemisphere.  Equinox means
    equal nights, at equinox the length of day and night is equal over all places on the earth’s surface. Viewed from the Southern Hemisphere the solstices and the equinoxes are reversed.

    LENGTH OF DAY AND SIGHT
    Places
    along the equator experience equal day and night all the year, but northwards
    or south wards towards the poles. The length of day and night varies
    with latitudes. For instance in
    Northern Summer when the Northern Hemisphere is inclined towards the sun, days are longer than nights. However at latitude 66°N known as the Arctic. Cycle and beyond
    the sun appears around the sky without
    setting in the North Pole daylight is experienced
    for six months before the sunset.

    Then this region remains in
    darkness for the next six months; Latitude 66° south is known as the Antarctic cycle. The Polar
    Regions south of the Antarctic cycle experience the long six months night from March to September and the six months day light from October to February.


    PARALLELS AND MERIDIANS

    Parallels
    are more commonly known as latitudes.
    Latitude refers to the angular distance North or South
    of the equator calibrated in degrees, minutes and seconds, measured from the
    centre of the Earth
    . The equator is given a value of 0º. It is an
    imaginary line which divides the Earth into two hemispheres (northern
    hemisphere and southern hemisphere). The Northern hemisphere has latitude of
    90ºN and the Southern hemisphere has latitude of 90ºS. All other latitudes are
    drawn north or south, parallel to the equator. A particular latitude, say 60ºN
    joins all points on the surface of the Earth which make an angle of 60º from
    the centre of the Earth (the equator). Any circle drawn around the Earth,
    parallel to the equator, is a parallel of latitude. Table 1.3 shows important
    parallels and figure 1.18 shows the location of these parallels on the Earth’s
    surface.

    Latitude
    Parallel
    Meridians are commonly known as longitudes.
    A longitude is an imaginary line drawn on the map from the North Pole to the
    South Pole. Meridians are numbered in degrees East or West of longitude 0°,
    called Greenwich Meridian (because it passes through a town in England
    called Greenwich). It is also known as the Prime Meridian because it is
    the line of reference from which all other meridians are established.

    A
    longitude, therefore,
    refers to angular distance measured in degrees East and West of the Greenwich
    Meridian
    . The Prime Meridian runs through the poles and the
    Greenwich observatory near London. All lines of longitude are in equal length
    and divide the Earth into two equal semi circles. There are 360° in a circle,
    with 180° lying east of the Greenwich Meridian and the other 180° west of
    Greenwich.

    The
    Greenwich line has been chosen by convention (meaning that any other line could
    have served the same purpose).

    Longitude/Meridian: Is angular distance measured in degrees East or west of the prime meridian, the run from north to south. 
    Longitudes and Latitudes 




    The importance
    of parallel and meridians

    Longitudes and
    latitudes are very important to any geographer or map reader. The importance of
    longitudes and latitudes include the following:

    1. They
    are used by pilots and sailors to guide their paths as they steer the planes
    and ships.

    2. When
    used together, longitude and latitude define a specific location through
    geographical coordinates (Fig 1.23).Each location on Earth has its unique
    latitude and longitude. For example, the location of a point shown on figure
    1.23 below is 40°N,60°W.

    3. Longitudes
    enable geographers to calculate the local time of a place, X, given the local
    time and longitude of place Y, as the point of reference.. 

    4. Latitudes
    are used as a guide to explain the variation in climate on the surface of the
    Earth. It is generally known that places along the equatorial belt experience a
    hot and wet climate for most of the year. As you move north or south of the
    equator, the climate progressively become cold. Places at the north and south
    poles are extremely cold and are covered by ice and snow throughout the year.

    LATITUDE AND LONGITUDE

    Latitude:  Is the angular
    distance north or south of the equator measured in degrees,
    minutes and seconds. Also can be
    defined as the lines drawn on a map from east to west.

    – The
    equator is latitude of
    0°
    – The
    equator divides the earth into two
    equal parts (Hemisphere)
    –  The
    hemisphere north of the
    equator is northern hemisphere
    –  The
    hemisphere south of the equator is
    known as Southern hemisphere
    – Latitude
    are also known as a
    parallel lines of equator
    because they never meet.
    – The lines of latitude are
    measured from 0° (the equator) to 90° north and south.


    Lines of Latitude are;
    ·       
    The equator 0°
    ·       
    The tropical of cancer 231/2°N
    ·       
    The Tropical of Capricorn 231/2°S
    ·       
    Arctic cycle 661/2°N
    ·       
    Antarctic cycle 661/2°S
    PARALLEL
    OF
    LATITUDE
    30°N 
    Longitude
    Is an
    angular distance measured in degrees east or west of the prime meridian, they
    run from north to south.

    Greenwich is a longitude 0°. It is also
    known as prime meridian. The prime meridian is the line running through the
    poles (North and South) and is known as Greenwich 0°. Longitudes are measured
    from 0° to 180° East or West of Greenwich, all meridians are passing through
    the North and south poles. 

    LONGTUDE  AND TIME

    The
    earth rotates on its own axis from west to east once every twenty-four hours
    (one day). This means that the earth turns through 360° in twenty-four hours.
    All places along a given meridian will experience midday along the same
    meridian, it is known as Local Mean, on the Greenwich meridian is known as
    Local Mean Time (LMT).

    When
    it is 12:00 noon; on the Greenwich meridian it will be 1:00 pm at a place of
    15°E or 11:00 at a place of 15°W. To
    find time for example
    for Musoma
    in Tanzania (34
    °) when it is 12:00 in Kinshasa Zaire
    1.  
    Note
    the 1onitude position of Kinshasa 15°
    30°E and Musoma 34°
    2.  
    Find
    the difference in
    degree of longitude between Kinshasa and Zaire 34°­ 15°30 = l81/2
    3.   Find the difference in time between
    Kinshasa and Zaire


    4.   Since
    Musoma is to the east of Kinshasa,  Musoma time will be ahead of that
    of Kinshasa by 1 hour and
    14 minutes therefore time for Musoma will be 12:00 + 1:14 =
    13:14 pm Or 1:14 pm.

    In the other hand given the time difference between two places and the longitude of one of them,
    one can calculate the longitude position
    of the second places Kinshasa 15° 30° and 1 hour and 14
    minutes. Behind the time of Musoma.

    Find the longitude position of Musoma
    Difference in time between Musoma and Kinshansa 1
    hour and 14 minutes.
    Difference
    in degrees of longitude between Musoma and Kinshansa is lhr and 14 minutes =
    74/4 or 18°30°


    Since
    the time of Kinshasa is behind that of Musoma, Musoina must be east of
    Kinshansa. Therefore the longitudinal position of Musoma will be 15°30´ +
    18°30´ = 34°E.

    GREAT CIRCLE
    The
    intersection of the surface of a sphere
    and a plane through its centers for example meridians of
    longitude and equator e great circle in the earth’s surface. Therefore
    there is no limit to the number of
    great circle that can be drawn. 
    Great Circle
    Great circle also is a circle drawn
    on a globe (or other sphere) with a center that includes the center of the globe. Thus a great circle divides the
    globe into two equal halves.


    IMPORTANCE
    OF GREAT CIRCLE
    1. The
    great circles are important for
    aero planes which use them as route ways to guide their path
    2. Great circles are important for ship to follow routes along great
    circles


    TIME
    Refers
    to a period that is used for a event or activity. It is measured in seconds,
    minutes, hours, days, months or years.

    TIME ZONES
    Is the
    region having the same standard time, Standard time is common on time for all
    countries belonging to the same time zone for example; Tanzania, Kenya, Uganda,
    Ethiopia, Djibouti and Somalia use the same standard time. This is commonly
    referred to the East African Standard time.

    There
    would be problems of telling time if every place had its own time set according
    to local mean time. For example, there would be great confusion in railway and
    airway timetable or in radio programs if they had to show difference time each
    one place within a small area. To avoid this problem, different stretches of
    land take their time from great Meridian. The time adopted is known as STANDARD TIME.

    In
    East Africa, standard time is taken from meridian of 45ºE when a whole stretch
    of land keeps to the same standard time that stretches from a time zone.
    Therefore time zone refers to a stretch of land where standard time is accepted
    through out a longitudinal zone 15° width. Countries with large stretches of
    land have several standard time zones. There are 24 time zones in the world.
    The Greenwich Meridian is the starting point for dividing the globe into 24
    time zones, the standard time for Greenwich is known as the 

    Greenwich Mean Time (GMT)
    Essence of Time Zone
    In a certain place there could be a place
    on the surface using its’ own
    local time. This would brought a lot of confusion example every radio station would have to announce different times for every
    region within the same country: Local time
    of Bukoba would be different from that of Dodoma.

    – The above confusion was avoid when it was internationally agreed to split the world into 24 time zone according to Longitudes

    – The
    longitudinal
    division across the earth with an approximates
    with of 15 of longitude which is regular across the oceans.

    – Each
    time zone has a standard
    time which is the time of the longitude (meridian near the center of time zone. In the same way, all countries belonging to the same time zone
    have common time.

    Note: Large
    countries like Canada, USA
    and
    Russia have different standard times for
    different regions within them because they are crossed by many time zone.

    Exercise
    5

    1.  If
    it
    is 9:30 am at
    Kasse 33°15°E what time is in
    Zanzibar 45°15°E?

    2.   Find
    the time for the Youncle 30°w if it
    is 12.00 noon London 


    3.   When
    it is 3.30 pm at Nairobi (25°E) what
    is the time for Comoro 120°E?
    INTERNATIONAL DATE LINE.

    The
    line where date is changed or where the calendar day begins. 


    One
    travels eastwards and cross the date
    line, one will gain a day, if one
    travels westwards and cross the date line, one will lose a
    day, if Greenwich it is noon on
    Tuesday a place 90°W would be 10 am on
    Tuesday, at a place 180°W it would be midnight Monday. On the other hand a place 90°E would be 6.00pm on Tuesday and at a place 180°E would be midnight on Tuesday. 
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