EFTA00281229.pdf
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Introduction
Parsons The New School for Design
School of Constructed Environments
Interior Design (AAS)
Environmental Design
PAID 1028-X1
SP-17
Hikida
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Learning Objectives
• At the end of this presentation you should learn basic facts about:
• Water: composition, states, and ability to seek its own level
• Air (atmosphere): cause, and how to measure: direction and speed
• Fire (energy and light): requirements, types of fuels, and temperature of a
candle
• The Sun: size, composition, and distance to Earth
• You should be able to use a sun chart identi the position of the sun at any
time anywhere in the world.
• The Earth: age, size, location in the solar system, and composition
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Elements
• Water
• Air
• Fire
• Earth
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Water Facts
H2O: Water is composed of 2
hydrogen molecules bonded to 1
oxygen molecule
Three states: solid (at 0° C or 32° F),
liquid, gas (around 100 °C or
212 °F)
Water seeks it own level
Example: New York City reservoirs
and wooden water tanks
Capillary action
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Wind Facts
Wind is the flow of gases, here on
Earth it refers to the movement of
air.
It is caused by differences in air
pressure. Air rushes from high
pressure areas to lower ones.
Wind direction is given by the
direction from which the wind
comes.
Anemometers are used to measure
wind speed.
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Fire Facts
Fire is a chemical reaction that
releases light and heat.
Fires require fuel, oxygen and heat
to burn.
Different types of fuel include coal,
oil and wood.
Flames are the part of a fire which
we can see, they can be dWerent
colors, depending on the substance
which is burning.
A candle flame typically burns at
around 1000 degrees Celsius (1800
Fahrenheit).
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Sun Facts
1. Earth-Sun Distance: 150 million
km (93 million miles)
2. Elemental Composition of Sun:
74% Hydrogen, 25% Helium, 1%
other (by mass).
3. Solar Luminosity: — 4 x 1033
erg/s. [As bright as 4 trillion
trillion 100-watt light bulbs]
4. Age of Sun: 4.5 billion years.
5. The sun rises in the east, and sets
in the west.
6. In the northern hemisphere the
sun traverses the southern sky.
7. In the southern hemisphere the
sun traverses the northern sky.
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summer solstice (June 21)
Summer Solstice
The summer solstice is the date
(usually June 20 or 21) when all
places in the northern hemisphere
receive the most hours of daylight in
the whole year. This is because the
earth is tilted on an angle of 23.5
degrees away from being up and
down (measured from the flat plane
created by its orbit around the sun).
N
polar day (6 months of day)
z
Arctic Circle (66.5° N)
24 hours of daylight
Tropic of Cancer (23.5° N)
13.5 hours of daylight
Equator (0°)
12 hours of daylight
Tropic of Capricorn (23.5° 5)
10.5 hours of daylight
Antarctic Circle (66.5° S)
0 hours of daylight
polar night (6 months of night)
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winter solstice (December 21)
Winter Solstice
The winter solstice is also known as
the "shortest day of the year". This
usually happens on December 21st
or 22nd in the Northern hemisphere,
and June 20th or 21st in the
Southern hemisphere.
During the northern hemisphere's
winter solstice (December 21 or 22),
the sun sits directly overhead of the
Tropic of Capricorn at noon, and
places at this latitude have their
shortest night of the year
polar night (6 months of night)
Arctic Circle (66.5° N)
24 hours of darkness
Tropic of Cancer (23.5° N)
13.5 hours of darkness
Equator (0°)
12 hours of darkness
Tropic of Capricorn (23.5° S)
-----------
10.5 hours of darkness
polar day (6 months of day)
Antarctic Circle (66.5° S)
0 hours of darkness A
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Earth Axis
i
Equinox
An equinox occurs twice a year,
around 20 March and 22 September.
The word itself has several related
definitions. The oldest meaning is
the day when daytime and night are
of approximately equal duration.
The word equinox comes from this
definition, derived from the Latin
aequus (equal) and nox (night).
Arctic Circle
Tropic of Cancer
Equator
Tropic of Capricorn
Antarctic Circle
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X70'
N
1706
New York Sun Diagram
New York is at approximately 41-
degrees north latitude.
Month is in Roman numerals
Time is shown in Arabic numerals
East-West axis, North-South axis are
shown.
Degrees on the horizon begin with
0-degrees at due south.
Angle in the sky is indicated along
the lines radiating from the center of
the diagram.
(e) 40°N LATITUDE
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11 O.
N
/70.
New York Sun Diagram
Example:
Where is the sun located in New
York at 6:00 PM on May 25?
1.
Month May is Roman numeral
V.
2.
Follow the curve to 6:00 PM.
3.
The sun position on the horizon
is between 110-degrees and
110-degrees West of due South.
4.
The sun angle is approximately
12-degrees above the horizon.
Question:
Where is the sun located in New
York at 9:00 AM on October 15?
o--
(e) 40°N LATITUDE
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Earth Facts (1 of 3)
1. The Earth was formed 4.6 billion
years ago.
2. The Earth is the third planet from
the Sun.
3. The Earth orbits the Sun once
every 365.27 days and the
orbital speed the Earth travels is
averaged at 107,000 km/h.
4. The Earth has one satellite, the
Moon.
5. The surface of the Earth is 70%
water and 30% land.
6. The circumference of Earth
around the equator is 24,901
miles.
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Earth Facts (2 of 3)
1. The earth is made from the
following materials — 32.1%
iron, 30.1% oxygen, 15.1%
silicon, and 13.9% magnesium.
2. The Earth core is made up of
88% iron, and the temperature
can reach 3,000 degrees C.
3. The atmosphere on Earth is
composed largely of nitrogen
(78%) and oxygen (21%) with
trace elements of other gases.
4. The troposphere is the region in
the atmosphere 12km above the
surface of the Earth. It is in the
troposphere that all of our
weather takes place.
lit
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Earth Facts (3 of 3)
I. Approximately 25km above the
surface of the Earth is the ozone
layer. This is a layer of ozone
that protects the Earth flOn1 the
Sun's harmful ultraviolet
radiation.
2. The atmosphere extends as far as
500 km and the Earth's magnetic
field stretches as far as 100,000
km.
3. The magnetic field is essential
because it protects us from the
Suns solar winds.
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Earth's tilt
1. The earth tilts 23.5 degrees on its
axis as it rotates around the sun.
Winter
Solstice
Earth's Seasons
Autumnal Equinox
Autumn
Winter
Summer
Vernal Equinox
Spring
/
Summer
Solstice
timeanddate.com 2013
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Earth's Magnetic Field
The gravity of Earth, which is
denoted by g, refers to the
acceleration that the Earth imparts
to objects on or near its surface due
to gravity. In SI units this
acceleration is measured in meters
per second squared (in symbols,
m/s2 or m•s-2) or equivalently in
newtons per kilogram (N/kg or
N•kg— 1). It has an approximate
value of 9.81 m/s2, which means
that, ignoring the effects of air
resistance, the speed of an object
falling freely near the Earth's
surface will increase by about 9.81
meters (32.2 ft) per second every
second. This quantity is sometimes
referred to informally as little g (in
contrast, the gravitational constant
G is referred to as big G).
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Sources
• http://ds9.ssl.berkeley.edu/solarweek/MONDAY/facts.html
• http://www.8planets.co.uk/facts-about-earth
.
solstice.html
.
solstice.html
.
Equinox/
• http://en.wikipedia.org/wiki/Equinox
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Sources (continued)
• http://en.wikipedia.org/wiki/Gravity_of Earth
•
• hap ://hendrix2.uoregon.edui—imamura/1 02/images/pascalvases.jpg
• http://www.sciencekids.co.nz/sciencefacts/weather/wind.html
• http://www.sciencekids.co.nz/sciencefacts/fire.html
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| Filename | EFTA00281229.pdf |
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| OCR Confidence | 85.0% |
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| Text Length | 7,860 characters |
| Indexed | 2026-02-11T12:47:31.863777 |