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Kate L

Wind Energy Institute of Canada, North Cape PEI Canada on Flickr - Photo Sharing! - 0 views

shared by Kate L on 08 Dec 08 - Cached
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    Description: The WEICan facility at the North Cape is used to conduct wind energy research and test wind technologies. Various scales and styles of wind turbines can be seen from the trail that runs along the bluffs above the Gulf of St. Lawrence, in addition to the ocean view. The site includes an interpretative visitor center and a historic lighthouse. Photo Taken: July 2005.
Kate L

Wind Energy - A New Kind of Power Generation in Panama on Flickr - Photo Sharing! - 0 views

shared by Kate L on 08 Dec 08 - Cached
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    Two large companies are developing wind energy fields in Panama. This green, clean energy will create a new source of energy for a new generation, even providing surplus energy for surrounding countries. One development, Los Pozos will have its OWN wind generation system. This will be the first green community in Panama, and will in fact create surplus energy to benefit surrounding areas. Contact ThinkPanama.com for more information.
Kate L

Grolier Multimedia Encyclopedia - 0 views

  • basic laws of physics dictate that energy is conserved and can only be changed from one form to another or into matter.
  • Fuel, on the other hand, is the accumulation of matter and therefore represents a store of energy.
  • released in the form of heat when the fuel is burned in chemical or nuclear reactions
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  • cannot be reversed to regenerate the original fuel mass
  • a fuel problem does exist
  • If the supply of fuel is finite, not only will there be no energy supply when the fuel is exhausted
    • Kate L
       
      Finite means: a form of a verb that can occur as the head of a sentence. In Sam wants to leave, wants is finite, leave is non-finite.
  • all other processes that depend on it will cease
  • Several factors combine to make the problem an urgent one
  • World population
  • demand for energy will also increase
  • coal, oil (petroleum), natural gas, uranium, and fuel wood—is limited and insufficient to sustain rapid rates of development.
  • debate about the exact length of time available before the effects of a worldwide shortage become apparent
  • shortage will occur.
  • geothermal energy, hydroelectric power, peat, ocean thermal energy, solar energy, tidal energy, wind power, and fuel wood.
  • replenish themselves naturally in a relatively short time and will therefore always be available.
  • Renewable energy resources
  • indirectly responsible for many other renewable energy sources.
  • ocean currents and winds are results of the uneven distribution of solar radiation over the Earth's surface
  • winds in turn produce waves whose energy can be utilized
  • windmills and wind power
  • ocean thermal energy, solar heating of the upper layers of the ocean produces temperature gradients that can be harnessed to generate electricity
  • Sun also powers the hydrologic cycle, in which ocean water is evaporated, transported over the continents, and precipitated as rain or snow to form rivers
  • flow energy produces hydroelectric power.
  • energy locked in such renewable fuel sources as wood and peat is derived from the Sun by the process of photosynthesis.
  • renewable energy source is geothermal energy
  • arises through the leakage of heat from the Earth's interior to the surface
  • over the entire surface of the Earth at a very low average rate, leakage is much higher in certain locations.
  • Yellowstone National Park
  • Iceland, Italy, and New Zealand.
  • possible to tap the heat and use it for human purposes.
  • Nonrenewable resources originate from two processes: (1) photosynthesis, which occurred many millions of years ago, followed by the fossilization of the plant and animal life that resulted, and (2) the formation of the Earth itself.
  • fossil fuels—coal, oil (petroleum), and natural gas;
  • produced the fuels for nuclear energy, such as uranium for fission and lighter elements for fusion
  • irreplaceable fuels represent an energy capital that must be invested wisely.
  • A cleaner-burning fuel than oil, natural gas seemed to be in abundant supply at the turn of the 21st century and, with the greatly enlarged network of gas pipelines, was rapidly growing in use.
  • nearly total dependence on fossil fuels and hydroelectricity ensures that efforts to solve energy problems by switching to alternative sources will have to overcome a great deal of inertia, both economic and psychological.
  • sources as solar power, wind power, and synthetic fuels suffer from the serious drawback that few major installations now exist.
  • handicapped by the engineering problems of converting the energy to a form useful to human beings.
  • solar energy reaches the top of the atmosphere in amounts 10,000 times greater than all human production of energy, it reaches the Earth's surface at rates of only about 80 to 250 W/m2, and considerably less on cloudy days.
  • arge-scale system based on solar-collector panels will be physically huge, causing problems of maintenance and land use
  • Wind power, wave power, and ocean-thermal-generation sources suffer from similar difficulties
    • Kate L
       
      Even though there are some difficulties with working towards the alternative fuels, it may prove to be more efficient for smaller things (heat and power to small communities or single buildings) in the long run
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    Energy Problem
Kate L

American Wind Energy Association - 0 views

shared by Kate L on 05 Dec 08 - Cached
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    wind energy
will sylvester

Yellowstone National Park Vacation and Tour, Wyoming | GORP - 0 views

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    Ski among Geysers Skinny-skiing Yellowstone is one of the premier winter-wilderness experiences in North America. To glide along the abandoned, snow-covered trails of the Old Faithful area in winter is to enter bottomless silences and watch tendrils of steam writhing in the chill wind. The geysers occasionally roar and billow, and buffalo use their massive heads to clear the frozen grasslands of snow. Accessible only by snow coach in winter, the rebuilt Old Faithful Snow Lodge makes a cozy backcountry base camp. Joining a naturalist-led ski trip offers rare and delightful insight into a world that only seems dormant; some of the best trips are run through the Yellowstone Institute.
cory delacruz

Blue Sky - Why is the Sky Blue? - 0 views

  • end of the spectrum are the reds and oranges. These gradually shade into yellow, green, blue, indigo and violet. The colors have different wavelengths, frequencies, and energies. Violet has the shortest wavelength in the visible spectrum. That means it has the highest frequency and energy. Red has the longest wavelength, and lowest frequency and energy. LIGHT IN THE AIR Light travels through space in a straight line as long as nothing disturbs it. As light moves through the atmosphere, it continues to go straight until it bumps into a bit of dust or a gas molecule. Then what happens to the light depends on its wave length and the size of the thing it hits. Dust particles and water droplets are much larger than the wavelength of visible light. When light hits these large particles, it gets reflected, or bounced off, in different directions. The different colors of light are all reflected by the particle in the same way. The reflected light appears white because it still contains all of the same colors. Gas molecules are smaller than the wavelength of visible light. If light bumps into them, it acts differently. When light hits a gas molecule, some of it may get absorbed. After awhile, the molecule radiates (releases, or gives off) the light in a different direction. The color that is radiated is the same color that was absorbed. The different colors of light are affected differently. All of the co
  • d after Lord John Rayleigh, an English physicist, who first described it in the 1870's.) WHY IS THE SKY BLUE? The blue color of the sky is due to Rayleigh scattering. As light moves through the atmosphere, most of the longer wavelengths pass straight through. Little of the red, orange and yellow light is affected by t
  • As you look closer to the horizon, the sky appears much paler in color. To reach you, the scattered blue light must pass through more air. Some of it gets scattered away again in other directions. Less blue light reaches your eyes. The color of the sky near the horizon appears paler or white.
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  • THE BLACK SKY AND WHITE SUN On Earth, the sun appears yellow. If you were out in space, or on the moon, the sun would look white. In space, there is no atmosphere to scatter the sun's light. On Earth, some of the shorter wavelength light (the blues and violets) are removed from the direct rays of the sun by scattering. The remaining colors together appear yellow. Also, out in space, the sky looks dark and black, instead of blue. This is because there is no atmosphere. There is no scattered light to reach your eyes. WHY IS THE SUNSET RED? As the sun begins to set, the light must travel farther through the atmosphere before it gets to you. More of the light is reflected and scattered. As less reaches you directly, the sun appears less
  • The sky around the setting sun may take on many colors. The most spectacular shows occur when the air contains many small particles of dust or water. These particles reflect light in all directions. Then, as some of the light heads towards you, different amounts of the shorter wavelength colors are scattered out. You see the longer wavelengths, and the sky appears red, pink or orange.
  • RE ABOUT:THE ATMOSPHERE WHAT IS THE ATMOSPHERE? The atmosphere is the mixture of gases and other materials that surround the Earth in a thin, mostly transparent shell. It is held in place by the Earth's gravity. The main components are nitrogen (78.09%), oxygen (20.95%), argon (0.93%), and carbon dioxide (0.03%). The atmosphere also contains small amounts, or traces, of water (in local concentrations ranging from 0% to 4%), solid particles, neon, helium, methane, krypton, hydrogen, xenon and ozone. The study of the atmosphere is called meteorology. Life on Earth would not be possible without the atmosphere.
  • d increases with increasing altitude. The increase is caused by the absorption of UV radiation by the oxygen and ozone. · The temperature increase with altitude results in a layering effect. It creates a global "inversion layer", and reduces vertical convection. Mesosphere - Extends out to about 100 km (65 miles) · Temperature decreases rapidly with increasing altitude. Thermosphere - Extends out to about 400 km ( 250 miles)
  • hes the Earth, 30% is reflected back into space by clouds and the Earth's surface. The atmosphere absorbs 19%. Only 51% is absorbed by the Earth's surface. We are not normally aware of it but air does have weight. The column of air above us exerts pressure on us. This pressure at sea level is defined as one atmosphere. Other equivalent measurements you may hear used are 1,013 millibars, 760 mm Hg (mercury), 29.92 inches of Hg, or 14.7 pounds/square inch (psi). Atmospheric pressure decreases rapidly with height. Pressure drops by a factor of 10 for every 16 km (10 miles) increase in altitude. This means that the pressure is 1 atmosphere at sea level, but 0.1 atmosphere at 16 km and only 0.01 atmosphere at 32 km. The density of the lower atmosphere is about 1 kg/cubic meter (1 oz./cubic foot). There are approximately 300 billion billion (3 x 10**20, or a 3 followed by 20 zeros) molecules per cubic inch (16.4 cubic ce
  • ers). At ground level, each molecule is moving at about 1600 km/hr (1000 miles/hr), and collides with other molecules 5 billion times per second. The density of air also decreases rapidly with altitude. At 3 km (2 miles) air density has decreased by 30%. People who normally live closer to sea level experience temporary breathing difficulties when traveling to these altitudes. The highest permanent human settlements are at about 4 km (3 miles). LAYERS OF THE ATMOSPHERE The atmosphere is divided into layers based on temperature, composition and electrical properties. These layers are approximate and the boundaries vary, depending on the seasons and latitude. (The boundaries also depend on which "authority" is defining them.) LAYERS BASED ON COMPOSITION Homosphere
  • LAYERS BASED ON TEMPERATURE Troposphere - Height depends on the seasons and latitude. It extends from ground level up to about 16 km (10 miles) at the equator, and to 9 km (5 miles) at the North and South Poles. · The prefix "tropo" means change. Changing conditions in the Troposphere result in our weather. · Temperature decreases with increasing altitude. Warm air rises, then cools and falls back to Earth. This process is called convection, and results in huge movements of air. Winds in this layer are mostly vertical. · Contains more air molecules than
  • · The air is very thin. · The prefix "strato" is related to layers, or stratification. · The bottom of this layer is calm. Jet planes often fly in the lower Stratosphere to avoid bad weather in the Troposphere. · The upper part of the Stratosphere holds the high winds known as the jet streams. These blow horizontally at speeds up to 480 km/hour (300 miles/hour) · Contains the "ozone layer" located
  • gen we need to breath. But it also serves other important functions. It moderates the planet's temperature, reducing the extremes that occur on airless worlds. For example, temperatures on the moon range from 120 °C (about 250 °F) in the day to -170 °C (about -275 °F) at night. The atmosphere
    • cory delacruz
       
      sounds good, by the way am i annoying you with my sticky note??? well, TOO BAD!!!!!!
Carlen Hodgson

12 Surefire Basketball Tips for the Off Season - What Should Players Do Between Seasons? - 0 views

  • The season is winding down. Routines change, friendships have grown, priorities change. As a player, what should you do now? When practice time comes and there is no practice, what do you do? When there are no games to prepare for, what do you do with your time? Here are a just a few thoughts I had as to how to recover and prepare for the next season. 1. Take 3 - 4 weeks to relax. It has been a long, physically and mentally draining season. If you want to improve, you have to give yourself a chance to recover. 2. Catch up and get ahead of your schoolwork. 3. Talk to your coach and evaluate your season. Talk about what you did well and what you did not. Determine the areas you need to improve on. Discuss the things you would like to do and how to accomplish them. 4. After taking a month off, start on your off-season workout program. The program should be about 75% skill work and 25% play. 5. Develop your shooting stroke. If you want to become a GREAT shooter and raise your percentage, it MUST happen during the off season. It's just TOO difficult to develop these skills and improve during the season. It must be done during the off season! 6. Start a strength training program. Your objective should be to gain strength from now until the end of the summer. 7. As you enter the summer, add more play to your workout. You should be at about 50% skill work, 50% play. Don't neglect your weight work. Great strength gains can be made during this period. 8. Go to camp. Learn form other coaches, play against different players. The more diverse your summer experience, the better player you will become. 9. When the summer is over, your routine changes. GET AHEAD in the classroom. Once the season starts, it is easy for your schoolwork to slip. 10. Change your workout routine to 25% skill, 75% play. 11. Switch you strength training routine to an endurance and strength maintenance routine. 12. A week before the season, take some time off. Get ready to go.
Carlen Hodgson

Basketball Tip, Basketball Tips, Basketball Shooting Tips, Free Basketball Tips - 0 views

  • One of the keys to getting the most out of your training program is to work outside of your comfort zone.
  • I can't argue that you're doing something to stay in shape and work on your game. But you're not really pushing yourself, and you shouldn't really expect those types of workouts to pay huge dividends.
  • Change your approach. Push yourself harder than you normally do, and you'll start to see results. Instead of shooting 30 or 40 random, lazy jump shots, create a plan for yourself. Shoot from 4 or 5 spots on the floor until you've made 30 or 40 shots from each spot (or some number that you set as a goal for yourself). Get in the triple-threat position, head-fake, take a quick dribble to one side or the other, get good lift on your shot (really getting off the ground), and concentrate on your follow-through. Push yourself to move quicker than you normally do, and to jump higher than you normally do.
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  • Or when you go to the track, create a plan to really work on your stamina and quickness. Run 2 laps at a good pace to warm up. Then do some interval training where you sprint at top speed for 40 or 50 yards, then walk for 30 or 45 seconds to get your wind back. When you first start doing interval training, you'll probably only be able to do 4 or 5 repetitions, but you'll get in better shape over time and the numbers will increase. As you get into better shape, you'll work your way up to longer distances, shorter breaks in between sprints, and more repetitions. Follow-up your sprints with 4 or 5 hard minutes of jumping rope. Mix in some longer distance training during the week and you're on your way to really improving your stamina and quickness.
Stephania D

Grolier Multimedia Encyclopedia - 0 views

  • For example, some types of water pollution change the color of the water in a lake or stream, whereas other types are less visible, but both can be equally detrimental to the health of humans and nonhuman animals.
  • For example, 2,000 years ago, when the Romans smelted silver, lead was released into the environment and carried by the wind over long distances; this lead can still be detected in Scandinavian lake sediments.
  • Relatively few of these new compounds have been thoroughly tested for possible health or environmental effects.
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  • Hazardous chemicals are dangerous because they are flammable, explosive, strong irritants, sensitizers, or acids and bases.
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    Water pollution
Kate L

Alternative Fuel Sources - Cheaper And Eco-Friendly - 0 views

  • The conventional and traditional fuel sources are becoming more and more expensive to extract and their indiscriminate use in the past century has resulted in their depletion.
  • natural fuel sources will reach critically low levels and precipitate a crisis much earlier than we think.
  • promising discoveries
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  • mankind would have perfected and commercialized alternate sources of fuel that will be eco- friendly and affordable too.
  • Its contents of 15% gasoline and 85% ethanol mean that it is at least better than using pure gasoline.
  • E 85, bio-diesel
  • Bio-diesel is one such alternate fuel source that is extracted from plants.
  • uch alternate fuel sources like E 85 score above gasoline, they still pollute and require a vast amount of corn to be grown
  • translates into availability of lesser land for growing food for people.
  • electric cars seem to be the best alternate fuel source that we have
  • conserve our natural fuel sources.
  • efficient because all of the electricity that they need can be generated at one central location.
  • much better option than consuming petroleum derivatives and polluting more by using small and inefficient combustion motors.
  • Electricity
  • produced in any manner that suits the needs on a particular location depending on the resources it has
  • coal, hydro-electric or wind to produce this electricity that is required for electric cars.
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    alternative fuel sources
Bibin John

Aircraft - Wikipedia, the free encyclopedia - 0 views

  • An aircraft is a vehicle which is able to fly through the Earth's atmosphere or through any other atmosphere. Rocket vehicles are not aircraft if they are not supported by the surrounding air. All the human activity which surrounds aircraft is called aviation.
  • Heavier-than-air aircraft must find some way to push air or gas downwards, so that a reaction occurs (by Newton's laws of motion) to push the aircraft upwards. This dynamic movement through the air is the origin of the term aerodyne. There are two ways to produce dynamic upthrust: aerodynamic lift, and powered lift in the form of engine thrust. Aerodynamic lift is the most common, with aeroplanes being kept in the air by the forward movement of wings, and rotorcraft by spinning wing-shaped rotors sometimes called rotary wings. A wing is a flat, horizontal surface, usually shaped in cross-section as an aerofoil. To fly, the wing must move forwards through the air; this movement of air over the aerofoil shape deflects air downward to create an equal and opposite upward force, called lift, according to Newton's third law of motion. A flexible wing is a wing made of fabric or thin sheet material, often stretched over a rigid frame. A kite is tethered to the ground and relies on the speed of the wind over its wings, which may be flexible or rigid, fixed or rotary. With powered lift, the aircraft directs its engine thrust vertically downwards. The initialism VTOL (vertical take off and landing) is applied to aircraft that can take off and land vertically. Most are rotorcraft. Others, such as the Hawker Siddeley Harrier, take off and land vertically using powered lift and transfer to aerodynamic lift in steady flight. Similarly, STOL stands for short take off and landing. Some VTOL aircraft often operate in a short take off/vertical landing regime known as STOVL. A pure rocket is not usually regarded as an aerodyne, because it does not depend on the air for its lift (and can even fly into space), however many aerodynamic lift vehicles have been powered or assisted by rocket motors. Rocket-powered missiles which obtain aerodynamic lift at very high speed due to airflow over their bodies, are a marginal case.
  • The forerunner of the aeroplane is the kite
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  • Number of planes - Monoplane, biplane, etc. Wing support - Braced or cantilever, rigid or flexible. Wing planform - including aspect ratio, angle of sweep and any variations along the span. Includes the important class of delta wings. Location of the horizontal stabiliser, if any. Dihedral angle - positive, zero or negative (anhedral). A variable geometry aircraft can change its wing configuration during flight. A flying wing has no fuselage, though it may have small blisters or pods. The opposite of this is a lifting body which has no wings, though it may have small stabilising and control surfaces.
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    Tells all about different kinds of aircrafts.
Bibin John

History Who Really Invented the Airplane Part 1 - Trivia-Library.com - 0 views

  • Leonardo da Vinci designed a flying machine in the 15th century, and by the 19th century men were airborne in hot-air balloons, gliders, and huge kites.
  • depended on the whimsy of the wind
  • And so, at the end of the 19th century, enthusiasts around the world joined in the race to invent the first flying machine.
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  • CLEMENT ADER (1841-1925)
  • Clement Ader
  • producing a kite capable of carrying a man aloft
  • build and design countless kites
  • In the early 1870s he created an ornithopter, an engine to which was attached flapping wings, but it failed to fly
  • Ader went to Algeria to study the flight of vultures
  • In order to fly, he decided, a machine must have fixed wings and an engine capable of lifting it off the ground
  • the Eole
  • akeoff and a powered flight of approximately 165 ft.
  • 330 ft.
  • Ader himself did not publicly report this flight until 1906.
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