Our lives will not be the same without electricity
We communicate, travel and compute faster because of the devices run by electricity
An atom is electrically neutral because they have an equal number of protons and electrons
Following Benjamin Franklin's study of electricity, we call electrical charges positive and negative
These two types of charges exist in all materials and in all states of matter
Protons are the carriers of positive charges, neutrons are the uncharged particles, and electrons are the carriers of negative charges
A force that pushes objects apart is a force of repulsion, it exists between particles of the same charge
A force that pulls objects together is a force of attraction, it exists between particles of unlike charges
Negatively charged electrons are attracted to positively charged protons
The standing of the hair on your arm is the result of staticelectricity
Ways to charge an object
Friction
Conduction
Induction
Charging
The process of supplying electric charge to an object or losing the electric charge from an object
Charging by friction
The process in which an object gets charged when it is rubbed against another object or there is a direct contact between the two objects
When two objects are rubbed together, one object loses electrons while the other gains electrons
Charging by conduction
The process in which an object gets charged by making contact with the charged object
Conductors
Materials that allow electrons to move freely, like metals
Insulators
Materials that do not allow electrons to flow freely, like rubber, wood, glass, or plastic
Charging by induction
The process in which an object gets charged by an object without direct contact, the movement of electrons to one part of an object by the electric field of another object
A neutral object needs only to come close to a charged object for the leaves of the electroscope to move separately
More than three quarters of earth's atmosphere is made up of nitrogen while one film is oxygen
These gases not only produce important weather features such as cloud and rain but also have considerable influence on the overall climate of the earth through the greenhouse effect and global warming
Greenhouse
A structure with walls and roofs made chiefly of a transparent material such as plastic or glass, useful in growing seedlings when this winter or spring before planting them in the open field
Uses of greenhouses
Growing seedlings
Protecting flowering and ornamental plants from harsh weather conditions and insectattacks in tropical countries
How greenhouses work
Transparent covering allows visible light to enter without obstruction
Warms the inside of the greenhouse as energy is absorbed by the plants soil and other things in the building
Air warmed by the heat inside is retained in the building by the roof and wall
Transparent covering prevents the heat from leaving by reflecting the energy back into the walls and preventing outside winds from carrying it away
Greenhouse effect
The process where greenhouse gases trap the heat in the atmosphere
Global warming
The current rise in the average temperature of earth's air and oceans
Sources of greenhouse gas emissions
Burning fossil fuels for electricity, heat and transportation
Deforestation and land clearing for agriculture
Degradation of soils
Agricultural activities
Waste management
Energy use
Biomass burning
Use of fertilizers
Industrial processes
Refrigeration
Use of consumer products
Many of these greenhouse gases can cause earth's atmosphere to trap more and more heat, increase air temperature and cause global warming
Global warming is feared to melt polar ice caps and cause flooding to low-lying areas, resulting in a reduction in biodiversity and changing climates around the globe, causing stronger typhoons and creating many health related problems
There are a number of unique combinations of atmospheric phenomena experienced by people in all parts of the world
Wind
Air that is moving horizontally
Land surface heats up faster than bodies of water during the day, but land loses heat faster than bodies of water at night
Sea breeze formation
1. Land warms up faster than bodies of water during the day
2. Warm air above land rises
3. Cooler air above the sea moves toward the land and replaces the warm air
Land breeze formation
1. Land cools faster than the sea at night
2. Warm air over the sea rises
3. Cooler air from the land moves toward the sea
Monsoon formation
1. Air moves toward the place where warm air is rising (low pressure area)
2. Cold air sinks in the high pressure area
3. Wind moves from high pressure to low pressure area
Northeast monsoon
High pressure in China and Siberia, low pressure in South Indian Ocean/Australia
Brings dry, cold wind
Intertropical Convergence Zone (ITCZ)
Place where trade winds from Northern and Southern hemispheres meet at the equator
Warm, humid air masses form resulting in heavy precipitation and thunderstorms
Breeding zone of low pressure areas
The earth is constantly moving around the sun and the moon is constantly moving around the earth
Eclipse
Occurs when the shadow of either the moon or earth is cast on the other
Straight or nearly straight line formation of the sun, earth, and moon