Large system broken into smaller subsystems including the atmosphere, biosphere, geosphere, and hydrosphere
Water movement
1. Moves within the hydrosphere and into other Earth systems
2. Changes state between liquid, solid, and gas
Water is not just a liquid, it can also be a solid (ice) or a gas (water vapor)
As water flows or changes state, it moves thermal energy among Earth's systems
Evaporation
The process by which a liquid, such as water, changes into a gas
Condensation
The process by which a gas changes to a liquid
Crystallization
The process by which a liquid turns into a crystalline solid
Sources of water vapor in the water cycle
Evaporation
Transpiration
Cellular Respiration
Precipitation
Moisture that falls from clouds to Earth's surface
The amount of water on Earth does not change, it is stable
Changes in Earth's global temperature can affect how water is cycled
Aquifer
Areas of permeable sediment or rock that hold significant amounts of water
Groundwater flow
Moves from higher areas to lower areas, eventually reaching the ocean
Radiation
The transfer of energy by electromagnetic waves
Radiation is the only way thermal energy can travel from the Sun to Earth
Latitude
The distance in degrees north or south of the equator
The equator is the largest circle, areas in low latitudes near the equator are referred to as the tropics
Sunlight strikes Earth's surface at the tropics at a high angle, nearly 90 degrees, resulting in more sunlight per unit of surface area
Conduction
The transfer of thermal energy between materials by the collisions of particles
Conduction occurs in the bottom part of the atmosphere where it comes in contact with Earth
Albedo
Describes how much solar radiation is reflected off of a surface
Dark colors absorb more solar radiation than light colors, causing their temperature to rise
Snow- and ice-covered fields reflect the most sunlight of all
The temperature of the atmosphere is greatly affected by the albedo of the hydrosphere, geosphere, and biosphere
Meteorologists
Scientists who study and predict weather
Weather
The atmospheric conditions, along with short-term changes, of a certain place at a certain time
Air masses
Large bodies of air with distinct temperature and moisture characteristics
Form when a large, high-pressure system stays over an area for several days
The air circulating in the high-pressure system comes in contact with Earth and takes on the temperature and moisture characteristics of the surface below it
Can extend for a thousand kilometers or more
Cool air molecules
Are closer together than warm air molecules
Cool air masses
Have high pressure, or more weight, than warm air masses
Warm air masses
Have low pressure, or less weight
What happens when air masses meet
1. Wind carries an air mass away from the area where it formed
2. The air mass will eventually bump into another air mass
3. A weather front is the boundary between two air masses
Climate
The long-term average weather conditions that occur in a particular region
Weather forecasts
Short term forecasts are the most detailed but still only able to be predicted probabilistically
Long term forecasts are more difficult to make because weather conditions are constantly changing
Climate
The long-term average weather conditions that occur in a particular region
Climate
Depends on average temperature
Depends on precipitation
Depends on how these variables change throughout the year
Regions with rain forests and deserts differ due to precipitation
Climate
Depends on average temperature
Depends on precipitation
Depends on how these variables change throughout the year
Rain forest
High annual rainfall
No freezing temperatures
Rich collection of plant and animal life
Regions with rain forests and deserts differ due to precipitation