AP Environmental Science - Chapter 5

hydrologic cycle

Global circulation of H2O from the environment to living organisms and back to the environment

transpiration

the emission of water vapor from the leaves of plants

runoff

movement of water from land to bodies of water such as lakes and eventually to the ocean

watershed

area of land drained by a runoff

Fixed Nitrogen

nitrogen that's chemically combined with hydrogen, oxygen or carbon

photochemical smog

a mixture of air pollutants caused by nitrogen oxides. These pollutants hurt plant tissues and irritate humans' eyes and throats

nitrogen oxides

cause photochemical smog

Aerosols

tiny particles of air pollution made up chiefly of sulfates, nitrates, carbon and mineral dusts. Produced from burning of fossil fuel and forests. These particles further the scattering and absorbtion of sunlight and create brighter clouds, resulting in a

albedo

The proportional reflectance of solar energy from Earth's surface, expressed as a percentage.

troposphere

Atmosphere layer nearest the Earth's surface

stratosphere

atmosphere layer above troposhere. There is a steady wind here, but no turbulence

mesosphere

directly above stratosphere. Contains the atmosphere's lowest temperature (as low as -138 degrees Celsius)

thermosphere

Part of atmosphere that absorbs X-rays and short-wave ultraviolet radiation. Very hot. The aurora is caused by charged particles from the sun colliding with oxygen and nitrogen molecules in this layer of the atmosphere.

Exosphere

Outer layer of atmosphere

winds

horizontal movements" in the atmosphere caused by differences in atmospheric pressure and also the Earth's rotation

Coriolis Effect

The influence of the Earth's rotation, which tends to turn fluids (air and water) toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere.

Prevailing winds

Major surface winds that blow more or less continually. Includes polar easterlies, westerlies, and trade winds

polar easterlies

one of three kinds of prevailing winds, these winds come from the northeast (near the North Pole) and the southeast, near the South Pole

Westerlies

These prevailing winds come from the southwest in the Northern Hemisphere and northwest in the Southern Hemisphere

Trade winds

Tropical winds coming from the northeast in the Northern Hemisphere and the southeast in the Southern Hemisphere. These are one of the three kinds of prevailing winds

gyres

Large, circular ocean current systems that often encompass an entire ocean basin

Ocean Conveyor Belt

The circulation of shallow and deep currents

El Nino-Southern Oscillation (ENSO)

A cycling of alternating warming and cooling of surface waters of the tropical eastern Pacific Ocean that affects both ocian and atmospheric circulation patterns. Every 3 to 7 years, the trade winds weaken, causing there to be a wider spread of warm water

upwelling

This is what it is called when deeper ocean water comes to the surface

La Nina

The eastern Pacific Ocean's surface water temperature becomes unusually cool and westbound trade winds get unusually strong. This event often occurs after El Nino

climate

the average weather conditions that occur in an area over a period of years

Wladimir Koppen

German botanist & climatologist. Developed the most widely used climate-classifying system

Rain Shadow

dry conditions, often on a regional scale, that occur on the side of a mountain barrier towards which the wind blows; the passage of moist air across the mountains removes most of the moisture

Tropical Cyclones

giant, rotating tropical storms" winds are 119+ km/hr. Aka hurricanes, typhoons, cyclones

Plate Tectonics

the study of the dynamics of Earth's lithosphere and the movement of its seven plates

Asthenosphere

the region of the mantle of the lithosphere where rocks become hot and soft

lithosphere

Earth's rigid outer rock layer

seismic waves

vibrations that spread through the lithosphere's rocks rapidly in all directions

focus

site where an earthquake begins

epicenter

spot on Earth's surface, directly above an earthquake's focus

Charles Richter

The seismologist who invented the Richter scale in 1935

Richter Scale

A way to measure the magnitude of energy released by an earthquake. Invented by Charles Richter in 1935.

tsunami

giant sea wave caused by an underwater earthquake

landslide

avalanche of rock, soil & debris that slides down a mountain. Often the result of an earthquake

hot spot

1. A rising plume of magma that flows from deep within the Earth's surface, occuring at a weak point in a tectonic plate rather than where two tectonic plates meet 2. An area of great species diversity that is at risk of destruction by human activities

Nitrogen fixation

first stage of Nitrogen cycle. gaseous nitrogen is converted to ammonia (NH3) or ammonium (NH4) by certain kinds of bacteria, such as cyanobacteria

Nitrification

second step of nitrogen cycle. ammonia (NH3) or ammonium (NH4) is converted to nitrate by bacteria in the soil.

Assimilation

Third step in Nitrogen Cycle. Nitrate (NO3), ammonia (NH3) or ammonium (NH4) is absorbed by plant roots, which incorporate the nitrogen into plant proteins and nucleic acids. Animals then eat the plants and take in the nitrogen compounds (amino acids) and

Ammonification

Fourth step in the Nitrogen Cycle. Biological nitrogen compounts change into ammonia (NH3) and ammonium (NH4). Animals will often form waste containing nitrogen, called "urea" or "uric acid.

Denitrification

The fifth and last step of the Nitrogen Cycle. Nitrate (NO3) is reduced to gaseous nitrogen