Chapter 4: Ecosystems and the physical environment Flashcards
cellular respiration
a process in which the energy of organic molecules is released within cells
ammonification
part of nitrogen cycle: conversion of nitrogen compounds into ammonia via pee and ammonifying bacteria
gyres
large, circular ocean current systems that often encompass an entire ocean basin
dentrification
part of nitrogen cycle: the conversion of nitrate (NO3) to nitrogen gas (N2) by certain bacteria in the soil
photosynthesis
the biological process that captures light energy and transforms it into the chemical energy of organic molecules (like glucose), which are manufactured from carbon dioxide and water
albedo
the proportional reluctance of solar energy from earth’s surface, commonly expressed as a percentage
thermosphere
outermost layer of the atmosphere
El Nino-southern oscillation
a periodic, large-scale warming of surface waters of the tropical eastern Pacific Ocean that affect both ocean and atmospheric circulation patterns
nitrogen fixation
part of the nitrogen cycle: the conversion of atmospheric nitrogen (N2) to ammonia (NH3) by nitrogen-fixing bacteria and cyanobacteria
upwelling
occurs when a rising ocean current transports colder, nutrient-laden water in the surface
asthenosphere
region of the mantle where rocks become hot and soft
trade wind
a prevailing tropical wind that blows from the northeast (in the Northern Hemisphere) or from the southeast (in the Southern Hemisphere)
Polar easterly
a prevailing wind that blows from the northeast near the North Pole or from the southeast near the South Pole
Lithosphere
Earth’s outermost rigid rock layer that is composed of seven large plates, plus a few smaller ones
transpiration
part of the hydrologic cycle: the loss of water vapor from the aerial surface of plants
biogeochemical cycle
the process by which matter cycles from the living physical environment and back again
Parts of the carbon cycle
photosynthesis
cellular respiration
fossil fuels
combustion
fossil fuels
coal, oil, and natural gas from ancient decaying trees deep underground
combustion
how the carbon from the trees returns back into the atmosphere (oxidized)
Human-induced changes to the carbon cycle
more Co2 in atmosphere than what was in the ground
all basic effects of global warming
parts of the nitrogen cycle
nitrogen fixation nitrification assimilation ammonification dentrification
nitrification
conversion of NH3 to NO3 via soil bacteria
assimilation
plant roots absorbe nitrate or ammonia and use the nitrogen to form plant proteins and nucleic acids
human induced changes to the nitrogen cycle
nitrogen fertilizer is creating dead zones
less plant species
nitrogen oxides
high temps of combustion convert N2 into nitrogen oxides which produce photochemical smog
photochemical smog
mixture of air pollutants that injures plant tissues, irritates eyes, and causes respiratory problems
acid deposition
nitrogen oxides react with water in the atmosphere and leave the atmosphere
parts of the phosphorus cycle
land
sediments in the ocean
land
human induced changes to the phosphorus cycle
accel long-term loss of phosphorus from land
plants to cows to poop to sewage and ocean and it is permanently lost to the terrestrial cycle
parts of the hydrologic cycle
transpiration
runoff
watershed
grondwater
runoff
part of the hydrologic cycle
the movement of water from land to rivers, lakes, wetlands, and the ocean
watershed
part of the hydrologic cycle
the area of land drained by runoff
groundwater
part of the hydrologic cycle
fresh water stored underground in rock
aresols
tiny particles of air pollution consisting mostly of sulfates, nitrates, carbon, mineral dusts, and smokestack ash
human induces changes to the hydrologic cycle
aerosols and melting of polar ice
temperature changes with latitude
not direct sunlight at poles like at the equator
ozone
in the stratosphere, our sunglasses
Coriolis effect
the influence of earth’s rotation which turns air and water right in north and left in south
prevailing winds
major surface winds that blow more or less continually
currents
winds create ocean movement
ocean conveyor belt
the circulation of shallow and deep ocean currents
rain shadow
dry conditions, often on a regional scale, that occur on the leeward side of a mountain barrier; the passage of moist air across the mountains removes most of the moisture
plate tetonics
the study of the processes by which the lithosphere plates move over the asthenosphere
plate boundary
area where two plates meet
transformation plate boudary
when plates move horizontally across eachother
seismic waves
vibrations that spread through rocks rapidly in all directions
landslide
avalanche of rock, soil, etc down mountain
tsunami
giant sea wave