Studied by 7 peopleCarbon
present as CH4 in permafrost soils and lake bottoms.
Over the past 900,000 years
Glacial and interglacial periods
Over the past 10,000 years
Interglacial period
Over the past 1,000 years
Temperature has been stable
Over the past 100 years
Temperature changes; methods of determination
Global warming
rapid rate of increasing temperatures
Thick, light-colored low-altitude clouds
decrease surface temperature
Thin, cirrus clouds at high altitudes
increase surface temperature
Prolonged droughts
grasslands become dustbowls
Organisms that increase global warming
Insects, fungi, and microbes
Monsoons
Climatic systems anywhere in which the moisture increases dramatically in the warm season
Jet Stream
Current of fast-moving air found in the upper levels of the atmosphere
Global change
changes in the biological, physical, and chemical properties of Earth
Global climate change
changes in average climate (long-term weather patterns over years or decades)
Monsoons
Climatic systems anywhere in which the moisture increases dramatically in the warm season
Jet Stream
Current of fast-moving air found in the upper levels of the atmosphere
Global change
changes in the biological, physical, and chemical properties of Earth
Global climate change
changes in average climate (long-term weather patterns over years or decades)
Note
Flashcard