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Vocabulary flashcards reviewing core climate, atmospheric circulation, global wind patterns, climate history proxies, and greenhouse effect concepts from Chapter 21.
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Industrial Greenhouse Gases
The four main industrial gases that trap heat in the atmosphere: carbon dioxide, methane, nitrous oxide, and fluorinated gases.
Three-Cell Model
A model of global wind patterns that deciphers three convection cells in each hemisphere bordered by alternating bands of high and low pressure.
Subtropical Jet Stream
A jet stream that flows in high altitude between the trade winds and the westerlies.
Polar Jet Stream
A jet stream that flows in high altitude along the polar front.
Coriolis Effect
The force that deflects high-altitude air at boundaries between climate cells, causing jet streams to form.
Horse Latitudes
The region located around 30o N/S latitude where global winds are calm or very weak, historically named because Spanish ships became stranded in calm waters and horses were thrown overboard.
Tree Ring Indicators
Annual growth rings in trees that become smaller and thinner during cool, dry years.
Atmosphere Warming (Past 50 Years)
The observed global temperature increase of 0.8oC in the atmosphere over the past 50 years.
Plankton Temperature Proxies
Microscopic organisms used to determine past water temperatures based on species survival preferences in warm versus cold water and their oxygen isotope ratios.
Factors Driving Planetary Climate
The three fundamental energy factors that determine heat available for climate and weather: energy input, energy absorbed, and energy reflected.
Trade Winds
Global wind belts located between the equator and 30o latitude that blow toward the equator from the northeast and southeast.
Prevailing Westerlies
Global wind belts located between 30o and 60o latitude marks.
Polar Easterlies
Global wind belts located between 60o latitude and the North/South Poles, where cold air sinks at the poles and deflects from the east.
Polar Front
The latitude line around 60o N/S where the prevailing westerlies and polar easterlies converge.
Ancient Sea Sediment Fossils
The most useful geological method for determining Earth's temperatures up to one billion years ago.
Oxygen-16 (16O)
The lighter isotope of oxygen that evaporates more easily than oxygen-18 (18O).
Oxygen Isotope Ratio (16O/18O)
A ratio measured in glacial ice and calcium carbonate organisms to determine past mean ocean temperatures.
Subtropical Deserts
Large deserts situated around 30o latitude created because dry air is sinking and warming.
Urban Heat Island Effect
A phenomenon where cities are significantly warmer than surrounding rural areas due to trapped air pollutants, low-pressure systems, and rising warm air.
Faint Young Sun
The condition early in Earth's history when the sun was approximately 30% fainter than it is today.
Holocene Climate
The climate of the past 10,000 years, which has been mild compared to the previous 100,000 years.
Antarctic Coal Deposits
Geological evidence indicating that the climate in Antarctica was warm and wet in the past.
Albedo
The measure of reflectivity of surfaces like glaciers and snowfields, which cools climate by reflecting solar energy back into space.
Carbonic Acid
The acid formed when carbon dioxide gas dissolves in seawater.
Doldrums
An equatorial ocean region characterized by calm or very light winds.
Methane Release from Permafrost
The release of methane, a potent greenhouse gas, caused by the thawing and melting of permafrost.
Human-Induced Carbon Emissions Share
The statistic that nearly 80% of human-induced carbon emissions occur through industry and agriculture.
Non-Linear Climate Feedback
The property of the climate system where relationships are non-linear, meaning small changes can produce substantially larger consequences.