Climate and Climate Change Review

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Vocabulary flashcards reviewing core climate, atmospheric circulation, global wind patterns, climate history proxies, and greenhouse effect concepts from Chapter 21.

Last updated 1:21 PM on 9/9/26
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28 Terms

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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.

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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.

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Subtropical Jet Stream

A jet stream that flows in high altitude between the trade winds and the westerlies.

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Polar Jet Stream

A jet stream that flows in high altitude along the polar front.

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Coriolis Effect

The force that deflects high-altitude air at boundaries between climate cells, causing jet streams to form.

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Horse Latitudes

The region located around 30o N/S30^\text{o}\text{ 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.

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Tree Ring Indicators

Annual growth rings in trees that become smaller and thinner during cool, dry years.

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Atmosphere Warming (Past 50 Years)

The observed global temperature increase of 0.8oC0.8^\text{o}\text{C} in the atmosphere over the past 50 years.

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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.

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Factors Driving Planetary Climate

The three fundamental energy factors that determine heat available for climate and weather: energy input, energy absorbed, and energy reflected.

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Trade Winds

Global wind belts located between the equator and 30o30^\text{o} latitude that blow toward the equator from the northeast and southeast.

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Prevailing Westerlies

Global wind belts located between 30o30^\text{o} and 60o60^\text{o} latitude marks.

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Polar Easterlies

Global wind belts located between 60o60^\text{o} latitude and the North/South Poles, where cold air sinks at the poles and deflects from the east.

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Polar Front

The latitude line around 60o N/S60^\text{o}\text{ N/S} where the prevailing westerlies and polar easterlies converge.

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Ancient Sea Sediment Fossils

The most useful geological method for determining Earth's temperatures up to one billion years ago.

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Oxygen-16 (16O^{16}\text{O})

The lighter isotope of oxygen that evaporates more easily than oxygen-18 (18O^{18}\text{O}).

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Oxygen Isotope Ratio (16O/18O^{16}\text{O}/^{18}\text{O})

A ratio measured in glacial ice and calcium carbonate organisms to determine past mean ocean temperatures.

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Subtropical Deserts

Large deserts situated around 30o30^\text{o} latitude created because dry air is sinking and warming.

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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.

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Faint Young Sun

The condition early in Earth's history when the sun was approximately 30%30\text{\%} fainter than it is today.

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Holocene Climate

The climate of the past 10,000 years10{,}000\text{ years}, which has been mild compared to the previous 100,000 years100{,}000\text{ years}.

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Antarctic Coal Deposits

Geological evidence indicating that the climate in Antarctica was warm and wet in the past.

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Albedo

The measure of reflectivity of surfaces like glaciers and snowfields, which cools climate by reflecting solar energy back into space.

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Carbonic Acid

The acid formed when carbon dioxide gas dissolves in seawater.

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Doldrums

An equatorial ocean region characterized by calm or very light winds.

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Methane Release from Permafrost

The release of methane, a potent greenhouse gas, caused by the thawing and melting of permafrost.

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Human-Induced Carbon Emissions Share

The statistic that nearly 80%80\text{\%} of human-induced carbon emissions occur through industry and agriculture.

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Non-Linear Climate Feedback

The property of the climate system where relationships are non-linear, meaning small changes can produce substantially larger consequences.