Global Climate Cycling Flashcards

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A set of vocabulary flashcards covering global climate cycling, the hydrological cycle, the mercury cycle, and the carbon cycle based on the introductory lecture transcript.

Last updated 11:45 AM on 6/20/26
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70 Terms

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Elemental cycle

The pathways that elements move through as they change status and pass between the atmosphere, biosphere, hydrosphere, and geosphere.

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Biosphere

The sphere within earth systems inhabited by living things that experiences considerable change due to carbon and nitrogen levels.

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Hydrosphere

The sphere of earth systems comprising all water environments, including terrestrial, freshwater, and marine ecosystems.

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Geosphere

The solid part of the earth system through which elements move as they change status.

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Fundamentals of Ecosystem Sciences

The recommended textbook for the course written by Weathers, Strayer, and Lycans.

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Hydrological fluxes

The movements of water that enable the circulation of earth-atmosphere systems and empower interaction between processes.

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Evaporation

The process of changing water from an aqueous phase into a gaseous phase.

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Condensation

The process where water changes from a gaseous phase back into an aqueous phase.

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Precipitation

One of the seven movements of water; total land precipitation is estimated at 111,000km3/year111,000\,km^3/year.

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Sublimation

One of the seven specific movements by which water enables transfer between different pools.

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Transpiration

A movement of water involving the release of water vapor from plants into the atmosphere.

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Runoff

The movement of water over the land surface as a hydrological flux.

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Infiltration

The process by which water on the ground surface enters the soil.

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Vector

A role played by water as a carrier for the migration of elements between different pools.

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International Bulk Containers (IBCs)

Containers used to carry liquid that represent 1m31\,m^3 of liquid, or 1ton1\,ton in the case of water.

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Cubic kilometer (km3km^3)

A unit equivalent to 1×1015liters1 \times 10^{15}\,liters or 1×1012m31 \times 10^{12}\,m^3, approximately the size of 400,000,000400,000,000 Olympic sized swimming pools.

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Flux

A term describing an element or substance in motion between different reservoirs.

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Pool

A reservoir or location where an element is sequestered or stored.

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Groundwater discharge

Water moving from the ground into rivers, estimated to be about 10%10\% of total river discharge globally.

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Hydrogyrum

The former name for mercury, derived from the Greek words 'hydor' for water and 'Argyros' for silver.

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Mercury (HgHg)

Atomic number 80; a dense metallic element that is liquid at standard temperature and pressure with a molecular weight of 200.59200.59.

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Divalent mercury (Hg2+Hg^{2+})

The oxidized form of mercury which is more prone to toxicity than the reduced form.

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Zero valent mercury (Hg0Hg^0)

The reduced, elemental form of mercury.

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Amalgam

A mercury-based mixture traditionally used to remove gold from complex mineral matrices.

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Methyl mercury

An organo form of mercury produced in anaerobic environments with much greater potency and toxicity than elemental mercury.

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Methylation

The transformation of mercury (IIII) into an organo form in anaerobic environments, a process driven by the carbon cycle.

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Demethylation

The process of converting methyl mercury back into an ionic state.

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Megagram (MgMg)

A unit of mass equal to 1,000,000grams1,000,000\,grams or one metric ton.

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Biocide

A medical use for mercury due to its high level of toxicity.

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Anthropogenic flux

The movement of elements, such as the 7,300Mg/year7,300\,Mg/year of new mercury releases, caused by human activity.

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Carbon (CC)

Atomic number 6; the fifteenth most abundant element in the Earth's crust, derived from the Latin word for coal ('carbo').

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Allotropes

Different structural forms of the same element, such as graphite and diamonds for carbon.

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Inorganic carbon

Forms of carbon like carbon dioxide (CO2CO_2) that can be converted to organic forms with an input of energy.

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Organic carbon

Pre-fixed carbon forms that release energy upon the breaking of organic bonds to return to an inorganic state.

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Photosynthesis

The process by which photosynthetically active cells in plants and algae take CO2CO_2 from the atmosphere and turn it into prefixed organic carbon.

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Aerobic respiration

The process of taking prefixed carbon and producing carbon dioxide while liberating energy.

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Decomposition

The process of taking organic carbon linked to water to release energy and produce carbon dioxide.

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Redox reactions

Coupled reactions involving electron donation (oxidation) and electron acceptance (reduction).

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Electron donation

The part of a redox reaction that creates an oxidized product.

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Electron acceptance

The part of a redox reaction that creates a reduced product.

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Lithosphere

The rigid outer part of the earth where carbon is buried or sequestered within mineral processes.

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Petagram (PgPg)

A unit of mass equal to 1,000,000,000metrictons1,000,000,000\,metric\,tons, a gigaton, or 1×1015grams1 \times 10^{15}\,grams.

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Carbon stocks

The reservoir mass of carbon, often measured in petagrams (PgPg).

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Sedimentary rocks

A massive carbon pool estimated to hold between 50,000,00050,000,000 and 90,000,000Pg90,000,000\,Pg of carbon.

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Fossil fuels

A carbon reservoir holding about 10,000,000Pg10,000,000\,Pg of carbon.

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Marine biota

Living organisms in the ocean that interact with surface ocean carbon pools at a flux of about 50Pg/year50\,Pg/year.

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Dissolved organic carbon (DOC)

A form of carbon stored in water that may not go through further degradation.

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Particulate materials

Sinking matter through which carbon can be sequestered into water.

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Biome

A large naturally occurring community of flora and fauna, such as tropical rainforests or tundra, used to estimate carbon stocks.

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Tropical rainforest (carbon density)

An environment with a high carbon density of 194tons194\,tons of carbon per hectare.

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Tundra (carbon density)

An environment with a low carbon density of 4tons4\,tons of carbon per hectare.

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Carbon residence time

The turnover time for carbon in a biome; for example, 15.5years15.5\,years in tropical rainforests.

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Industrial Revolution

The historical period starting around 1800 that caused a sudden spike in atmospheric CO2CO_2 concentrations.

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Interglacial periods

Times between ice ages when concentrations of CO2CO_2 have historically changed between approximately 190190 and 300ppm300\,ppm.

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Parts per million (ppm)

The unit used to measure the concentration of atmospheric carbon dioxide.

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Calcareous rocks

Types of rocks in the lithosphere associated with the storage of approximately 50,000,000Pg50,000,000\,Pg of carbon.

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Permafrost

A carbon pool sitting at about 1,700Pg1,700\,Pg that is in danger of being released into the atmosphere due to climate change.

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Scottish Monroe

An analogy used to visualize volume, being approximately 3,000feet3,000\,feet or 1,000meters1,000\,meters high.

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Steady state

A conceptual condition where the inputs and outputs of a particular element's cycle are balanced.

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Biomass

Biological material that can pick up trace amounts of mercury and release it into the atmosphere when burned.

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Long range transport

The movement of elements like mercury over great distances, often following high-altitude release from volcanic eruptions.

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Anaerobic sediments

Oxygen-poor environments where mercury can react to become bound as a sulfide.

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Troposphere

The lowest layer of the atmosphere, containing about 4,000Mg4,000\,Mg of mercury.

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Evapotranspiration

The combined process of evaporation and plant transpiration; forestry evapotranspiration constitutes about 1,100Mg1,100\,Mg of mercury flux.

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Recalcitrant carbon

Stable forms of carbon that build up in the soil over time rather than being easily degraded.

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Deep ocean (carbon pool)

A large carbon reservoir containing approximately 38,000Pg38,000\,Pg of carbon.

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Surface ocean (carbon pool)

An oceanic reservoir holding about 1,000Pg1,000\,Pg of carbon with an annual flux of 970Pg970\,Pg.

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Global climate cycling

The overarching study of how elements and water move through earth systems.

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Multitude of isotopes

The reason why mercury has a varying molecular weight, averaged at 200.59200.59.

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Polymers

Complex chains formed by carbon that are essential for the existence of life as we understand it.