Chapter 9, 10, 11 Study Guide Flashcards

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1
Q

water covers ___% of the Earth’s surface

A

71%

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2
Q

water/water vapor emerge from deep in the Earth

A

outgassing

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3
Q

changes in sea level due to water being stored in glaciers and ice sheets

A

Glacio-eustasy

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4
Q

has operated for billions of years from the lower atmosphere to several kilometers beneath Earth’s surface; a model of Earth’s water systems

A

Hydrologic Cycle

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5
Q

can be used to describe the flow of water and in out of a system
precipitation = actual evapotranspiration + surplus +/- change in soil

A

water balance equation

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6
Q

how to find actual evapotranspiration

A

potential evapotranspiration - deficit

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7
Q

the windshield can reduce on under catch and improve the accuracy of rainfall measurements

A

precipitation measurement

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8
Q

the net movement of free water molecules away from a wet surface into air

A

evaporation

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9
Q

the movement of water through plants and back into the atmosphere; it is a cooling mechanism for plants

A

transpiration

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10
Q

water supply/receipt; PRECIP; the moisture supply to Earth’s surface arriving as rain, sleet, snow, and hail

A

precipitation

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11
Q

majority water expenditure; a combination of evaporation and transpiration

A

evapotranspiration

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12
Q

POTET; the ultimate demand for moisture; the amount of water that would evaporate and transpire under optimum moisture conditions (adequate precipitation and adequate soil moisture)

A

potential evapotranspiration

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13
Q

finding actual evapotranspiration

A

ACTET = POTET – water deficit

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14
Q

if demand exceeds supply, water shortage results

A

water deficit

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15
Q

the volume of water stored in the soil that is accessible to plant roots

A

soil moisture storage

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16
Q

water is inaccessible to plants because it is a molecule-thin layer that is tightly bound to each soil particle by hydrogen bonding

A

hydroscopic water

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17
Q

generally accessible to plant roots because it is held in the soil by surface tension and hydrogen bonding between water and soil. Almost all of this type is available in soil-moisture storage

A

capillary water

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18
Q

has the most available water for plants

A

loam soil

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19
Q

When soil is saturated after a precipitation event, surplus water in the soil becomes this type and percolates to groundwater

A

gravitational water

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20
Q

over-use of ground water; over-pumping, collapsing aquifers, saltwater intrusion

A

ogallala aquifer

21
Q

Weather patterns over long time scales and broad geographic areas. “averaged weather” – long term

A

climate

22
Q

areas of similar weather statistics (temperature, rainfall, etc.) these regions form the basis of climate classification

A

climate regions

23
Q

areas of similar weather statistics (temperature, rainfall, etc.) these regions form the basis of climate classification
natural, self-regulating communities formed by plants and animals in their environment climate oscillates, therefore ecosystems and biomes are in a constant state of adaptation and response

A

ecosystem

24
Q

large, naturally occurring community of flora and fauna occupying a major habitat (ex. Forest, tundra, desert, etc.)

A

biome

25
Q

world climates are grouped into six basic categories. Temperature and precipitation form the basis of five categories (tropical, mesothermal, microthermal, polar, and highland) and one is categorized by moisture efficiency as well as temperature (dry)

A

climate types

26
Q

ordering or grouping of data or phenomenon based on statistical data, such as temperature or precipitation

A

empirical classification

27
Q

ordering or grouping of data or phenomenon based on causative factors, such as the interaction of air masses

A

genetic classification

28
Q

temperature and precipitation data are measurable aspects of climate and are plotted to display the basic characteristics that determine climate regions

A

Maps/Climographs

29
Q

A change in solar output of only 1 percent per century alters Earth’s average temp by 0.5-1.0°C

A

solar variability

30
Q

Caused by huge magnetic storms–Cycle is about 11 years

A

sunspots

31
Q

Earths orbital cycle/three main Milankovitch cycles

A

Eccentricity, Obliquity, and Precession

32
Q

plate movement can cause some landmasses to move higher latitudes. Evidence of glaciation in landforms of the Sahara Desert. 465 mya, parts of Africa were centered over the South Pole. Mountain building from plate-plate interactions (Pangea)

A

continental position and topography

33
Q

Outgassing–Natural greenhouse gases: water vapor, carbon dioxide,..–Correlate with Interglacialsand glacials. Volcanic Activity – combined with ejected particulate matter = blocks insolation!–One of the coldest years in the last two centuries was 1816, the “Year Without a Summer”; Caused by eruption of Tamborain Indonesia in 1815

A

atmospheric gasses and aerosols

34
Q

proxy climate indicators

A

two types of proxy records:–Human archives–Natural archives

35
Q

Diaries, letters, personal accounts. Newspapers, almanacs, published sources. Ship logs, naval records. Wine/grape harvests, agricultural sources. Good for the last 100 to 500 years

A

human archives of climate

36
Q

The study of tree growth rings for climate data is known as dendroclimatology. From about 100 to a few 1000 years of records. Tree are long standing weather stations, constantly recording climate conditions at a set location for long periods of time with annual temporal resolution. What kind of data can tree rings tell us?–Rainfall–Temperature–ENSO, PDO, AMO–Wildfires–Earthquakes–Volcanic Eruptions–Landslides, etc.

A

tree ring

37
Q

From 500 to about 40,000 years. Via pollen records etc. Past wildfires from charcoal. Past hurricane activity. Past human activity related to climate

A

lake sediments

38
Q

From about 10,000 to 1 million years into the past. Cores are just like lake sediment cores, but from much deeper depths. Sedimentation rates can be MUCH slower. Microscopic ocean fauna can be used to analyze past climate

A

ocean sediments

39
Q

From 1000 to 100,000s of years in the past. Antarctic Ice Core project in Antarctica now has climate records for the past 800,000 years! (more info). Past climate from trapped air–Carbon dioxide–Oxygen isotopes (18O/16O)–Methane–Sulfur from volcanic eruptions

A

ice cores

40
Q

the production of greenhouse gases emitted by human activity

A

anthropogenic influence on climate change

41
Q

a gas in an atmosphere that absorbs and emits radiation within the thermal infrared range. This process is the fundamental cause of the greenhouse effect. The primary greenhouse gases in Earth’s atmosphere are water vapor, carbon dioxide, methane, nitrous oxide, and ozone

A

greehouse gasses

42
Q

the trapping of the sun’s warmth in a planet’s lower atmosphere due to the greater transparency of the atmosphere to visible radiation from the sun than to infrared radiation emitted from the planet’s surface

A

greenhouse effect

43
Q

Humans disrupt the carbon cycle–Fossil fuel extraction–Fossil fuel combustion–Deforestation. Release carbon and remove carbon sink. Speeds up the soil-atmosphere cycle. More in atmosphere than natural process would allow

A

carbon cycle

44
Q

a general term for buried combustible geologic deposits of organic materials, formed from decayed plants and animals that have been converted to crude oil, coal, natural gas, or heavy oils by exposure to heat and pressure in the earth’s crust over hundreds of millions of years

A

fossil fuels

45
Q

average release between 70 and 120 kg of Methane per year. Methane is a greenhouse gas like carbon dioxide (CO2). But the negative effect on the climate of Methane is 23 times higher than the effect of CO2

A

livestock

46
Q

International Panel on Climate Change–Scientific body set up by the World Meteorological Society and the United Nations Environment Programm. Hundreds of scientists who review the work of the entire scientific community–Largest collaborative scientific effort in history

A

Ippc

47
Q

Elliptical orbit shape varies (by more than 17.1 million km!) on a 100,000 year cycle

A

Eccentricity

48
Q

Earth’s axial tilt varies from 22-24 degrees on a 41,000 year cycle

A

Obliquity

49
Q

Earth’s axis “wobbles” on a 26,000 year cycle

A

Precession