BIEB 174: Test 1

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101 Terms

1
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What is radiative equilibrium?

When incoming radiation is equal to outgoing radiation

2
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What is albedo? When is albedo high? When is it low?

The reflectivity of the Earth's surface. Albedo is high when the earth is very reflective, such as when it is snow-covered. Albedo is low when the earth is not reflective, such as when there's a dark tree covered forest.

3
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Explain the greenhouse effect and why the planet needs it

The greenhouse effect is when gaseous molecules get stuck in the earth's atmosphere and insulate the planet's warmth like a greenhouse. If this phenomenon did not happen or the atmosphere was not there, the earth would be too cold to host life.

4
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What causes atmospheric circulation?

Differential/uneven heating of the earth's surface due to be at different angles from the sun

5
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Name the processes of the hadley cell

At the equator, the air gets warmed by the sun at the intertropical convergence zone and rises. There is high rainfall here because the air is warm and moist. It then cools as it makes its way to the higher latitudes and sinks as cool, dry air. It gains moisture as it travels back to the equator.

6
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Where are the westerlies? What direction do they go in?

Westerlies occur in the mid latitudes. They go FROM the west to the east.

7
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Where are the easterlies/trade winds? What direction do they go in?

Easterlies occur in the poles (high latitudes). Trades occur in lower latitudes. They go FROM the east to the west.

8
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What is the relationship between sea surface height and currents?

Gravity affects sea surface height, gradients caused by this process causes currents.

9
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How does Ekman flux vary SSH in subtropical vs subpolar gures?

High SSH in subtropical, low SSH in subpolar

10
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What direction does Coriolis force deflect in the northern hemisphere?

to the right

11
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What direction does Coriolis force deflect in the southern hemisphere?

to the left

12
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If wind is blowing in a certain direction 0 degrees, at what angle do we expect the surface current to travel from it? What angle do we expect Ekman transport to travel from it?

Sea surface current will travel 45 degrees from the wind. Ekman transport will travel 90 degrees from the wind.

13
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Which direction will Ekman transport go in the northern hemisphere?

To the right

14
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Which direction will Ekman transport go in the southern hemisphere?

to the left

15
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Which direction do we expect geostrophic currents to flow in the northern hemisphere? What mechanism causes it?

Water will flow to the right due to the pressure gradient caused by the Coriolis effect

16
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Do subtropical gyres have upwelling or downwelling? How does this affect temperature, nutrients, and chlorophyll?

Downwelling

Higher temperatures, lower nutrients, lower chlorophyll

17
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Do subpolar gyres have upwelling or downwelling? How does this affect temperature, nutrients, and chlorophyll?

Upwelling

Lower temperatures, higher nutrients, higher chlorophyll

18
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What drives ocean gyres?

Wind

19
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What determines the distributions of Earth's biomes?

Spatial variations in temperature, precipitation, nutrients, light, and other environmental factors

20
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Define features of the biome tropical wet forest

consistently warm, rainy

found largely along the equator and near the ITCZ

21
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Define features of the biome tropical dry forest

consistently warm, seasonally dry

typically have wet summer season and drier winter

22
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Define features of the biome tropical grassland/savannahs

consistently warm, seasonally rainy

tree cover limited by precipitation but also fire

23
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Define features of the biome warm deserts

exceptionally dry

very hot summers, cool in the winter

24
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Define features of the biome temperate forest

seasonally cold and low light, relatively high precipitation

coniferous or deciduous

25
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Define features of the biome boreal forest/taiga

very cold, low light in winters, warmer in summer

generally found in continental interior of the northern hemisphere

26
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List some of the global carbon pools

Most held in rocks on very long timescales
After that, most in oceans as DIC
Then other ones are atmosphere, soils, terrestrial biota, and fossil fuels

27
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List some of the global carbon fluxes

ocean uptake, rivers, volcanoes, burial to sediments, deforestation and land use change, photosynthesis, respiration, and burning of fossil fuels

28
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What is the solubility pump?

Solubility increases with lower temperatures, that cold dense water sinks in the north Atlantic and southern ocean.

Very little water sinks in the north pacific ocean, so water in the deep pacific ocean has been away from the atmosphere for a very long time

29
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What is the relationship between DIC and depth

DIC increases with depth

30
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What is the relationship between DIC and time and why

it is constant because the solubility pump is constant

31
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What does solubility of CO2 depend on?

temperature and salinity. Colder water is more soluble

32
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How does dissolution of CO2 affect the water's pH?

dissolution of CO2 will cause a reaction that will release an H+ ion, so an acid will be created and therefore the water's pH will be lowered and it will become more acidic

33
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What does it mean when the pH is lowered by one?

The H+ concentration has increased by a factor of 10

34
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What happens if high DIC water upwells?

It can lead Co2 to outgass into the atmosphere

35
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What is the Redfield Ratio?

The ratio of different nutrients are required in different proportions. For phytoplankton, it is 106:16:1 for N:P:C

36
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What is remineralization?

Nutrients that were once taken up by phytoplankton are ultimately released back into the water (respiration increases DIC)

37
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Describe how the biological pump works

Organic matter is created at the surface, but sinks due to gravity. As it falls, its broken down mechanically or chemically. As you go further down, less and less material is leftover and it is used by respiration. Most of the organic matter is remineralized and returns the nutrients back into the water. Less than 1% of the organic matter flux from the surface arrives into the deep ocean. This flux increases DIC and nutrients in the deep ocean

38
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Does solubility pump or biological pump add more DIC to deep ocean?

Solubility pump. 90% of deep ocean DIC is because of the solubility pump while 10% is because of the biological pump.

39
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If there was no biological pump, what effect would we see on climate?

We would expect atmospheric CO2 to increase by about 200ppm and the climate would be much warmer

40
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How are anthropogenic carbon emission accumulations divided up by atmosphere, terrestrial, and marine systems?

1/2 atmosphere, 1/4 marine, 1/4 terrestrial

41
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How does the addition of nutrients influence primary production and biomass?

More nutrients means more primary production and more biomass

42
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Major pools of nitrogen

Atmosphere, sedimentary rocks, and the ocean. Smaller ones include soil organics, land biota, and marine biota

43
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Major nitrogen fluxes

Fertilizer, burning of fossil fuels, deposition, N2 fixation, denitrification, nitrification, atmospheric deposition

44
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Why is atmospheric N2 not important for ecosystems?

It is not available to be used as-is, it must be fixed through nitrogen fixation into a bioavailable form

45
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Is N fixation more on land or in the ocean?

They are approximately equal

46
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How has anthropogenic N inputs changed through time?

Historically they were negligible but now they are almost equal to total terrestrial nitrogen fixation

47
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What is denitrification?

Removes nitrogen from the ecosystems back into N2 gas. Anaerobic process facilitated by heterotrophic bacteria. Occurs in low O zones (oxygen minimum zones) and in soils where nitrate and carbon is present

48
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Why is nitrogen important?

It is a key macronutrient required by plants and phytoplankton

49
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Explain the steps in the MARINE nitrogen cycle

atmospheric n2
n fixation into ecosystem and bioavailable as ammonia (NH4)
nitritification into no2- nitrite
nitrification into no3- nitrate

>nitrate can be denitrificated into atmospheric n2
>OR assimilated into phytoplankton then remineralized into ammonia from detritus

50
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Explain the steps in the TERRESTRIAL nitrogen cycle

atmospheric n2
nitrogen fixing bacteria in root nodules
OR n fixation into ecosystem and bioavailable as ammonia (NH4)
nitritification into no2- nitrite
nitrification into no3- nitrate

>nitrate can be denitrificated into atmospheric n2
>OR assimilated into plants
>then remineralized into ammonia by decomposers
> then consumed by animals, who are then remineralized into ammonia by decomposers

51
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What is nitrogen fixation

Atmospheric N2 is converted into bioavailable ammonium

52
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Where can we expect to find nitrogen fixers?

In areas of low nitrogen but high phosphorous, ample light and aerobic conditions

53
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What is the Haber-Bosch process? What is it used for and why is it unique?

Converts N2 to NH3 (not NH4) under higher temperatures and pressure than traditional N fixation. It is used to produce N for fertilizer and is unique because it is a man-made process of artificial fixation

54
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What is nitrogen assimilation?

Takes up nitrogen (and C and P and others) from the environment to make organic matter. N can be a limiting factor. N is assimilated through molecular diffusion.

55
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Why is the assimilation of nutrients limited in phytoplankton?

Cells have limited number of membrane transport proteins due to their size.

56
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What is nitrogen remineralization?

A process that returns fixed nitrogen into ammonium in water/soil from organic matter. Ultimately facilitated by heterotrophic bacteria.

57
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How does nitrogen remineralization change with water temperature?

Faster with warmer water temperature

58
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What is nitrification

A 2 step process where ammonia goes to nitrite and nitrite goes to nitrate. It is aerobic and inhibited by light. It acidifies the soil/water and the reactions and driven by bacteria

59
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where do we expect the highest levels of denitrification?

In anaerobic soils with high nitrate levels

60
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Where do most ammonium levels peak?

At around 50-100m because most decomposition occurs there

61
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What are the expected projections for changes in anthropogenic N inputs?

Fertilizer and agricultural inputs will likely increase but combustion inputs will likely decrease

62
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What are the expected projections for changes in biological N2 fixation?

May increase but by how much is uncertain

63
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What causes oxygen minimum zones?

sinking organic matter, which consumed oxygen (more likely to occur if surface productivity is high and biological matter to depth is strong)

64
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How can burning of fossil fuels lead to forest die-offs?

Burning fossil fuels emits large amounts of nitrogen oxides, which can react with water to create nitric acid. Acid deposition can lower the pH of soil in areas of high depositions well as change soil and water chemistry. Forest die-offs can occur because of the change in soil pH and the addition of a new acid

65
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How can addition of N change plant diversity?

Adding N to plant communities can increase primary productivity but lower species diversity. More N causes plants to grow faster and taller, which can out-shade and out-compete understory plants

66
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What are the major pools of the phosphorous cycle

rocks and sediments; deep ocean have long residence times

terrestrial biota holds more P than the ocean, as there are faster turnover rates

67
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What are the major fluxes of the phosphorous cycle

weathering, recycling, river flux, biological pump, upwelling, fertilizer. burial, remineralization

68
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Why is P important?

Used in the creation of DNA/RNA and for ATP and phospholipid membranes

69
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Why is P difficult to obtain? How is it made bioavailable?

Tightly bound in insoluble compounds. Made bioavailable slowly through weathering processes

70
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What is the most limiting nutrient in terrestrial primary production?

P

71
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What is the most limiting nutrient in marine primary productioin?

Fe

72
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How have humans interfered with the P cycle?

Recently we've seen an increase of P added into fertilizer, so there has been an increase of flux of P in the ocean through runoff due to human activities

73
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Why is the sulfur cycle important in providing stabilizing feedback for climate?

The S cycle is responsible for cloud condensation nuclei and aerosols, and increased CCN can lead to high albedo and cool climate.

74
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Explain how the S cycle works

Aqueous dimethyl sulfate turns into atmospheric dimethyl sulfate, which turns into cloud condensation nuclei

75
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Why is S important

Required for proteins and enzymes (Including nitrogenase)

76
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What are the major pools of the sulfur cycle

rocks, ocean

small amount in the atmosphere

77
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What are the major fluxes of the sulfurcycle

volcanoes, aerosols, acid deposition

78
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How can S acid deposition affect pH in soils?

It can lower it and cause the soil to be more acidic. Can chemically change soil and water and thus ecosystems

79
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Explain how sulfate aerosols can affect albedo

Sulfate aerosols in the atmosphere can accumulate and increase albedo in the atmosphere, potentially leading to cooling effects on climate

80
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Why is iron a necessary nutrient

Needed for photosynthesis, respiration, and N fixation

81
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What is the largest pool of iron? Why is it still scarce?

Continental rocks. It is highly scarce in a bioavailable form and almost doesn't exist on the oceans surface its that rare

82
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Why is Fe so rare in the ocean?

Competition for scavenging, binding with organic ligands, and is taken up by phytoplankton

83
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What is the most important source of Fe in the ocean?

Dust

84
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If most Fe is taken up by phytoplankton, then how is it used by others?

Through recycling of organic matter

85
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What is Liebig's Law of the Minimum?

Production is limited by the factor in least abundance

86
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What's interesting and special about Diazotrophs?

They are a symbiotic N fixing bacteria living in phytoplankton. But they can be found in areas of low nitrogen and are limited by low iron and P

87
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What is an HNLC region and why does it occur?

An HNLC region is an area with high nutrient but low chrlorophyll.

This occurs because even though there is high abundance of nutrients as a whole, there is a severe scarcity of a limiting nutrient

88
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Explain what the Iron fertilization experiments were and what they showed us

Experiments where adding Fe to the ocean increased chlorophyll and changed the community structure to a large cell dominated regime shift. It spurred growth until N and P were consumed as they were the new limiting factors

Shows us that Changes in iron availability throughout earth's history may be linked to large scale changes in climate's state

89
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Explain the difference between a food chain and a food web

A food chain is a group of organisms that are linked together by consumption

A food web is a conjoining of many complex and interwoven food chains

90
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Contrast heterotrophs and autotrophs. How are mixotrophs related?

Autotrophs create organic matter through photosynthesis while heterotrophs derive energy from eating organic matter

Mixotrophs are able to consume organic matter but also photosynthesize

91
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What is a typical trophic efficiency?

About 10%

92
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What does it mean if trophic efficiency is at 20%?

Production by trophic level 1 is 5x greater than trophic level 2. Production by level 2 is 1/5th as much as trophic level 1.

93
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What is consumption efficiency?

The proportion of lower trophic level that is ingested by the next level (ie. half of deer eaten by wolves would be 0.5)

AMOUNT OF PREY BEING EATEN

94
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What is assimilation efficiency?

Proportion of ingested energy that is assimilated into an organism (ie. diffused across the stomach lining)

AMOUNT OF NUTRIENTS FROM PREY BEING ABSORBED

95
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What is production efficiency?

Proportion of assimilated energy that is converted into consumer production (ie. whats left over after basic cost of living that can be used for growth)

AMOUNT OF OF SURPLUS NUTRIENTS FROM PREY BEING ABSORBED THAT CAN BE USED FOR EXTRA PROCESSES SUCH AS GROWTH

96
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What is the trophic efficiency formula

Trophic Efficiency=Consumption Efficiency x Assimilation Efficiency x Production Efficiency

97
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What is top-down control

Higher trophic levels control structure of lower trophic levels (ex. predators present, reduced herbivores, more plants; predators absent, herbivores abundant, less plants)

98
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What is bottom-up control

Environmental conditions and primary producers control ecosystem structure (ex. plant defenses to protect against herbivores limit how much the herbivores can eat; harmful algal blooms produce toxins that can be harmful to all other organisms)

99
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Why is consumption efficiency low for ecosystems with woody plants

Large fraction of biomass is not eaten by herbivores

100
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Why are aquatic primary producers more rich in N and P than terrestrial plants? Why does this increase their trophic efficiency?

Aquatic primary producers dont need to build tall carbon structures to compete for light, so they can save that N and P.

heterotrophs need that N and P, so they are a better food source than plants are and they have a higher grazing pressure on them