Earth's Biomes and Spatial Diversity Flashcards

1
Q

climate

A

long term average weather

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2
Q

solar radiation angle and surface temperature

A

sun hits the equator directly - hotter
at the poles, light hits less directly and is spread further - cooler
earth tilts 23.5 degrees - seasonal variation (more sun/closer in summer). variation is most impactful at poles

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3
Q

topography

- mountains

A

physical features of the earth

mountains can be glaciated to reflect heat

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4
Q

ocean currents and wind and heat movement

A

move heat to poles - equator is less hot than expected and the poles are warmer

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5
Q

wind and ocean current mechanisms

A
  • hot air rises from equator and spreads towards poles, cooling as it goes. eventually it is dense enough to return to the surface where it heats and moves towards the equators
  • series of cells (heating and cooling cycles)
  • when warm air moves up, cool air replaces it (wind)
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6
Q

Coriolis effect

A

because of the earth’s counterclockwise rotation about its axis, winds and oceanic currents in the Northern Hemisphere deflect to the right and those in the south deflect to the left

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7
Q

earth’s rotation and winds and water

A

earth rotates clockwise - equator moves furthest and fastest in a spin

  • wind push oceans to form currents in surface water
  • water carries more heat than air and moves to the poles
  • cold water sinks and moves to equator
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8
Q

rainfall

A
  • warm air carries more water vapour than cold air
  • rising air cools = rain
  • descending air warms, taking more moisture = arid climate
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9
Q

rain shadows

A

the area on the lee side of mountains, where air masses descend, warming and taking up water vapour; these lands are arid
- takes moisture into mountains where the air cools and it rains

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10
Q

biomes and distributions

A

distributions of biomes reflect regional climates

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11
Q

evapotranspiration

A

the sum of evaporation directly from soils and water bodies plus the amount transpired by plants

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12
Q

potential evapotranspiration

A

the amount of evapotranspiration that temperature, humidity and wind would cause if water supply wasn’t limiting; the demand on water in an ecosystem

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13
Q

potential evapotranspiration ratio

A

the ratio of water demand to supply - what vegetation can be supported?

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14
Q

plant evolution

A

evolve to conditions and may look similar but be unrelated

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15
Q

tundra

A

coldest, short days - grasses, moss, rabbits, wolves

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16
Q

alpine

A

lacks permanent ice below soil (tundra), cold, windy, small plants

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17
Q

taiga

A

cool, moist forests, rainy summers, conifers, mosses, shrubs, moose

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18
Q

temperate coniferous forest

A

lots of rain, enormous conifers, warm

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19
Q

deciduous forests

A

moderate climate, nutrient rich soil from leaf fall, lots of insects, lizards etc.

20
Q

temperate grassland

A

lack of precipitation (few trees), bison, horses, prairie dogs, foxes, eagles

21
Q

desert

A

deep-rooted plants, low nutrient soils, high salinity, not much primary production, small animals

22
Q

chaparral

A

30-75mm rain a year, herbs that die and reseed, shrubs, small trees, olives, eucalypts

23
Q

savanna

A

tall, perennial grasslands, warm, dry, seasonal rain, scattered trees, grazers, predators

24
Q

tropical rainforest

A

more than 250mm rain, warm, fast decay, small mammals, insects

25
Q

plants in aquatic biomes

A

buoyancy means plants don’t need structural support like those on land

26
Q

nutrients in aquatic biomes

A

dissolves in water
nutrients and oxygen supply impact biomes
nutrients run off continents into oceans; cyanobacteria fix nitrogen
nutrients from bottom upwell - 1% of earth supports 20% of fish

27
Q

fresh water

A

2.5%

glaciers, permafrost, groundwater

28
Q

oceans

A

71% of earth surface

29
Q

photic zone

A

top 200cm

30
Q

deep sea organisms

A

detritus and chemotropic bacteria and archaea support deep sea

31
Q

algae

A

occupy continental shelves and are grazed upon

32
Q

viruses

A

lyse phytoplankton and algae, releasing organic molecules that support bacteria and other consumers

33
Q

deep sea oxygen

A

less wind so less oxygen

34
Q

lakes

A

20% of freshwater, varying nutrients, plants and algae in shallows, cyanobacteria, zooplankton, fish, birds

35
Q

rivers

A

well oxygenated, plants and algae on edge, phytoplankton, fish, turtles, insects

36
Q

intertidal

A

neritic (shallow water), close to shore, rock pools, muscles, dry out daily

37
Q

coral reefs

A

most diverse, tropical/subtropical, little water movement, algae live in corals, low nutrients

38
Q

pelagic realm

A

not close to seashore or seafloor

39
Q

final oceanic region

A

deep sea

40
Q

physical factors of biodiversity’s unequal distribution

A

climate, topographical regions, barriers to movement

41
Q

biotic factors of biodiversity’s unequal distribution

A

depend on another species for survival

42
Q

evolution factors of biodiversity’s unequal distribution

A

large diversity of animals, plants etc. arrive at a place by chance and adapt to that environment

43
Q

cradle

A

high speciation rates - tropics are a cradle for diversity

44
Q

museum

A

low extinction rates in the tropics

45
Q

destination

A

high immigration rates