Physical Geography Flashcards

(40 cards)

1
Q

Def 1. ecosystem
2. autotrophs
3. heterotrophs

A
  1. the biological, physical and chemical factors that make up its non living abiotic environment eg pond
  2. produce own food from substances available in their surroundings using photosynthesis or chemosynthesis- self feeders primary producers
  3. can’t synthesise food and rely on others
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

scales of an ecosystem

A

micro - under stone local scale
habitat- feild local scale
zone - coastal/river mesoscale
biome - climate region global scale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

def
1. biome
2. fauna
3. flora
4. biotic
5. abiotic

A
  1. a large area on the earths surface complex collection of micro, habitats and zones that all interact with eachother controlled by local climate patterns
  2. animals
  3. plants
  4. living environment- fungi
  5. non living environment - humidity
    ,
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

def
1. soils
2. vegetation
3. decomposers

A
  1. made up of weathered rock fragments, decomposed organic matter, supports amount of water available provides nutrients
  2. autotrophs in an area affected by climate wnd soil uses nutrients available in the soil the growth, heat, moisture. nutrients return when leaves are shed ect
  3. organisms which cause the breakdown/decay of organic matter facilitate the recycling of nutrients from litter to soil
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

name
1: inputs
2. stores/transfers
3. outputs

A
  1. nutrients from weathered rocks
  2. plants animals decomposers
  3. nutrients leached from soil CO2 water heat
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

def
1. biomass
2. dead organic matter
3. productivity

A
  1. tot amount of living matter present at any given moment in an ecosystem expressed as dry weight
  2. made up of surface litter and soil humus exceeds the living biomass in volume weight
  3. process of absorbing light energy in plants
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

explain gersmehl model

A

width of arrows are proportional to rate ofto nutrient flow

describes how nutrients move from physical environment into living organisms and are recycled back to physical environment

must be balanced and stable

humans influence via removing land nutrients and discharging into aquatic environments

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

vegetation succession

A

directional non seasonal cumulative change in the types of plant species that occupy a given area through time. involving colonisation, establishment, extinction

stops when spieces composition changes no longer occur with time- climax community

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

types of succession

A

lithosere bare rock
hydrosere water
halosere salt
psammosere sand

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

tundra characteristics

A

coldest
low biotic diversity
simple veg structure
limitation of drainage
short season growth and reproduction
energy in the form of dead organic material

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

artic tundra
alpine tundra
temperate grasslands

A

N alaska, Canada , greenland, N russia
N hemisphere N of coniferous forests high latitudes 60°+

alpine tundra mountainous regions any latitude 10000ft+ rockies andes

Prairies Steppes

mid lats 30-40° N and S
more extensivein N continental interiors

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

hot desert
tropical rainforest

A

Mexico deserts, australian desert
15-30° N and S trade wind belt western side of continents

Amazon, congo basin, SE asia
on tropics 5° N and S trade wind

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Soil forming factors

A

organisms assisting in decomposition
topography shape of land
climate
parent material
time

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

soil profile

A

organic
surface
subsoil
substratum
bedrock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

soil processes

A

leaching - vertical movement of water if rainfall id greater than evaporation downward movement is dominant
upward capillary action - where rainfall is less thsn evaporatranspiration water is drawn upwards

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

soil characteristics

A

depth older is deeper
colour- chemistry
acidity - fertility
structure- combination
texture - particle sizes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

temperate grassland soil profile

A

6-7 pH
1m+ depth
texture - loam clay
thick sod layer
deep layer of nutrient rich
deep topsoil

18
Q

soil processes un chernozems molisols

A

formation of mull humus - summer grasses die and decomposed mixed by earth worms

slight leaching - snowmelt causing leaching moving K and Mg downward

capillary action- high summer temps and lack of soil moisture draws water and minerals upwards

calcification - calcium carbonate deposited downwards enhancing fert

rich organic material
1-2m
netural Ph
ideal structure

19
Q

Describe tundra in barrow alaska

A

-30° winters, little insulation from the song, long hours of darkness, cool summers, limited cloud cover, struggle to reach 10°

low precipitation high pressure dominates 110mm a year

frozen gelisols freeze and thaw a lot argoturbation

too cold for decomp permafrost preventing nutrient uptake

summer meltwater saturates soils activating top layer

limited agricultural ops

20
Q

characteristics of the tundra

A

flora diversity - no deep roots, wide variety of shallow root plants which are adapted to the cold/wind, long summer days allowed 24/7 photosynthesis, 50/60day growing season 400 kind of plants

infertile - acidic water logged topsoil and frozen during winter restrict reproduction and decomp

waterlogged - low evaporation, higher summer precipitation,

acidic - accumulation and concentration of hydrogen ions, higher summer precipitation water table, thick peat layer

nutrients - limited to summer

fauna diversity - hibernation, migration or lie dormant insects usr glycerol as antifreeze

21
Q

development of the tundra

A

transport- new sea/air routes new infrastructure but pollution

settlements - pollution disturbing permafrost loss of veg/habitat

renewable resources- eg water/fish/electric pollution, over hunting, habitat destruction

non renewable resources- eg fossil fuel pollution destruction of habitat, waste disposal, spills

tourism

political issues - conflict pollution exploitation

conservation of native cultures, landscapes, ecosystems

22
Q

effects of climate change on tundra

A

biotic
spruce trees/shrubs 2m+ overshadowing plants
Alaskan berries ripen 2 weeks earlier
arrival of exotic species in Alaskan rivers eg beavers
seberia reindeer hearders modify hearding techniques

abiotic changes
snow melts 10 days earlier than 1970s
summer growth season extended 1-3 weeks
n canada intuit groups summer lakes/marshes disappeared having to change fishing patterns
increased summer wildfires showing better surface drainage to allow veg to dry out
increased landslides/mudflows

23
Q

alaska north slope - 650 miles of coastline sparseley populated, 8 villages, 95km^2, 10000 people, 68° N Temperature has risen 4° fastest on earth what is the effect of this

A

thawing permafrost - 600 more lakes, 12 villages relocated (4000 ppl) however soft ground for oil drilling

increased wildfires/thunderstorms - 2000s were record high 3 times as many area burned to double by 2050. Caribous prey lichen take 50-100 years to grow but are being burnt, july 16th 2007 lightning ignited a fire burning 228500 acres for 2 months. however created more fertile soil

thawing glaciers /sea ice- glaciers loosing 75 billion tonnes a year most disappear by end of century , affecting water quality, 1.5m coastline lost everyyear, causing sea levels to rise endangering species however opens sea routes and tourism

24
Q

def of weather and climate

A

state of atmosphere at local level usually short time eg cloud rain sun

long term behaviour of the atmosphere represented by data arranged over long periods of time

25
describe structure of the atmosphere
80% gases found in troposphere thermosphere ———————mesopause mesosphere ———————stratopause stratosphere ———————tropopause troposphere troposphere varies in thickness from 8km in poles to 16km at the equator
26
describe the global balance
an open system the energy heats the surface which emits long wave energy back into the atmosphere which is absorbed by gases 68% absorbed 50 surface 21 clouds albedo = 32% its the reflective index of clouds and the earths surface
27
describe and give examples of horizontal heat transfers
heat transferred away from the tropics to prevent overheating and the poles freezing winds such as jet streams, hurricanes, depressions are responsible for 70% ocean’s currents = 30% eg N atlantic drift
28
def wind and factors affecting wind speed and direction
the movement of air caused by uneven heating of the earth. air is warmed by the tropical land/sea pressure gradient force - how wind apart isobars are wider = calmer Coriolis effect = earths rotation moving faster at the equator than poles gravity - different temperature and force exerted by gravity as pressure decreases with height friction lowest 1000m of air is slowed by friction
29
vertical heat transfers
convection- transfer of energy by the movement of a medium eg water to evaporate radiation- sun heating ground conduction- sea heats closest land
30
def of tricellular model and ITCZ and description of pressure belts
shows how energy is redistributed across the globe ITCZ low pressure belt - inter tropical convergence zone , high insolation , humid , at equator, surface evaporation, heavy rainfall when condenses subtropical high pressure belt - 30° N and S air carried polewards descends in high pressure area found between hadley and ferrel cells formation of deserts humid little rainfall polar front low pressure belts. - 60-70° N and S Air converges at low altitudes to ascend along the boundaries between cool polar air and warm tropical air wind between pressure belts most originate close to subtropical high pressure belt
31
describe hadley ferrel and polar cell
hadley - largest from equator to 30-40° N and S trade winds blow towards equator and ascend near equator ferrel - air converges at low altitudes to ascend along cool polar air and warm subtropical air 60-70° N and S moved in opposite direction to others polar - smallest and weakest 60/70 - poles N and S air sinks over highest latitudes and flows out towards lower latitudes at the surface
32
factors that influence air temperature
latitude- high latitude day length varies as sun height does not altitude - warmed by heat radiated off the earth’s surface temp drops 0.6 every 100 m continentality - land/water ability yo absorb and retain radiation seasonality - earth tilted so n hemisphere 6 months closer to the sun prevailing winds/ ocean currents - determined by area of origin type of land surface - white reflects more
33
Def of 1. Humidity 2. Dew point 3. Adiabatic cooling 4. Relief orographic rainfall 5. Frontal cyclonic rainfall 6. Conventional rainfall
1. How much water vapour is in the air 2. Air has 100% humidity 3. Process of reducing heat through a change in air pressure through volume expansion 4. Warm moist air forced to rise over a mountain range when descending creates dry low rain 5. Meeting of 2 air masses 6. When the ground is intensely heated by insolation air above rises cooling abatically
34
Def of 1. Air masses 2. Synoptic chart 3. Satellite images
1. Large body of air with similar temperature and humidity characteristics over 100s of km 2. Shows air pressure at the surface using isobars 3. Geostationary satellites orbit at 22300 miles above earths surface
35
Def of 1. Jet stream 2. Rossby waves
1. Between troposphere and stratosphere 17km above the earth at the equator strongest and most variable temp gradients meandering N and S 2. Formed when polar air moves towards the equator while tropical air is moving towards the poles
36
Low pressure systems depressions
Occurs 30-40 N and S Dominated by upper westerlies by the orientation of the polar jet streams Refer to notebook
37
High pressure systems anti cyclones Summer and winter
3km diameter air sinking from 8km towards the surface involving one air mass lasting days to weeks Cloud formation is inhibited so settled weather small cloud cover wide isobars light winds Summer - warm, dry, fine weather long sunny conditions high sun, can trigger thunderstorms, morning dew/mist, light winds, wildfires, flash floods, 17 hours daylight Winter - below 0 freezing, settled conditions, frost, fog, clear skies cause heat loss, light winds, frozen pipes burst - flooding, hypothermia in elders, icy pavements - injury’s
38
El Niño southern oscillation
Pressure/precipitation reverses occurs 3-7 years lasting 9-12 months Tropical trade winds causes warm water to build up on western side - warm wet conditions on eastern side cold waters are pulled up - cool dry conditions. Air travels towards the east descending - walker circulation Impacts - decreased rice production, Australian droughts, flooding in SA and CA, hard to fish in Peru due to change in sea temp, wet in the UK, hurricane seasons
39
Hurricane
Large intense large pressure systems with high winds, heavy rain, storm surges, Hot humid conditions over tropical oceans, not within 5 degrees of the equator move westward. 27C+ water, 119km+ winds, up to 11000 km. eye = 200-300km pressure under 800 mb, eye creates peace, 1st June - 30th November, land = dissipates
40
How hurricane forms
Surface air drawn upwards Strong convection uplift of hot damp air Beyond 5 degree of equator corolis effect occurs Clouds form spiral bands Rising air carries energy from evaporation released by condensation causing precipitation Process strengthens winds under 120km Cumulonimbus clouds extend to top of troposphere 12km Mature eye forms causing air to sink bringing calm Surface winds spiral inward towards low centre cyclonic flow Aloft air spirals outwards and clockwise Only decays and dies when moves over land or cold water