Physical Geography Flashcards
(40 cards)
Def 1. ecosystem
2. autotrophs
3. heterotrophs
- the biological, physical and chemical factors that make up its non living abiotic environment eg pond
- produce own food from substances available in their surroundings using photosynthesis or chemosynthesis- self feeders primary producers
- can’t synthesise food and rely on others
scales of an ecosystem
micro - under stone local scale
habitat- feild local scale
zone - coastal/river mesoscale
biome - climate region global scale
def
1. biome
2. fauna
3. flora
4. biotic
5. abiotic
- a large area on the earths surface complex collection of micro, habitats and zones that all interact with eachother controlled by local climate patterns
- animals
- plants
- living environment- fungi
- non living environment - humidity
,
def
1. soils
2. vegetation
3. decomposers
- made up of weathered rock fragments, decomposed organic matter, supports amount of water available provides nutrients
- 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
- organisms which cause the breakdown/decay of organic matter facilitate the recycling of nutrients from litter to soil
name
1: inputs
2. stores/transfers
3. outputs
- nutrients from weathered rocks
- plants animals decomposers
- nutrients leached from soil CO2 water heat
def
1. biomass
2. dead organic matter
3. productivity
- tot amount of living matter present at any given moment in an ecosystem expressed as dry weight
- made up of surface litter and soil humus exceeds the living biomass in volume weight
- process of absorbing light energy in plants
explain gersmehl model
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
vegetation succession
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
types of succession
lithosere bare rock
hydrosere water
halosere salt
psammosere sand
tundra characteristics
coldest
low biotic diversity
simple veg structure
limitation of drainage
short season growth and reproduction
energy in the form of dead organic material
artic tundra
alpine tundra
temperate grasslands
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
hot desert
tropical rainforest
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
Soil forming factors
organisms assisting in decomposition
topography shape of land
climate
parent material
time
soil profile
organic
surface
subsoil
substratum
bedrock
soil processes
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
soil characteristics
depth older is deeper
colour- chemistry
acidity - fertility
structure- combination
texture - particle sizes
temperate grassland soil profile
6-7 pH
1m+ depth
texture - loam clay
thick sod layer
deep layer of nutrient rich
deep topsoil
soil processes un chernozems molisols
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
Describe tundra in barrow alaska
-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
characteristics of the tundra
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
development of the tundra
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
effects of climate change on tundra
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
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
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
def of weather and climate
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