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Wildlife Ecology and Management> Major Bioms > lecture notes


This section is a brief introduction to Physical Geography and Biogeography

Please follow the links for more information.

..

 

1. BIOMS: Major ecosystems on Earth

   
     

Physical Geography

SUN:
Source of energy for EarthShort wave radiation to upper level atmosphere: 2 cal/sq cm/min
To surface: 50%

 
     
Back-radiation: long-wave (green-house effect)  
     
Glass ~ large molecules
Greenhouse gases:
water (H2O), nitrous oxide (N2O), methane (CH4), and carbon dioxide (CO2)

Aerosol particles (brown cloud)

Methane: 60% of global methane emissions are caused by human-related activities
fossil fuel production, animal husbandry (enteric fermentation in livestock and manure management), rice cultivation, biomass burning, and waste management.

nitrous oxide: human-related sources of N2O are agricultural soil management, animal manure management, sewage treatment, mobile and stationary combustion of fossil fuel, and nitric acid production. Naturally from a wide variety of biological sources in soil and water, particularly microbial action in wet tropical forests.


 
     

Brown cloud: aerosol particles from woodfire, cars, factories
Ramanathan et al. 2007. Nature: abstract, news
Measured aerosol concentration and solar fluxes directly by light weight aeroplans.
Brown clouds enhanced atmospheric solar heating by 50%

Atmospheric brown clouds are mostly the result of biomass burning and fossil fuel consumption. They consist of a mixture of light-absorbing and light-scattering aerosols and therefore contribute to atmospheric solar heating and surface cooling. The sum of the two climate forcing terms—the net aerosol forcing effect—is thought to be negative and may have masked as much as half of the global warming attributed to the recent rapid rise in greenhouse gases.... Here we use three lightweight unmanned aerial vehicles that were vertically stacked between 0.5 and 3 km over the polluted Indian Ocean. ... We found that atmospheric brown clouds enhanced lower atmospheric solar heating by about 50 per cent... . We propose that the combined warming trend of 0.25 K per decade may be sufficient to account for the observed retreat of the Himalayan glaciers

 
     
     
Why are tropics hot?
Equator: sunlight perpendicular
More energy / unit on surface
 
     

Why are winters cold? Axis is tilted by 23,5 0.

Please read Fredrik Venold's essay on seasonal temperature changes in Oslo (student assignment)

 
     
Air rises at Equator
Travels to Poles
Sinks at Poles
Travels back to Equator

Steady winds from the Poles?

No, not really...

What's going on here?

 
     

The Earth is rotating: Coriolis force

 

 
     

Earth rotates on its axis from West to East

Air lags behind

Coriolis effect

Rotating Earth breaks up air currents into six coils

 
     
Major winds on Earth  
     
  Major warm and cold currents
     

Global warming causing ice-age in Europe?
Read this BBC - OU article
http://www.open2.net/landscapemysteries/article2_pg2.htm

Picture shows the Great Conveyor belt transporting energy to the North. See original pic and article here.

Student essay by Rickard Kohler here

 
     

Generation of precipitation

Heat, Evaporation, Air rising, Cooling, Cool air holds less humidity -> Precipitation

 
     
Uplift of air: cooling -> precipitation
Descending air (high pressure): no cloud formation
 
     

Mountains
Air is forced upward by mountain
Air cools
Precipitation
Dry air descents

Arid areas: deep in the continents, downwind of mountains

 
     

Convective uplift: air warms

 


Orographic uplift: mountains drive the air

 

Frontal uplift: warm and cool air clashes

 
     
Cold and hot winds meet

Hurrican: radar image
Eye of typhon

 
     
Biogeography    
     
Global temperature: 21st February 2006
 
     
Annual precipitation  
     
Warmth and water: photosynthesis

Figure: satellite image of chlorophyl avareged for 8 years.

   
     
 
   
     
  Major bioms (dependence on precipitation and temperature)
  • TUNDRA
  • BOREAL FOREST or TAIGA
  • TEMPERATE BROADLEAF DECIDUOUS FOREST
  • TROPICAL BROADLEAF EVERGREEN FOREST
  • TROPICAL SAVANNA
  • DESERTSCRUB
  • TEMPERATE GRASSLANDS
  • MEDITERRANEAN SCRUB
     
Please, note: you need to be able to fill in the blank graph  
     
Bioms and vegetation  
     
  Terrestrial bioms of Earth
     

Tropical Broadleaf Evergreen Forest: The Rainforest

Precipitation: 200 – 400
Temperature: 20-350C
High growth rate
Tall trees – shadow - levels
Forest floor, understory, canopy, emergent layer

High productivity
2 million species (50% of all)

more

 
 
     

Why are tropics wet?


Although rain forests create most of their rain,

 
     
winds also bring humid air from oceans to rainforests  
     

DESTRUCTION OF RAIN FORESTS

  1. Commercial logging
  2. Clearing land for grazing animals and for
  3. Subsistence farming

Shallow soil, low carrying capacity, agriculture cannot be sustained, erosion
Carbon to atmosphere: adds to global warming

 
     

SAVANNAS: tropical grasslands

Rainfall: 75-125 cm Rain is seasonal
Temperature < 18 oC
Vegetation: perennial grasses (controlled by grazing – fire)
Fauna: greatest diversity of ungulates > 40 species more

 
     
 
     
DESERT, DESERTSCRUB    

Rainfall:
< 25 cm

more

 
     

TEMPERATE GRASSLANDS (Prairie, pampa, steppe, puszta)

Precipitation: 25-50 cm (rain and snow) more

 
     

Vegetation. Perennial grasses and perennial forbs

No grazing: invasive plants

 
     

TEMPERATE (MEDITARRANIAN) SCRUB: Chaparral

Precipitation: 40-100 cm (summers are dry!)
Vegetation: (evergreen) shrubs

more

 
     

Regular burns stabilize vegetation.

Global warming: frequent fires

 
     

TEMPERATE BROADLEAF DECIDUOUS FOREST

Precipitation: 50 – 150 cm
Temperature: ~ 6 month growing season

More

 
     

TAIGA OR BOREAL FOREST

Largest terrestrial biom
Rainfall: 40 – 100 cm (mostly snow) (but low evaporation, high humidity)
Temperature: 50-100 frost free days
Vegetation: Needleleaf trees

Fauna: large herbivores, fur-bearing predators more

 
     
Trillemarka area: the last unlogged landscape in Norway wiki
Temperate coniferous forests (taiga or boreal forest)
   

 
     

TUNDRA

Tundra: from Finnish „tunturia”= treeless plain
Temperature: extremely low (3-12 oC in summer)
Precipitation: variable (15 – 25 cm)
Arctic tundra

 
 

extremely short growing season,
low primary production

More

Alpine tundra (mountains)  
     

HUMAN IMPACT    
Exponential growth during industrial phase  
     
Mexico city today and in 1628  
     
     
     

Human impact

greenhouse gases

 
     
insecticides: DDT was banned (Stockholm Convention), however, traces of DDT can be detected in YOUR tissues.
 
     
Ozone hole  
     
     
     
     

IN THE NEWS (follow the links if interested)    

 

  • How to Buy Time in the Fight against Climate Change: Mobilize to Stop Soot and Methane SciAm
  • Sperm whale faeces 'offset CO2 emissions' BBC
    Iron defecation by sperm whales stimulates carbon export in the Southern Ocean html
  • A new study from Toronto researchers suggests that the collapse of a large portion of the Antarctic ice sheet would shift the very axis of the Earth. here
   
     
     
     

See aquatic bioms here

excellent pdf file on bioms here

   

 

 

Page written by: peter kabai 
 
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