EVPP 110 Lecture
Instructor: Dr. Largen Fall 2002
Physical Environment:
Climates, Biomes
Ecosystems
Ecosystem
a concept in which the physical and biological components of the environment are considered as a single, interactive system
two main categories
Ecosystems & Biomes
Ecosystem
similar physical environments lead to
- the evolution of organisms similar in form and function
- similar ecosystems
this is known as the rule of climatic similarity
- leads to the concept of the biome
- which is a kind of ecosystem
Ecosystems & Biomes
Biomes
major communities of organisms that
- have a characteristic appearance
- are distributed over a wide land area
- defined largely by regional variations in climate
Ecosystems & Biomes
Biomes
the strong relationship between climate and life suggests that
- if we know the climate of an area
- we can predict what biome will be found there
- approximate biomass
- approximate productivity
- dominant types of organisms
Ecosystems and biomes
distribution of biomes results from interaction of
physical features of the earth
two key physical factors
- amount of solar heat
- global atmospheric circulation
together these factors dictate local climate
two most important climatic factors are
- precipitation
- temperature
Climate shapes the character of ecosystems
why are there variations in the earth’s climate?
different parts of the earth receive different amounts of energy from the sun
- variations in the amount of energy received from the sun
- responsible for
- many of the major climatic differences on the earth
- and, indirectly, for much of the diversity in the earth’s biomes
Climate shapes the character of ecosystems
why the tropics are warmer?
since the earth is a sphere, some parts receive more energy from the sun than others on a per unit area basis
- tropics are warmer than temperate regions
- because they receive more sun energy per unit area
- poles are colder than other areas
- because they receive less sun energy per unit area
Climate shapes the character of ecosystems
key natural and physical elements
precipitation
all organisms require water
on land, water is often scarce
important aspects
total amount per year
form in which it arrives
seasonal distribution
ecosystem productivity increase with increased precipitation
Climate shapes the character of ecosystems
key natural and physical elements
precipitation
generally low near 30°
N & S latitude
where air is descending & warming
partly as a result of this, all the great deserts of world lie near 30°
N or S latitude
other major deserts are formed in the interiors of large continents
where precipitation is limited because of the great distance from the sea, the ultimate source of most moisture
Climate shapes the character of ecosystems
key natural and physical elements
precipitation
precipitation is generally higher near equator and 60°
north and south latitude
where air is rising & cooling
- releasing moisture it contains as its ability to hold the moisture decreases as temperature decreases
Climate shapes the character of ecosystems
key natural and physical elements
precipitation
can produce deserts
some mountains intercept moist winds from the sea
- air encounters mountains & then rises
- as air rises, its ability to hold moisture decreases
results in increased precipitation on the windward side of mountains (the side from which the wind is blowing)
Climate shapes the character of ecosystems
key natural and physical elements
precipitation
can produce deserts
air descends the other side of the mountains (the leeward side)
- is warmed & moisture-holding capacity increases
- which tends to inhibit precipitation
example, Sierra Nevada Mountains of CA
- eastern sides much drier than western sides & vegetation often very different
Climate shapes the character of ecosystems
key natural and physical elements
temperature
- most organisms are adapted to live within a relatively narrow range of temperatures
- won’t survive if temperatures are significantly warmer or colder
- ex., growing season of plants is influenced by temperature
- ecosystem productivity increases with increased temperature
Climate shapes the character of ecosystems
key natural and physical elements
temperature is affected by latitude
temperatures higher in tropics
- more sunlight falls per unit area
highest mean global temperatures occur near equator
there are no seasons in the tropics
- there is little variation in mean monthly temperature in tropical ecosystems
Climate shapes the character of ecosystems
key natural and physical elements
temperature is affected by latitude
temperatures decrease as you move from the equator toward temperate latitudes
- less sunlight strikes earth per unit area
temperature variations increase because of increasingly marked seasons
Climate shapes the character of ecosystems
key natural and physical elements
temperature is affected by elevation
higher altitudes become progressively colder
at a given latitude, air temperature falls about 6°
C/1000m increase in elevation
ecological consequences of temp varying w/elevation = temp varying w/ latitude
Climate shapes the character of ecosystems
key natural and physical elements
temperature is affected by elevation
higher altitudes become progressively colder
in North America, a 1000m increase in elevation results in a temp drop ~ to that of an 800 km increase in latitude
this is reason "timberline" (the elevation above which trees do not grow) occurs at progressively lower elevations as one moves farther from the equator
Figure: Vegetation, Latitude, Altitude
Figure: Temperature and latitude
Biomes
Biomes
are terrestrial climax communities with wide geographic distribution
concept is useful for describing in broad terms
- the general structure of the ecosystem
- the types of niches present
of the same type from different areas will exhibit variations in the exact species present
affected by two nonbiological factors
- temperature
- precipitation
Biomes
Biomes
major biomes of the world
- desert
- grassland
- savanna
- tropical rainforest
- temperate deciduous forest
- taiga or boreal forest
- tundra
Biomes
deserts
dry places where rainfall is <25 cm/yr
- so little that vegetation is sparse and survival depends on water conservation
- world’s great deserts are located in the interiors of continents
- Sahara in Africa
- Gobi in Asia
- Great Sandy Desert in Australia
Biomes
deserts
organisms have evolved adaptations to help them survive
- restricting activity to times of the year when water is present
- avoiding high temperatures by living in deep, cool, & moist (sometimes) burrows
- emerging only at night when temperatures are lower, especially if active year round
- drinking large quantities of water when it is available (camels) &then survive long, dry periods
Figure 6.10a: Climagraph for Cairo
Figure: Desert biome and climagraphs
Biomes
Grasslands
also known as temperate grasslands, prairies, steppes
widely distributed throughout temperate regions
- ~ halfway between equator & poles
rainfall is ~ 25cm -75cm per year
tend to be windy with hot summers, cold to mild winters
grasses make up 60%-90% of the vegetation
Biomes
Grasslands
once covered much of interior North America, were widespread in Eurasia & South America
- often highly productive when converted to agricultural use
- many of the agricultural lands of the US & Canada were originally occupied by grasslands (prairies)
- roots of perennial grasses characteristically penetrate far into soil
- grassland soils, therefore, tend to be deep and fertile
Biomes
Grasslands
temperate grasslands are often populated by herds of grazing mammals
- in North America, huge herds of bison and pronghorns once inhabited the prairies
- herds are almost all gone now
- most of the prairies have been converted into the richest agricultural region on earth
Figure 6.11a: Climagraph for Tehran
Figure: Temperate grassland biome and climagraph
Biomes
Savanna
great grasslands located in dry climates that border the tropics
transitional between tropical rainforest and desert (on global scale)
rainfall is 50cm-150cm /yr & occurs seasonally
- period of heavy rainfall followed by prolonged drought
predominant plants are grasses
- with widely spaced, drought resistant trees
landscape is open
Biomes
Savanna
many of its animals and plants are active only during the rainy season
fire is common and trees tend to be fire-resistant
savannas are increasingly being converted to agricultural use
- causing the inhabitants of savannas to struggle to survive
Figure 6.12a: Climagraph for Rangoon
Figure: Savanna biome and climagraph
Biomes
Tropical rainforest
rainfall is >200cm/yr
temperatures are warm and relatively constant, no frost
richest ecosystems on earth
- contain ~ half of all species of terrestrial plants and animals
- in 1sq mi of tropical forest in Rondonia, Brazil there are 1200 species of butterflies
- which is twice the number found in the U.S. and Canada combined
Biomes
Tropical rainforest
communities are diverse
- each kind of organism is often represented in a given area by only a few individuals
located near the equator
- South America, Africa, southeast Asia
are being destroyed
- many of the species in rainforests have never been seen by humans
- during our lifetime, a quarter of the world’s species will disappear with the rainforests
Figure 6.13a: Climagraph for Singapore
Figure: Tropical rain forest biome and climagraphs
Biomes
temperate deciduous forests
rainfall is 75cm-100cm per year
in areas with warm climates (warm summers and cool winters)
- plants grow actively for ~1/2 year
found in northeastern US, eastern Canada, Eurasia
often populated by deer, beaver, bear, raccoon
generally have a lower number of species but a higher number of individuals per species
trees are the major producers
Figure 6.14: Climagraph for Chicago
Figure: Temperate deciduous forest
Biomes
Taiga
rainfall is 25cm-100cm per year
- climate is humid due to low evaporation resulting from generally low temperatures
winters are long and cold
northern forests of coniferous trees such as hemlock, spruce, fir
- needle-shaped leaves limit moisture loss
- pyramid shapes accommodate snow
is one of the largest ecosystems on earth
Biomes
Taiga
has very short growing season for farming so few people live there
populated by many types of large mammals and carnivores such as moose, elf, deer, wolves, bear, lynx
has been used for fur trapping and lumber production
located in a ring that extends across vast areas of Asia and North America
also known as boreal forest, northern coniferous forest
Figure 6.15a: Climagraph for Moscow
Figure: Taiga biome and climagraphs
Biomes
tundra
located in the far north of the taiga and south of the polar ice
rainfall is <25cm/yr
soil layer is known as permafrost
extremely cold and windy
open, grassland that is often boggy
enormous ecosystem that covers 1/5th of the earth’s land area
Biomes
tundra
no trees grow in the area
herbs are perennials that grow rapidly during the brief summer
populated by large grazing mammals such as musk-oxen, caribou, reindeer and carnivores such as wolves, foxes, lynx
Figure 6.16a: Climagraph for Fairbanks
Figure: Tundra biome and climagraphs
Figure: World Biomes
Figure 6.8: Influence of precipitation and temperature on vegetation
The End