the biosphere
all spaces on Earth where life exists
climate
average weather conditions of an area over a long period of time. cloud cover, temp., humidity, and wind speed
where do air circulation patterns begin?
at the equator
30° latitude
many of the world’s great deserts are located here, including the Sahara
prevailing winds
a wind from the direction that is predominate a particular place or season
winds are named..
for the direction from which they blow.
influences on the directional movement of ocean currents
the force of major winds, Earth’s rotation, topography
coastal breezes
arise because of differences between the ability of water and land to absorb and release heat
monsoon
also arises from differential heating of water and land. wind that reverses direction seasonally
rain shadow
dry region downwind (leeward) of a coastal mountain range
leeward
mountain side facing away from the wind
ENSO
The El Niño Southern Oscillation. naturally occurring, irregularly timed fluctuations in sea surface temperature and wind patterns. occurs in equatorial pacific
biomes
distinctive biological communities that are adapted to particular physical conditions, characterized by predominant vegitation
deserts
receive an average of 10cm (4 inches) or less rainfall per year. located mainly at 30° latitude or in the rain shadow of a mountain range.
desert crust
a community that can include cyanobacteria, lichens, mosses, and fungi. secrete organic molecules that glue them to the soil. holds soil particles in place
temperate grassland
warm in the summer, cold in the winter. annual rainfall 10-40 in, with rains throughout the year. form in the interior of continents between deserts and temperate forests. cannot support woodlands.
tropical savannas
broad belts of grasslands with a few scattered shrubs and trees. 35-60in of rain during rainy season. abundant wildlife. lie between the tropical forests and hot deserts of Africa, India, and Australia
dry shrubland
biome dominated by fire-adapted shrubs. typically occurs on continent’s western coasts between 30 and 40° latitude. hot, dry summers and mild, wet winters. plants tend to have small, leathery leaves to withstand summer droughts.
temperate deciduous forests
form in the Northern Hemisphere. 20-60in precipitation/year. warm summers, cool winters. rich soil, somewhat open canopy
tropical rain forests
Occur between latitudes 10 degrees north and south of \n the Equator in Africa, the East Indies, Southeast Asia, \n South America, and Central America. 50-80 in rain yearly. greatest primary production of any land biome. most structurally complex and species-rich biome. soils are poor in nutrients
conifers
evergreen trees with seed-bearing cones. leaves are typically needle-shaped tolerant of cold, drought, and poor soil
Boreal forests
also known as taiga or “swamp forest”. Extensive high-latitude forest of the Northern Hemisphere; conifers are the predominate vegetation. Sweeps across northern Asia, Europe, and North \n America
montane coniferous forests
Extend southward through the great mountain ranges of \n North America
arctic tundra
Occurs between the polar ice cap and the belts of boreal \n forests in the Northern Hemisphere. most in Russia and China. annual precipitation is less than 10 in. harsh condition, permafrost, home to lichens and shallow rooted low growing plants.
permafrost
under top layer of soil – continually frozen soil layer \n that lies beneath artic tundra and prevents water from draining
alpine tundra
occurs at high altitudes throughout the world, no permafrost. thin, nutrient-poor soil. has grasses and small leafed woody shrubs, strong winds discourage tree growth.
lake
body of freshwater divided into zones that differ in physical characteristics and species composition. undergo succession - change over time
littoral zone
extends around the shore to a depth where \n rooted aquatic plants stop growing
limnetic zone
is the open waters where light penetrates and \n photosynthesis occurs
profundal zone
area deep enough light cannot penetrate
new lakes
are oligotrophic. deep, clear, and nutrient poor
spring overturn
in temperate zone lakes, a \n downward movement of oxygenated surface water and \n an upward movement of nutrient-rich water in spring
thermocline
thermal stratification in a large body of \n water; a cool mid-layer stops vertical mixing between \n warm surface water above it and cold water below it
fall overturn
During the fall, water of a temperate \n zone lake mix. Upper oxygenated water cools, gets \n dense, and sinks; nutrient-rich water from the bottom \n moves up
estuary
partly enclosed body of water where freshwater from a \n nutrient-rich river meets and mixes with seawater. Freshwater floats on top of seawater where they meet
spartina
Dominant plant in salt marshes of the Atlantic \n coast. Has a gland on its leaves that allows it to \n excrete salt taken up by roots
coral reefs
wave-resistant formations of calcium carbonate secreted by coral polyps
pelagic province
“the oceans waters” water over continental shelves and more extensive water further offshore
benthic province
ocean bottom; sediments and rocks
seamounts
undersea mountains, abundance of life makes these attractive to commercial fishing vessels
hydrothermal vents
hot, mineral rich water spews out from an opening on the ocean floor