• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/69

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

69 Cards in this Set

  • Front
  • Back
Empirical Classification
classification process based on statistical, physical, or observable characteristics of phenomena; it ignores the causes or theory behind their occurrence
genetic classification
classification process based on the causes, theory, or origins of phenomena; generally ignoring their statistical, physical, or observable characteristics
Thornthwaite system
climate classification based on moisture availability and of greatest use at the local level; climate types are distinguished by examining and comparing potential and actual evapotranspiration
potential evapotranspiration
hypothetical rate of evapotranspiration if at all times there is a more than adequate amount of soil water for growing plants
actual evaportranspiration
the actual amount of moisture loss through evapotranspiration measured from a surface
Koppen System
climate classification based on monthly and annual averages of temperature and precipitation; boundaries between climate classes are designed so that climate types coincide with vegetation regions.
tropical climate
climate regions where it is warm all year
polar climate
climate regions that do not have a warm season and are frozen much or all of the year
microthermal climate
climate regions or conditions with warm or mild summers that have winter months with temperatures averaging below freezing
mesothermal climate
climate regions or conditions with hot, war, or mild summers that do not have any months that average below freezing
arid climate
climate regions or conditions where annual potential evapotranspiration greatly exceeds annual precipitations
highland climate
a general climate classification for regions of high, yet varying, elevations
region
areas identified by certain characteristics they contain that make them distinctive and separates them from surrounding areas
zone of transition
an area of gradual change from one regions to another
climograph
graphic means of giving information on mean monthly temperature and rainfall for a select location or station
microclimate
climate associated wiht a small area at or near Earth's surface; the area may range from a few inches to one mile in size
oxygen-isotope analysis
a dating method used to reconstruct climate history; it is based on the varying evaporation rates of different oxygen isotopes and the changing ratio between the isotopes revealed in foraminifera fossils
Altithermal
an interval of time about 7,000 years ago when the climate was hotter than it is today
eccentricity cycle
the change in Earth's orbit from slightly elliptical to more circular, and back to its earlier shape every 100,000 years
obliquity cycle
the change in the tilt of the Earths axis relative to the plane of the ecliptic over a 41,000 year period
precession cycle
changes in the time (date) of the year that periohelion occurs; the date is determined on the basis of a major period 21,000 years in length and a sexondary period 19,000 years in length
little ice age
an especially cold interval of time during the early 14th century that had major impacts on civilizations in the Northern Hemisphere
annual temperature range
difference between the mean daily temperatures for the warmest and coolest months of the year
daily (diurnal) temperature range
the difference between the highes and lowest temperatures during the day - usually far greater than the annual range
cloud forest
moisture-laden maritime air is lifted up the windward slopes of mountains. an orographic precipitation that may not have rainfall but rather as an almost constant misty fog.
selva
characteristic tropical rainforest comprised of multistoried, broad-leaf evergreen trees with significant development of lianas and relatively little undergrowth
jungle
dense tangle of trees and vines in area where sunlight reaches the ground surface (not a true rainforest)
slash and burn (shifting cultivation)
also called swidden or shiting cultivation; typical subsistence agriculture of primitive societies in the tropical rainforest. Trees are cut, the smaller residue is burned, and crops are planted between the larger trees or stumps before rapid deterioration of the soil forces a move to a new area
tropical monsoon climate
most closely associated with the peninsula lands of Southeast Asia. The alternating circulation of air (from sea to land in summer and from land to sea in winter) is strongly related to the shifting of the ITCZ
tropical savanna climate
much in common with the tropical rainforest and monsoon. located well within the tropics (usually between latitudes 5 and 20 on either side of the equator
desert climate
the amount of precipitation received is less than half the potential ET
steppe climate
the precipitation is more than half but less than the total potential ET.
xerophytic
name for plants that manage to grow in the desert - adapted to extreme drought.
mediterranean climate
is one of the best arguments for organizing a study of the environment or developing an understanding of world regions, based on climte classification
sclerophyllous
natural vegetation that is hard-leafed and drought resistant like xerophytes, but in mediterranean regions
chaparral
plant communities made up of many low, scrubby, bushes that grow together in a thick tangle
humid subtropical climate
located within approximately the same latitudes and in a simalr transitinal positions as the Mediterranean climate but on the eastern instead of the western continental margins
marine west coast climate
proximity to the sea and prevailing onshore winds make it one of the most temperate in the world
humid continental, hot summer climate
unlike the other two microthermal climates, it's relatively limited in its distribution on the Eurasian landmass. It has the by far the greatest agricultural potential
Humid continental, mild summer climate
is a more continental or severe-winter version of its equatorward counterpart
subarctic climate
is the farthest poleward and most extreme of the microthermal climates
permafrost
a permanently frozen layer of subsoil and underlying rock that may extend to a depth of 300 meters or more in the northernmost sections of the climate
patterned ground, or frost polygons
commonly found in regions of subarctic yearly freezing and thawing. Repeated freezing and thawing causes the soil to produce polygonal shapes
Tundra climate
locations in the high latitudes; subsidence and divergence of the polar anticyclone; proximity to coasts
muskeg
the result of drainage blockage by permafrost that produces a cesspool of swarming black flies, mosquitoes, and gnats (in alaska and canada)
ice-sheet climate
the most severe and restrictive climate on earth
exposure
a severe control of highland climates
slope aspect
affects where people live in the mountains and where particular crops will do best
tree line
the line beyond which low winter temperatures and severe wind stress eliminate all forms of vegetation except those that grow low tot he ground.
snow line
the line above which summer melting is insufficient to remove all of the preceding winter's snowfall
abiotic (nonliving)
(the first of four basic components to an ecosystem) the physical environment in which the plants and animals of the system live.
autotrophs (meaning self-nourished)
second component consisting of the basic producers.
heterotrophs (other-nourished)
third component consists of consumers
Herbivores
eat only living plant material
carnivores
eat other animals
omnivores
feed on both plants and animals
decomposers
feed on dead plant and animal material and waste products
trophic structure
the pattern of feeding in an ecosystem is called the trophic structure and the sequence of levels in the feeding pattern is the food chain
trophic level
the number of steps they are removed from the autotrophs or pnats in a food chain
food web
an overlap and interaction between different members of the food chain that results in a feeding mosaic within an ecosystem
biomass
the total amount of living material in an ecosystem.
primary productivity
refers to the formation of new organic matter though photosynthesis by autotrophs
secondary productivity
refers to the rate of formation of new organic material at the heterotroph level
habitat
a specific role in the system and lives in a certain location
ecological niche
the combination of role and habitat for a particular species
generalists
can survive on a wide variety of food. (i.e. bears.)
natural vegetation
the development of plants naturally and without obvious interference from or modification by humans
plant communities
plant associations compatible because each species within the community has different requirements in relation to major environmental factors
succession
natural vegetation of a particular location develops in a sequence of stages involving different plant communities