GEOG Exam #2 - Climate Classification

temperature; precipitation

___ and ___ patterns provide key to climate classification

classification

process of ordering or grouping data or phenomena into related classes

genetic classification

a climate classification based on causative factors - for example, the interaction of air masses

empirical classification

a climate classification based on statistics or other data determined by measurement of observed effects - for example, climate classification based on temperature and precipitation

tropical, mesothermal, microthermal, polar, highland, dry

six basic climate catergories

rain forest, monsoon, savanna

tropical climate (tropical latitudes)

humid subtropical, marine west coast, mediterranean

mesothermal climate (midlatitude, mild winters)

humid continental, subarctic

microthermal (mid and high latitudes, cold winters)

tundra, ice caps, ice sheets, polar marine

polar (high latitude and polar regions)

highland

high elevations at all latitudes

arid desert, semiarid steppe

dry (permanent moisture deficit)

climograph

a graphical representation of the climate of a region

tropical rain forest

constantly moist and warm

tropical monsoon

feature a dry season that last 1 or more months (occurs when the convergence zone is not overhead); rainfall is 6 to 12 months

tropical savanna

exist poleward of the tropical rain forest climates; rainfall for about 6 months or less

humid subtropical hot summer

either are moist all year or have a pronounce winter-dry period, as occurs in eastern and southern Asia

humid subtropical winter dry

related to the winter-dry, seasonal pulse of the monsoons; extend poleward from tropical savanna climates and have summer month that receive 10 times more precipitation than their driest winter month

marine west coast

features mild winters and cool summer, dominate middle to high latitude west coasts; dominated by maritime polar (mP) air masses

Mediterranean dry summer

at least 70% of annual precipitation occurs during the winter months; brings summer water-balance deficits

humid continental hot summer

differentiated by their annual precipitation distribution

humid continental mild summer

soils are thinner and less fertile in the cooler microthermal climates, yet agricultural activity is important and includes dairy, poultry, flax, sunflower, sugar beet, wheat, and potato production

subarctic cold summer

average monthly temperatures below freezing around 7 months of the year, during which time light snow cover and frozen ground persist; high pressure dominates during its cold winter - this is the source region for the continental polar air mass

extreme subarctic cold winter

occur only in Russia; difficult to comprehend; has had probably to world's greatest annual temperature range from winter to summer (63 C�)

tundra

land is under continuous snow cover for 8-10 months, with the warmest month above 0 C�, yet never warming above 10 C�

ice sheet

cover the Antarctic continent and most of the island of Greenland, as does North Pole, with all months averaging below freezing

ice caps

smaller in extent than ice sheets, yet they completely bury the landscape like an ice sheet

polar marine

more moderate than other polar climates in winter, with no month below -7�C, yet they are not as warm as tundra climates; annual temperature ranges are low

dry

permanent moisture deficits; Subtropical high-pressure cell predominate, with subsiding, stable air and low relative humidity;Subdivided into deserts and steppes

steppe

regional term referring to the vast semiarid grassland biome of Eastern Europe and Asia; Too dry to support forest, but too moist to be a desert

Tropical (subtropical; low latitude) hot desert

Earth's true tropical(subtropical) deserts and feature annual average temperatures above 18�C; Some regions can get no rainfall and some can get up to 35 cm

Midlatitude cold desert

cover only a small area; Rainfall must be low because of lower temperatures and lower moisture-demand values

Tropical, (subtropical; low latitude) hot steppe

generally exist around the periphery of hot deserts, where shifting subtropical high-pressure cells create a distinct summer-dry and winter-wet pattern; Average annual precipitation is usually below 60 cm

Midlatitude cold steppe

occurs poleward of about 30� latitude and the midlatitude cold desert climates; Not generally found in the Southern hemisphere; rainfall is widely variable (20-40 cm)