U469 Mongolia: Theocracy, Communism, Democracy
(formerly Mongols of the 20th Century)
Week 1: Thursday
Mongolian Climate, Geography and nomadic pastoralism
Mongolian climate: very distinctive
Sunny
av. 2,900 hours of sun/year (200-500 more than elsewhere)
Windy
Winds steady, not too strong, from west and north
Over dry areas, picks up dust, deposits it in N. China (loess)
Dry
35-15 centimeters per year (30 cm necessary to farm)
Continental (very cold winters, warm summers)
January average 5 F to -31 F
July average 60 F to 77 F
Ranges of 80 to 100 degrees not uncommon
Frost-free season: May/June to August/Sept.
Problems for agriculture
Precipitation low, sunniness means air very dry > evaporation
Very short growing season
Catch 22: where it’s warm it’s dry, where it’s wet it’s cold
Seasonal distribution all wrong
Winter and spring: winds from high pressure center in Uws
Winds very dry, little snow, on plains 2-5 cm build up at most
Little snow > soil cold (snow insulates), no spring runoff
In summer Siberian/Uws high weakens, some southern winds
65-78% of precipitaion in three summer months
Rain falls AFTER the sowing, not before
Even wettest areas have ground humidity 60-70% of optimal
Other ground water resources
Small glaciers in Altai
Permafrost: 10% of Mongolia, mountains and north
Rivers and lakes: fed by spring mountain runoff, and summer rains
Kh
ö
wsg
ö
l-Selenge-Baikal system: drains into Arctic
Baikal and Kh
ö
wsg
ö
l: largest fresh lakes (by volume) on earth
Selenge, Orkhon, Tuul largest rivers in Mongolia
Onon-Kherlen-Khalkha system: drains to Amur into Pacific
Smaller rivers, also Kh
ö
l
ö
n (or Dalai) and Buir lakes
Central Asian landlocked basin: 2/3 of Mongolia
Many salt lakes, used commercially for salt, soda, etc.
Regions of Mongolia
Fundamental division: Gobi and Khangai
Khangai is wet, cold, wooded mountain: north
Gobi is dry, hot, desert plain: south
Major topographic features
Altai Mountains: highest, snow-covered, glaciers
Great Lakes basin: between Altai and Khangai mts. >> dry, salt lakes
Khangai: high mountains (peaks snow-covered), wooded slopes, valleys
Khentii: low mountain (no permanent snow), khangai terrain
Gobi: desert to semi-desert flat plain
Steppe: between khangai and gobi, and in eastern plain: rolling, fine grass
Selenge valley: best watered place in Mongolia, center of agriculture
Pastoral nomadism
The animals: Five snouts of animals (
tawan khoshuu mal
)
Horse: riding (war and peace), milk, mane & tail for religious use
In epics, horse is always hero’s best councilor
Horned cattle: milk, some meat, draws carts
In Khangai and Altai, yaks with fine hair
Camels: milk, hair, best pack animal
Sheep: vital for meat, wool ( >> felt), rarely milked
Goats: leads sheep herds, fine hair (cashmere)
Animal dung vital for fuel: esp. cattle dung, sheep for tinder
The yurt (
ger
)
Made of willow-wood framework, covered by felt
Can be assembled and disassembled in an hour
Structured space: right-male, left-female, back-high status, door-low
Up to 1945, usually open fires, yurt very smoky, now closed stoves
The annual cycle
Migration depends on water supply, grass, snow cover, topography
Also depends on population density--high density > short movements
Seasonal issues
Late spring, good water supply, needs to milk young
Summer, good grass, water, needs to put on fat for the winter
Autumn: like summer
Winter: use best fodder areas (water not vital)
early, mid-spring: animals weakest, danger of
zud
Improving productivity: key is improving water supply, spring grass supply
Obvious answer is cutting fodder and storing it >> irrigation (?)
Improved breeds also need more water >> wells >> less mobility