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Grasslands of the World.pdf - Disasters and Conflicts - UNEP

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308<br />

Plate 8.3<br />

Harvested wheat in <strong>the</strong> Yarlung Tsangpo river valley.<br />

<strong>Grassl<strong>and</strong>s</strong> <strong>of</strong> <strong>the</strong> world<br />

includes all grassl<strong>and</strong> in <strong>the</strong> Tibet Autonomous Region <strong>and</strong> Qinghai Province<br />

(118.4 million hectares), on <strong>the</strong> nor<strong>the</strong>rn flanks <strong>of</strong> <strong>the</strong> Kunlun Mountains in<br />

sou<strong>the</strong>rn Xinjiang (15 million hectares) <strong>and</strong> in western Sichuan (14 million<br />

hectares), northwestern Yunnan (5 million hectares) <strong>and</strong> western Gansu<br />

(12 million hectares). Less than one percent <strong>of</strong> <strong>the</strong> steppe is cultivated, although<br />

crops have exp<strong>and</strong>ed in recent decades, especially in <strong>the</strong> Qaidam Basin. In <strong>the</strong><br />

east <strong>of</strong> <strong>the</strong> plateau, crop l<strong>and</strong> is in <strong>the</strong> lower valleys; in western Tibet, along <strong>the</strong><br />

valley <strong>and</strong> tributaries <strong>of</strong> <strong>the</strong> Yarlung Tsangpo (Brahmaputra River). The upper<br />

limit <strong>of</strong> cultivation , which is as low as 3 300 m in some eastern parts, can reach<br />

4 400 m in <strong>the</strong> west. The major crops are barley, wheat (Plate 8.3), peas, rape<br />

<strong>and</strong> potatoes.<br />

The Tibetan Steppe has several distinct topographic regions determined<br />

by drainage <strong>and</strong> <strong>the</strong> parallel mountain ranges that divide it (Schaller, 1998).<br />

Only <strong>the</strong> east <strong>and</strong> south have outlets to <strong>the</strong> ocean; rivers originating in <strong>the</strong><br />

Kunlun Mountains flow north to <strong>the</strong> Taklimakan <strong>and</strong> Qaidam Deserts. Much<br />

<strong>of</strong> <strong>the</strong> Steppe consists <strong>of</strong> large lake basins with no outlets, ringed by mountains.<br />

Forests are limited to <strong>the</strong> eastern edge in western Sichuan, northwestern<br />

Yunnan, sou<strong>the</strong>astern Qinghai <strong>and</strong> eastern Tibet , <strong>and</strong> in some valleys on <strong>the</strong><br />

nor<strong>the</strong>rn slopes <strong>of</strong> <strong>the</strong> Himalaya .<br />

CLIMATE<br />

The Tibetan Steppe has a severe continental climate <strong>and</strong> is affected by <strong>the</strong><br />

sou<strong>the</strong>astern monsoon in summer <strong>and</strong> western air circulation patterns <strong>and</strong> high<br />

Mongol-Siberian air pressures in winter (Huang, 1987). The Steppe slopes to<br />

<strong>the</strong> sou<strong>the</strong>ast, so moisture from <strong>the</strong> southwest monsoon comes up gorges from<br />

S.G. REYNOLDS

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