Yemen, Land and Resources
Yemens, extensive agriculture, intensive cultivation, monsoon winds, wadis
Geologically, much of Yemen constitutes the upturned corner of the rectangular plate that defines the Arabian Peninsula. The edge of this corner takes the form of a steep, jagged mountain range that traces the western and southern limits of a high plateau; the plateau descends gradually north and east from the mountains into the desert interior, on the edge of the vast Rub‘ al Khali (Empty Quarter) of Saudi Arabia. To the west, the mountains drop abruptly to a low, flat coastal desert plain called the Tihamah; averaging about 50 km (about 30 mi) in width, this plain parallels the Red Sea the length of northern Yemen, turns abruptly east near the old border between the two Yemens, and then runs parallel to the Gulf of Aden for part of the length of southern Yemen. Averaging about 1,830 m (about 6,000 ft) and rising at Jabal an Nabi Shu‘ayb to 3,760 m (12,336 ft), the highest peak on the peninsula, the Yemeni highlands have a generally semiarid but otherwise temperate climate, despite their location well south of the tropic of Cancer. By contrast, the coastal desert is hot and humid much of the year, and at times extremely so; summer and winter winds often bring severe sandstorms. Average temperatures for Yemen as a whole vary from about 27°C (80°F) in June to about 14°C (57°F) in January.
Every year during the summer months, monsoon winds blow inland over the water, picking up moisture, and the mountains force the warm air to rise, cool, and condense. The considerable, although erratic, seasonal rainfall allows for intensive cultivation, much of it on stonewalled terraces and in wadis—streambeds that flow with water only during and after the rains. The average rainfall in the highlands varies from 303 to 762 mm (8 to 30 in), whereas on the coast it varies from 76 to 229 mm (3 to 9 in).
The mountains of northern Yemen are cut at right angles in several places by great wadis that feed large aquifers (underground layers of earth or stone that hold water) at their base on the Tihamah. Moreover, since the highlands in the north are loftier and more extensive than in the south, the north has a generally less forbidding climate, greater rainfall, more intensive and extensive agriculture, and a much larger population. The eastern two-thirds of southern Yemen are basically uninhabitable, except for coastal oases, fishing villages, the port of Al Mukalla, and the large, well-populated district of Hadhramaut, which extends from the coast into the country’s interior.
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