Lably
Skip to content

Sawad

  • 35 min read
  • 8 chapters

Related on Lably

Through Iraq, Mesopotamia and Umayyad Caliphate

As a generic term in Arabic, sawād (سواد) was used to denote the irrigated and cultivated areas in any district. Unmodified, it always referred to southern Iraq, the sawād of Baghdad. It replaced the earlier and more narrow term Rādhān.

The term sawad eventually came to refer to the rural district around a particular city; thus, contemporary geographers made references to the Sawad of Baghdad, of Basra, of Kufa, of Wasit, of Samarra, or of Anbar. This usage was exclusive to Iraq.

Geography

The enormous economic potential of the Sawad is reflected in early Abbasid revenue lists: the Sawad produced four times as much tax revenue as the second-highest-producing province, Egypt, and five times as much as Syria and Palestine combined.

During the medieval period, the lower Tigris followed a different course than it does today. It had shifted further west due to the floods of the early 7th century (before this, its course was the same as it is today). It passed the city of Wasit and entered the Batihah at the town of Qatr. According to Donald Hill, after about 1200, the Tigris and Euphrates started to gradually shift toward their present courses, which they finally reached during the 1500s. On the other hand, Stephen Hemsley Longrigg described the shift as taking place in the period between 1500 and 1650.

In Sasanian times, the Euphrates likely entered the swamps close to the site of the modern town of Shinafiya.

The Batihah (plural: Bata'ih) or great swamp was the medieval name for the vast marshlands of southern Iraq, along the lower courses of the Tigris and Euphrates. In the northwest, it stretched almost up to Kufa and Nippur, while in the northeast it began at al-Qatr, downstream from Wasit on the Tigris. Suhrab lists four great lagoons (Ḥawr) in the Batihah: Bahassa, Bakhmasa, Basriyatha, and finally al-Muhammadiyah, which was the largest. Below the Hawr al-Muhammadiyah, the channel called the Nahr Abi'l-As'ad finally carried the waters of the Batihah to the head of the Dijlah al-`Awra', or "one-eyed Tigris". The hydrography of the Bata'ih was not static.

Ibn Rustah described the Bata'ih as covered by reed beds crossed by water channels, where enormous amounts of fish where caught, then salted and exported to neighboring provinces. The water level was too shallow for most river boats to pass through, and only special pole-propelled vessels called mashhuf could be used for transport. Most of the marshes were covered by water, but there were some areas with good soil, where people formed settlements, grew crops, and dug canals for irrigation.

Climate

In Iraq, there are two very distinct seasons: summer and winter. Spring and autumn are very short. Summer, which lasts from May through October, is intensely hot and dry, with the sky mostly cloudless and rain extremely rare. The prevailing northwest wind (the Shamal) is a hot wind and is strong during the day but dissipates at night. Winter lasts from November until April, and the northwest winds are weaker and often interrupted by depressions coming from the Mediterranean. The southeast winds (called Sharqi) are accompanied by cold temperatures, cloudy skies, and rain. Average winter rainfall is about 5 inches. Frost may occur anywhere in Iraq during the winter, except for the southernmost parts, and they come in the wake of the depressions, after the rain. Snow sometimes lays on the ground for several days.

According to Husam Qawam El-Samarraie, the climate of Iraq during the Abbasid era was probably similar to today, although the greater abundance of date palm orchards then "may have mitigated the violence of the winter winds and prevented the occurrence of the sandstorms that now sweep all over the country."

Challenges to agriculture

The main crop-growing season in this region comes during the winter, and irrigation is needed at least monthly. However, neither the Tigris nor the Euphrates reaches its high water mark during the winter when farmers need water the most: the Tigris is fed by several tributaries in the Zagros mountains, and melting snows in the mountains lead to high water in April. The Euphrates, on the other hand, mostly consists of water from the Anatolian highlands, and melting snow reaches lower Mesopotamia later, in early May. This is too late to help with growing crops for the May and June harvest season.

The timing of the flooding in the Euphrates was less helpful than the Tigris. The Tigris, however, is prone to flooding, since winter and spring storms in the Zagros mountains lead to highly destructive floods. The most destructive flood on the Tigris in modern times was in 1954, when there was a flow of 16,000 cumecs, whereas the worst flood on the Euphrates was in 1929 with only 5,200 cumecs. The Euphrates was therefore more manageable, while settlements along the Tigris had to be built away from the river to avoid being destroyed by flooding. Additionally, the Tigris's banks were so deep that canals had to be extended far down the backslope of the protective levees built along the river in order to keep a high enough water level. Yet these labor-intensive canal offtakes were directly exposed to the floods and could be suddenly buried under a deep layer of silt.

Later on, however, a vast canal system came to use the flow of the Tigris to supplement the Euphrates: during the winter growing season, when the Tigris was less prone to intense flooding, Tigris water was brought in, and then its headworks closed off and protected as much as possible, while now the greatly enlarged Euphrates was used to support irrigation efforts. This massive reshaping of the natural relationship between these rivers, which reached its peak during the Sasanian period, led to a mushrooming population and the rise of many new cities.

Sign in to keep reading

7 more chapters are free with a Lably account.

More in Geography