Surface water resources in North Afghanistan

This is one of the most intricate and principal issues in further water use in the entire Aral Sea basin. As regards this, there are many papers and publications that unfortunately sometimes make a mess of the real situation with the role of Afghanistan in the feed of the Amudarya river basin.

In 1992 “Soyuzgiprovodkhoz” (nowadays “Intervod”) made a publication titled “Possible principles and options of water distribution in the Aral Sea basin”, authors A.A. Bostanzhoglo, O.A. Leontyev, G.Kh. Ismayilov, in which the volume of flow forming in the Amudarya river in North Afghanistan amounts to 19.6 km³. A.A. Pyatigorskiy (TsBNITI Ministry of Water Resources of the USSR, 1969, page 11) estimates this figure including Harirut 10-11 km³ and so on, V.I. Antonov (Vodproyekt) determines the volume of Pyanj water resources forming within Afghanistan 16 km³ (1994).

In his works, Prof. V.L. Shults (SARNIGMI, 1968) gave two values of the same resources: 370 m³/sec or 11544 million m³ on page 28 and 290 m³/sec or 9.048 million m³ on page 30. “Giprovodkhoz”, A. Kiyatkin (1984) gives overall water formation in North Afghanistan as 18.07 km³.

In the mentioned estimations, three independent groups of catchment areas within North Afghanistan should be kept in mind:

The catchment area of the Murghab and Harirut rivers (Tedzhen) on the territory of Afghanistan amounts to 117500 km², including 46880 km² of Murghab and 70620 km² of Harirut.

The catchment area of the Amudarya system rivers within Afghanistan amounts to 84000 km² and covers the whole area of North Afghanistan, from the Iranian-Afghan border in the west to high-mountain Vakhan in the east. This space of foothills, slopping hilly plains and deserts from the south to the north is cut through by rivers originating in mountains Hindu Kush and Tirbandi-Turkestan.

The Amudarya river is permanently fed by eastern rivers in the basin only, namely the Kunduz river with a catchment area of 31300 km², or 37300 km² according to other data, Kokca river - 21100 (or 21900) km² respectively, and rivers in mountainous Badashkhan – 30800 km².

The pre-Amudarya system includes Khulm, Balkh, Sary-Kul and Shirintagao rivers, with a total catchment area of 49400 km² (47700 km²). These four rivers are local rivers in North Afghanistan, which don’t carry their water to the Amudarya river. They are fully diverted for irrigation and lost in sands. The discharge of these rivers from irrigation systems into separate closed depressions, located at the periphery of irrigated lands, only takes place in flood period in high-water years. And only in years with especially high floods, river discharges (mainly Balkh) in depressions fall into the channel of the so-called Kelif Uzboy, over which, as supposed, the river formerly flowed towards the Caspian Sea, and which has now been used on the territory of Turkmenistan for constructing Karakum canal.

Between these rivers and the Amudarya river, there is a zone with an area of 72500 km² that almost does not have runoff (Pyatigorskiy, 1969). Below a brief description of all rivers in North Afghanistan is given.

Amudarya river

The length of the river is 2540 km, at that within Afghanistan its length amounts to 1250 km. The Amudarya river originates at a height of 4900 m and from a glacier with the same name around Vakhan. After the confluence with the Pamir river flowing out from Lake Zor-Kul, the river is known as Pyanj, and only after mountain gorges and the confluence with the Vakhsh river (right tributary) it is called Amudarya; and turning to north-west, passing through border settlement Khamkab (on the Afghan territory), it goes into the CIS (the former Soviet Union).

Kokca river

It is formed of the confluence of three small rivers Jirm, Varduj and Zardiv at Zhempuly bridge (above Fayzaabad town). The Jirm river originates at Zharun pass (height 4760 m). At the left, Jirm receives a big tributary, Anjuman, flowing from an area of Munjan pass (height 4362 m). The Varduj river at Zeybak settlement is formed of three small rivers Varduj, Zebak and Sanglich Doran). The Zardiv river in turn is formed of small rivers Sergalyan and Shishe. From Shash-Puli bridge to Fayzaabad town (center of Badashkhan province), the Kokca river flows through narrow gorge. Behind Fayzaabad town, Deraim, Toshkan and Kishm tributaries flow into Kokca at the left. The Kokca river flows into Amudarya at Afghan village Kala-iy-Zanum. The length of the river from Parui pass is 320 km. The width in the midstream is no more than 10-12 m, depth 1-2 m.

Kunduz river

The Kunduz river (Surkhab in the midstream) originates at Shibar pass. The river receives two tributaries at the left: Seygan and Kamerd. At the right the following tributaries flow into Surkhab:

Local rivers in North Afghanistan

The Hulm river originates near Kara-Kotal pass (height 3600 m). The highway from Mazari-Sharif to Kabul city passes through the valley of this river. In mountainous part, the river flows across small valleys, narrow gorges, and, finally, cutting through the mountain range at Tashkurgan town, flows into a vast valley. The river is about 230 km long, 40-50 m wide at Tashkurgan town and 1-1.5 m deep. The catchment area of the river is 8400 km².

The Balkh or Bandi-Amir (Dara-Gez) river in the midstream is called Vadkhab. Following the effusion of groundwater rich in lime in the upstream of this river, natural ponds and five lakes appeared. Two of them have been lost, and three ones fed by ground and surface water exist. From the right, the river receives Dara-iy-Suf tributary. The length of the river is about 400 km, the width in the midstream is 20-40 m, at a depth of 2-3 m. The catchment area is 18700 km².

The Sary-Pul (or Safed) river is formed of a lot of small mountain rivers, which flow from the northern Kohi-Bab mountain range. At Sari-Pul town, these small rivers unite into one river. The width of the river in the midstream is 15-20 m, at a depth of up to 20 m. The catchment area of the river is 9400 km², the length is 215 km (7800 km² according to some data).

The Shirintagao river originates in the northern Tirbandi-Turkestan mountain range, at Gurzimen. From the left, the river receives Maymene tributary, and this last tributary receives the Abi-Kaysar river, in which there is water only a few months a year. A small river, Almar, flows into Abi-Kaysar from the right. The catchment area of the river is 13600 km².

Transboundary rivers between Afghanistan and Turkmenistan (partly Iran)

Murghab river

Murghab originates on a high plateau located between Safedkokh (Paropamiz) and Bandi-Turkestan mountain ranges. From its sources to Mukhamedkhan village (length 300 km), apart from upper reaches, the Murghab valley is narrow, with a width of 200-1000 m, bounded by high and steep slopes. In some places, the valley passes to narrow gorges. At the end of location, between Darbandi-Kilrekht village and Mukhammedkhan, the river cuts through the western Bandi-Turkestan mountain ridge and flows in a deep canyon. Here, there are two narrow passages: at Darbandi-Kilrekht village and at Mukhammedkhan village (the latter is called Jaokar gorge). Below Mukhammedkhan, the Murghab valley gradually gets wider from 0.5-1 km to 1-2 km on the territory of Turkmenistan. Before Balamurghab village, the valley has high (70-100 m) and steep slopes, then their height reduces, and they become less steep, but greatly dissected by ravines and valleys of small tributaries. Below Mukhamedkhan, water resources of Murghab are partly taken for irrigation. However, owing to the narrowness of the valley and stony soils, here only 10000 ha of lands are irrigated, and available free irrigable funds, according to some data, amount to no more than 5000 ha. After the confluence of Murghab and Kaysar tributary at the right and before Khan-Tepe border mound, there is a line of Turkmen-Afghan frontier along Murghab. Above Takhta-Bazar town (on the territory of Turkmenistan), Kashan flows into Murghab at the left, and after 25 km downstream Kushka flows into the river.

Harirut river

The river called Sari-Jangal in the upstream is formed of the confluence of a few small mountain rivers at Shakhin village. From is source to Badghah (27 km west from Daulatyar town) Harirut flows through a vast valley, the bottom of which is partly allotted under crops and covered by pastures. Farther, the valley gets narrow, passing to gorges in some laces. From Kushnami village to Oba town, the river flows into a narrow valley, which is characterized by periodical narrowing and small expansions. Here, the river is a rapid mountain stream; in gorges it is mostly impetuous, in some places it rushes down as cascades and forms small waterfalls. Below Oba town, the Harirut valley become wider. The mountains get smooth and leveled shapes and form a vast valley with a plain bottom, moving aside. There Herat oasis (with a length of 150 km and maximum width of 30 km) with an extensive network of irrigation canals is located. The irrigated area of Herat oasis, including Oba, Gurian towns and Kozsan village, amounts to about 70000 ha.

From its source to Pule Khatum bridge, Harirut receives many tributaries. Among them, the Tagaoishlan (Kaugan), flowing into Harirut at the left below Oba town, and the Jam and Keshefrud rivers (left), especially the latter, are distinguished with their length and drainage area. Jam and Keshefrud flow through Iran. It is necessary to note that in summer many tributaries of Harirut located below Oba town do not reach it, since their water resources are used for irrigation.