Geography of Tajikistan

Coordinates: 39°00′N 71°00′E / 39.000°N 71.000°E / 39.000; 71.000
Source: Wikipedia, the free encyclopedia.
Map of Tajikistan

Panj River) and northern (Fergana Valley) sections of the country.[1] Especially in areas of intensive agricultural and industrial activity, the Soviet Union's natural resource utilization policies left independent Tajikistan with a legacy of environmental problems.[2]

Dimensions and borders

With an area of 142,600 km2 (55,100 sq mi), Tajikistan has a maximum east-to-west extent of 700 km (430 mi), and a maximum north-to-south extent of 350 km (220 mi). The country's highly irregular border is 3,651 km (2,269 mi) long, including 414 km (257 mi) along the Chinese border to the east and 1,206 km (749 mi) along the frontier with Afghanistan to the south. Most of the southern border with Afghanistan is defined by the

Panj River (Darya-ye Panj), which has headwaters in Afghanistan and Tajikistan. The other neighbors are the former Soviet republics of Uzbekistan (to the west and the north) and Kyrgyzstan (to the north).[1]

Topography and drainage

Detailed map of Tajikistan
Topography of Tajikistan

The lower elevations of Tajikistan are divided into northern and southern regions by a complex of three mountain chains that constitute the westernmost extension of the massive

Gissar) mountains. The last of these lies just north of the capital, Dushanbe, which is situated in west-central Tajikistan.[3]

More than half of Tajikistan lies above an elevation of 3,000 metres (9,800 ft). Even the lowlands, which are located in the

Fedchenko Glacier, covers more than 700 square kilometres (270 sq mi) and is the largest glacier in the world outside the polar regions. Because Tajikistan lies in an active seismic belt, severe earthquakes are common.[3]

Fergana Valley

The Fergana Valley, the most densely populated region in Central Asia irrigated by the Syr Darya in its upper course, spreads across the north-eastern arm of Uzbekistan and Northern Tajikistan. This long valley, which lies between two mountain ranges — the Kuramin Range in the north and the Turkestan Range in the south, reaches its lowest elevation of 320 metres (1,050 ft) at Khujand on the Syr Darya. Rivers bring rich soil deposits into the Fergana Valley from the surrounding mountains, creating a series of fertile oases that have long been prized for agriculture.[3]

Drainage

In Tajikistan's dense river network, the largest rivers are the Syr Darya and the

USSR in 1991, this system fell apart and a new resource-sharing plan has yet to be put in place. According to research conducted by the International Crisis Group, this is due to corruption and lack of political will; failure to solve this issue could lead to irreversible regional destabilization.[4]

The two most important rivers in northern Tajikistan are the Syr Darya and the

Sughd Province.[5] The lake is fed by the Syr Darya. Another well-known natural lake of glacial origin is Iskanderkul. It is smaller than the Kayrakum Reservoir and lies in the Fann Mountains
in western Tajikistan.

Climate

Tajikistan map of Köppen climate classification
Karakul is a lake formed inside a meteor crater in Tajikistan.

Tajikistan's climate is continental, subtropical, and semiarid, with some desert areas. The climate changes drastically according to elevation, however. The Fergana Valley and other lowlands are shielded by mountains from Arctic air masses, but temperatures in that region still drop below freezing for more than 100 days a year. In the subtropical southwestern lowlands, which have the highest average temperatures, the climate is arid, although some sections now are irrigated for farming. At Tajikistan's lower elevations, the average temperature range is 23 to 30 °C (73.4 to 86.0 °F) in July and −1 to 3 °C (30.2 to 37.4 °F) in January. In the eastern Pamirs, the average July temperature is 5 to 10 °C (41 to 50 °F), and the average January temperature is −15 to −20 °C (5 to −4 °F).[6]

Tajikistan is the wettest of the Central Asian republics,[7] with the average annual precipitation for the Kafernigan and Vakhsh valleys in the south being around 500 to 600 mm (19.7 to 23.6 in), and up to 1,500 mm (59.1 in) in the mountains[citation needed]. At the Fedchenko Glacier, as much as 223.6 cm (88.0 in) of snow falls each year[citation needed]. Only in the northern Fergana Valley and in the rain shadow areas of the eastern Pamirs is precipitation as low as in other parts of Central Asia: in the eastern Pamirs less than 100 mm (3.94 in) falls per year[citation needed]. Most precipitation occurs in the winter and spring.

Climate data for Dushanbe (1991–2020, extremes 1926–present)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 21.8
(71.2)
27.7
(81.9)
32.2
(90.0)
35.3
(95.5)
38.8
(101.8)
43.0
(109.4)
43.7
(110.7)
45.0
(113.0)
38.9
(102.0)
36.8
(98.2)
31.9
(89.4)
24.3
(75.7)
45.0
(113.0)
Mean daily maximum °C (°F) 9.0
(48.2)
11.0
(51.8)
17.0
(62.6)
22.8
(73.0)
27.9
(82.2)
33.6
(92.5)
36.4
(97.5)
35.5
(95.9)
31.3
(88.3)
24.4
(75.9)
16.7
(62.1)
11.1
(52.0)
23.1
(73.6)
Daily mean °C (°F) 3.1
(37.6)
5.0
(41.0)
10.5
(50.9)
15.8
(60.4)
20.1
(68.2)
25.1
(77.2)
27.4
(81.3)
26.0
(78.8)
21.2
(70.2)
14.7
(58.5)
9.0
(48.2)
4.6
(40.3)
15.2
(59.4)
Mean daily minimum °C (°F) −0.9
(30.4)
0.5
(32.9)
5.5
(41.9)
10.1
(50.2)
13.4
(56.1)
17.2
(63.0)
18.9
(66.0)
17.2
(63.0)
12.7
(54.9)
7.8
(46.0)
3.8
(38.8)
0.4
(32.7)
8.9
(48.0)
Record low °C (°F) −26.6
(−15.9)
−17.6
(0.3)
−12.9
(8.8)
−6.1
(21.0)
1.2
(34.2)
8.4
(47.1)
10.9
(51.6)
8.2
(46.8)
−1.0
(30.2)
−4.4
(24.1)
−13.5
(7.7)
−19.5
(−3.1)
−26.6
(−15.9)
Average precipitation mm (inches) 100
(3.9)
95
(3.7)
102
(4.0)
112
(4.4)
75
(3.0)
17
(0.7)
4
(0.2)
1
(0.0)
4
(0.2)
29
(1.1)
55
(2.2)
60
(2.4)
654
(25.7)
Average precipitation days (≥ 1.0 mm) 8.5 9.1 13.4 9.8 7.8 1.5 0.7 0.1 0.8 3.7 5.3 8.1 68.8
Average
relative humidity
(%)
69 67 65 63 57 42 41 44 44 56 63 69 57
Mean monthly sunshine hours 120 121 156 198 281 337 352 338 289 224 164 119 2,699
Source 1: Pogoda.ru.net[8]
Source 2: Deutscher Wetterdienst (humidity 1951–1993 and precipitation days 1961–1990)[9] NOAA (sun, 1961–1990)[10]
Climate data for Khujand (1961–1990, extremes 1936–present)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 15.7
(60.3)
22.1
(71.8)
28.8
(83.8)
36.5
(97.7)
39.9
(103.8)
43.5
(110.3)
45.9
(114.6)
43.8
(110.8)
38.4
(101.1)
33.8
(92.8)
25.0
(77.0)
21.1
(70.0)
45.9
(114.6)
Mean daily maximum °C (°F) 3.5
(38.3)
6.2
(43.2)
13.8
(56.8)
21.9
(71.4)
28.6
(83.5)
34.2
(93.6)
35.5
(95.9)
32.4
(90.3)
28.8
(83.8)
20.6
(69.1)
12.3
(54.1)
5.6
(42.1)
20.3
(68.5)
Daily mean °C (°F) −0.3
(31.5)
1.7
(35.1)
8.5
(47.3)
16.2
(61.2)
21.8
(71.2)
26.9
(80.4)
28.3
(82.9)
26.1
(79.0)
20.8
(69.4)
13.9
(57.0)
7.3
(45.1)
2.0
(35.6)
14.4
(57.9)
Mean daily minimum °C (°F) −3.4
(25.9)
−1.8
(28.8)
4.2
(39.6)
10.7
(51.3)
15.5
(59.9)
19.6
(67.3)
21.2
(70.2)
18.8
(65.8)
13.6
(56.5)
8.1
(46.6)
3.4
(38.1)
−0.5
(31.1)
9.1
(48.4)
Record low °C (°F) −22.8
(−9.0)
−22.2
(−8.0)
−13.6
(7.5)
−3.9
(25.0)
0.8
(33.4)
8.7
(47.7)
10.5
(50.9)
7.0
(44.6)
1.4
(34.5)
−6.8
(19.8)
−18.8
(−1.8)
−20.0
(−4.0)
−22.8
(−9.0)
Average precipitation mm (inches) 15.7
(0.62)
15.7
(0.62)
26.1
(1.03)
31.4
(1.24)
17.2
(0.68)
4.6
(0.18)
2.3
(0.09)
1.7
(0.07)
2.7
(0.11)
16.9
(0.67)
13.7
(0.54)
16.8
(0.66)
164.8
(6.49)
Average precipitation days 11.4 11.0 12.7 12.6 12.0 6.3 4.1 2.6 3.2 6.8 7.4 10.4 100.5
Average
relative humidity
(%)
77.8 75.4 64.0 56.3 48.7 34.8 33.8 38.4 43.3 55.4 75.2 76.4 56.6
Mean monthly sunshine hours 126 131 168 211 297 358 382 363 300 225 160 106 2,827
Source 1:
NOAA (mean temperatures and sun 1961–1990)[12]
Source 2: climatebase.ru (humidity),[13] Meteo Climat (record highs and lows)[14]

Environmental problems

Most of Tajikistan's environmental problems are associated with the agricultural policies imposed on the country during the Soviet period. By 1991 heavy use of mineral fertilizers and agricultural chemicals was a major cause of pollution in the republic. Among those chemicals were DDT, banned by international convention, and several defoliants and herbicides. In addition to the damage they have done to the air, land, and water, the chemicals have contaminated the cottonseeds whose oil is used widely for cooking. Cotton farmers and their families are at particular risk from the overuse of agricultural chemicals, both from direct physical contact in the field and from the use of the branches of cotton plants at home for fuel. All of these toxic sources are believed to contribute to a high incidence of maternal and child mortality and birth defects. In 1994 the infant mortality rate was 43.2 per 1,000 births, the second highest rate among former Soviet republics. The rate in 1990 had been 40.0 infant deaths per 1,000 births.[2]

Cotton requires particularly intense irrigation. In Tajikistan's cotton-growing regions, farms were established in large, semiarid tracts and in tracts reclaimed from the desert, but cotton's growing season is summer, when the region receives virtually no rainfall. The 50 percent increase in cotton cultivation mandated by Soviet and post-Soviet agricultural planners between 1964 and 1994 consequently overtaxed the regional water supply. Poorly designed irrigation networks led to massive runoff, which increased soil salinity and carried toxic agricultural chemicals downstream to other fields, the Aral Sea, and populated areas of the region.[2]

By the 1980s, nearly 90 percent of water use in Central Asia was for agriculture. Of that quantity, nearly 75 percent came from the Amu Darya and the Syr Darya, the chief tributaries of the Aral Sea on the Kazakhstan-Uzbekistan border to the northwest of Tajikistan. As the desiccation of the Aral Sea came to international attention in the 1980s, water-use policy became a contentious issue between Soviet republics such as Tajikistan, where the main rivers rise, and those farther downstream, including Uzbekistan. By the end of the Soviet era, the central government had relinquished central control of water-use policy for Central Asia, but the republics had not agreed on an allocation policy.[2]

Industry also causes

pollution problems. A major offender is the production of nonferrous metals. One of Tajikistan's leading industrial sites, the aluminum plant at Tursunzoda (formerly known as Regar), west of Dushanbe near the border with Uzbekistan, generates large amounts of toxic waste gases that have been blamed for a sharp increase in the number of birth defects among people who live within range of its emissions.[2]

In 1992 the Supreme Soviet of Tajikistan established a Ministry of Environmental Protection. However, the enforcement activity of the ministry was limited severely by the political upheavals that plagued Tajikistan in its first years of independence. The only registered private environmental group in Tajikistan in the early 1990s was a chapter of the Social-Ecological Alliance, the largest informal environmental association in the former Soviet Union. The Tajik branch's main functions have been to conduct environmental research and to organize protests against the Roghun Hydroelectric Plant project.[2]

Natural hazards: Earthquakes are of varying degrees and are frequent. Flooding and landslides sometimes occur during the annual Spring thaw.[15]

Environment - current issues: inadequate sanitation facilities; increasing levels of soil salinity; industrial pollution; excessive pesticides; part of the basin of the shrinking Aral Sea suffers from severe overutilization of available water for irrigation and associated pollution.

Environment - international agreements:
party to: Biodiversity, Climate Change, Desertification, Environmental Modification, Ozone Layer Protection

Pamir Mountains

Tartu Ülikool 350 is a 6,258-meter peak in Pamir Mountains.

Tajikistan is home to some of the highest mountains in the world, including the

Alay
ranges. 93% of Tajikistan is mountainous with altitudes ranging from 300 m (980 ft) to almost 7,500 m (24,600 ft), and nearly 50% of Tajikistan's territory is above 3,000 m (9,800 ft).

The massive mountain ranges are cut by hundreds of

Fedchenko Glacier
.

The Pamir Mountains in Tajikistan lie in

Mayakovskiy Peak (6,096 m (20,000 ft)), Karl Marx Peak (6,726 m (22,067 ft)), Engels Peak (6,510 m (21,360 ft)), and Concord Peak
(5,469 m (17,943 ft)) stretching west to east along the border to Afghanistan.

Rivers

The principal rivers of Central Asia, the Amu Darya and the Syr Darya, both flow through Tajikistan, fed by melting snow and glaciers from the mountains of Tajikistan and Kyrgyzstan. There are over 900 rivers in Tajikistan longer than 10 kilometres (6.2 mi).

The largest rivers of Tajikistan are:

  • Panj
  • Bartang
  • Gunt
  • Kafirnigan
    )
  • Kyzylsu
  • Muksu
  • Murghab
  • Obihingou
  • Oksu
  • Syr Darya
  • Surkhandarya
  • Surkhob
  • Vanj
  • Yazgulyam
  • Zeravshan

Lakes

About 2% of the country's area is covered by lakes:[15]

Area and boundaries

Area
  • total: 142,600 km2 (55,100 sq mi)
    • country rank in the world: 94th
  • land: 141,510 km2 (54,640 sq mi)
  • water: 2,590 km2 (1,000 sq mi)
Area — comparative
  • slightly smaller than Nepal
  • Australia comparative: slightly more than twice the size of Tasmania
  • Canada comparative: slightly less than twice the size of New Brunswick
  • United Kingdom comparative: slightly larger than England
  • United States comparative: slightly larger than North Carolina
  • EU comparative: slightly larger than Greece
Land boundaries
Coastline
0 km (0 mi) (
landlocked
)
Elevation extremes

Other peaks include:

Peak Korzhenevskaya 7,105 m (23,310 ft); Independence Peak 6,974 m (22,881 ft)[15]

Resources and land use

Natural resources:

Land use (2006 data):[16]
arable land: 6%
permanent crops: 1%
pastures: 21%
non-agricultural land: 72%
including forests and woodland: 3%

Irrigated land:
2006: 7,235 km2 (2,793 sq mi)

Total renewable water resources: 99.7 cu km (1997)

Natural hazards: earthquakes, floods[15]

References

  1. ^ a b "Geography". Library of Congress Country Studies. Archived from the original on 5 March 2016. Retrieved 31 July 2015. Public Domain This article incorporates text from this source, which is in the public domain.
  2. ^ a b c d e f "Environmental problems". Library of Congress Country Studies. Archived from the original on 6 March 2016. Retrieved 31 July 2015. Public Domain This article incorporates text from this source, which is in the public domain. Country Studies. Federal Research Division.
  3. ^ a b c d e "Topography and Drainage". Library of Congress Country Studies. Archived from the original on 4 March 2016. Retrieved 31 July 2015. Public Domain This article incorporates text from this source, which is in the public domain. Country Studies. Federal Research Division.
  4. ^ International Crisis Group. "Water Pressures in Central Asia Archived 2016-05-20 at the Wayback Machine", CrisisGroup.org Archived 2020-06-03 at the Wayback Machine. 11 September 2014. Retrieved 7 October 2014.
  5. ^ "Kayrakum Reservoir". Archived from the original on 2008-08-28. Retrieved 2008-08-14.
  6. ^ "Climate". Library of Congress Country Studies. Archived from the original on 9 April 2016. Retrieved 31 July 2015. Public Domain This article incorporates text from this source, which is in the public domain. Country Studies. Federal Research Division.
  7. ^ "Water in Tajikistan, abundant yet challenging". ACTED. 5 December 2017. Archived from the original on 18 May 2022. Retrieved 25 June 2022.
  8. ^ "Weather and Climate-The Climate of Dushanbe" (in Russian). Weather and Climate. Archived from the original on 29 October 2021. Retrieved 28 October 2021.
  9. ^ "Klimatafel von Duschanbe / Tadschikistan" (PDF). Baseline climate means (1961–1990) from stations all over the world (in German). Deutscher Wetterdienst. Archived (PDF) from the original on 13 November 2021. Retrieved 18 February 2016.
  10. ^ "Dushanbe Climate Normals 1961–1990". National Oceanic and Atmospheric Administration. Archived from the original on 29 October 2021. Retrieved 18 February 2016.
  11. ^ "World Weather Information Service – Khujand". World Meteorological Organization. Archived from the original on 20 January 2022. Retrieved 18 December 2019.
  12. ^ "Leninbad (Khujand) Climate Normals 1961–1990". National Oceanic and Atmospheric Administration. Archived from the original on 25 January 2023. Retrieved 18 December 2019.
  13. ^ "Leninabad, Tajikistan". Climatebase.ru. Archived from the original on 14 October 2017. Retrieved 30 January 2013.
  14. ^ "Station Khudjand" (in French). Meteo Climat. Archived from the original on 20 January 2022. Retrieved 18 December 2019.
  15. ^
    CIA
    .
  16. ^ Agriculture in Tajikistan, statistical yearbook, State Statistical Committee, Dushanbe, 2007, in Russian

External links

39°00′N 71°00′E / 39.000°N 71.000°E / 39.000; 71.000