Districts under Central Government Jurisdiction

Districts under Central Government Jurisdiction Tajik: Ноҳияҳои тобеи ҷумҳурӣ
Region
From top: Vahdat, Varzob ravine, Sangvor, Hisor fortress, and Lakhsh
Location of the Districts under Central Government Jurisdiction in Tajikistan
Coordinates: 39°0′N 70°0′E
Country	Tajikistan
Administrative centre	Dushanbe
Area
• Total	28,500 km2 (11,000 sq mi)
Population  (2024)
• Total	2,197,000
• Density	77.1/km2 (200/sq mi)
ISO 3166 code	TJ-RA
HDI (2023)	0.684 medium
Official languages	Tajik Russian

The Districts under Central Government Jurisdiction or Districts of Republican Subordination; Tajik: Ноҳияҳои тобеи ҷумҳурӣ, romanized: Nohiyahoyi tobe’i jumhuriy) is a region in Tajikistan, consisting of nine districts and four district-level cities that are directly administered by the central government. The national capital, Dushanbe, is geographically surrounded by the region but is administratively separate from it.

The region covers an area of 28,500 square kilometres (11,000 sq mi) and borders Dushanbe, Sughd, Kuhistoni Badakhshon, Khatlon, Kyrgyzstan (Batken and Osh regions), and Uzbekistan (Surxondaryo). Its estimated population in 2024 is 2,197,000.

Economy

As of 2019, the region had a population of approximately 2.12 million and a population density of 74 persons per km². Its economy benefits from the country's strong macroeconomic growth, Tajikistan's GDP grew by 8.4% in 2024, with services and industry driving the expansion. Growth continued at 8.1% in the first half of 2025, with projections moderating to 7.0% in 2025 and 4.5–5.0% in 2026–27.

The World Bank has provided significant financial support to the region. In June 2025, an additional $25 million grant was approved to extend the Socio-Economic Resilience Strengthening Project (SERSP) to districts within the region, including Faizobod, Nurobod, Roghun, and Tursunzoda. The project aims to improve infrastructure, support entrepreneurship, and build climate resilience.

Agriculture

The region's fertile valleys, particularly the Hisor Valley, are among Tajikistan's most important agricultural areas. The economy of many districts, such as Vahdat, relies heavily on agriculture. Cotton cultivation is a major activity, especially in districts like Tursunzoda and within the Hisor Valley. The district of Tursunzoda is a significant producer of rice and cotton. The region is a major producer of fruits and vegetables, including apples, pears, peaches, cherries, mulberries, apricots, pomegranates, and nuts. The production of construction materials and agricultural products, mainly vegetables and fruits, is a key economic activity. Both cattle and horses are raised, with breeds adapted to the mountainous terrain.

Industry and Mining

The region is a key industrial hub, hosting 703 industrial enterprises (17.9% of the national total) as of 2025. Industrial production in the districts under republican subordination grew by 111.8% in 2025. The region is rich in mineral deposits, including gold, silver, antimony, mercury, coal, and various construction materials. In 2025, Tajikistan's mining industry produced over 20 billion somoni worth of products, with production volume increasing by 36.2% compared to 2024. Growth in the mining sector was driven by metallic ores (up 36%), coal (up 10.6%), and other minerals (up 30.3%). The Tursunzoda and Rudaki districts are the main industrial output producers within the region. Tursunzoda is home to the country's largest aluminum smelter, TadAZ (now TALCO), which is a significant economic driver for the district. The region possesses substantial raw material deposits for cement production, supporting a growing cement industry. Industrial production is concentrated in the western part of the region, particularly in the Tursunzoda, Shahrinav, Hisor, and Rudaki districts.

Energy

The region plays a central role in Tajikistan's energy sector. The Roghun Hydropower Plant (HPP), located in Roghun District, is one of the largest infrastructure projects in Central Asia. Once complete, it is expected to Generate 14,400 GWh of renewable electricity annually, roughly 60% of Tajikistan's current electricity generation. Provide electricity to 10 million people in Tajikistan. Enable electricity exports to Kazakhstan and Uzbekistan, strengthening regional energy markets. Create more than 30,000 direct and indirect jobs during and after construction. The World Bank has approved multiple phases of grant financing for the Rogun HPP. In June 2026, a second-phase grant of $300 million was approved, bringing the World Bank's total financing for the project to $650 million. Investment is seen as a key driver of economic growth in the region. The Tajik government has prioritized private investment, offering over 240 incentives and 110 customs exemptions for foreign investors. Investment growth in the regions of republican subordination reached 18.8% in 2024. The development of the Rogun HPP is also expected to drive significant investment and economic activity.

Geography

The Districts under Central Government Jurisdiction cover a total area of approximately 28,500 square kilometres (11,000 sq mi), stretching horizontally across the middle of Tajikistan from the Hisor valley near the Uzbekistan border to the eastern mountain ranges. The region is predominantly mountainous and is characterised by significant variations in altitude, climate, and landscape.

Topography and mountain ranges

The region is defined by several major mountain ranges that form its natural borders. On the northern border run the Hisor and Zarafshan mountains, while the southern border is marked by the Darvoz range, which reaches heights of up to 7,600 metres (24,900 ft). The Hisor Range runs along the northern edge of districts such as Varzob and Vahdat, with the Kondara Gorge cutting through its southern spurs north of Dushanbe. The Zarafshan mountains form the border between Sughd Region to the north and the Districts of Republican Subordination to the south. In the eastern part of the region, the Sangvor District extends north of the Darvoz range, which forms the boundary with the Kuhistoni Badakhshon.

The terrain is extremely mountainous. The eastern districts, such as Rasht, are particularly rugged, with average elevations around 1,461–1,671 metres. The Pamir Mountains, home to some of the highest peaks in Central Asia including Ismoil Somoni Peak (7,495 m) and Ibn Sina Peak lie along the region's eastern periphery.

Hydrography

The region's river systems are part of the greater Amu Darya basin. The principal river traversing the region is the Vakhsh, a right-hand tributary of the Amu Darya. The Vakhsh River is 524 km long with a catchment area of 31,200 km² and an average annual flow of 19.6 billion m³, with peak flows occurring in July–August.

Other major rivers include:

• Kofarnihon (387 km, catchment 11,600 km², peak flow April–May)
• Zarafshon (310 km, catchment 14,300 km², peak flow July–August)
• Karatag (112 km, catchment 13,500 km², peak flow June–August)

The Kofarnihon river system includes tributaries such as the Elok, Sorvo, and Varzob, with the Karatag as a sub-basin. Numerous smaller rivers and streams drain the mountain valleys, many of which are fed by glacial meltwater.

Soils

The soil cover of this reigon is characterized by remarkable diversity, a direct consequence of the region's complex topography. The dominant soil-forming processes are strongly influenced by vertical zonality, with distinct soil belts occurring at different altitudes. Loess deposits serve as the major parent material for many of the region's soils. This vertical zonation creates a dynamic mosaic of soil types, each adapted to specific climatic and ecological conditions.

Soil Types and Vertical Zonation

Based on the World Reference Base for Soil Resources (WRB) and local classification systems, the following major soil types and their respective altitude ranges have been identified:

Soil Types and Altitudinal Distribution

Soil Type (Local Classification)	WRB Equivalent	Altitude Range	Key Characteristics
Light serozems (light gray soils)	Calcisols / Solonchaks	300–600 m	Low humus content (1–1.5%), used for cotton cultivation.
Typical serozems (gray soils)	Calcisols	600–900 m	Humus content 1.5–2%, common in foothill and sloping areas.
Dark serozems	Calcic Xerosols / Calcisols	900–1,600 m	Humus content 2.5–4%, found in the Hisor Valley, high fertility.
Mountain brown carbonate soils	Calcaric Cambisols / Calcisols	800–2,000 m	Rich in calcium carbonate, humus content 0.5–6.4%, relatively high humus portions in upper layers (2.70–3.18%).
Mountain brown typical soils	Cambisols / Kastanozems	900–2,800 m	Found in mid-altitudes, well-developed profiles, high humus content (5–8%).
High-mountain meadow-steppe and desert soils	Leptosols / Regosols	Above 2,800 m	Thin, underdeveloped soils, often stony, with low organic matter (0.5–1%).
Alluvial soils	Fluvisols	Valley bottoms	Recent river deposits, layered sandy loam, loam, and gravel; high initial fertility.

Lowland Valleys

In the lower elevations of the Hisor Valley, grey-brown serozems (gray soils), brown-carbonate soils, and mountain steppe soils are prevalent. These soils, often derived from loess, have low to moderate organic matter content. The dark serozems in this zone are particularly valued for agriculture, especially for early potato cultivation. Along river valleys (e.g., Vakhsh and Kofarnihon), alluvial soils are widespread—fertile, layered deposits of sandy loam, loam, and gravel.

Mid-Altitude Woodlands and Shrublands

Between approximately 800 and 2,000 meters, mountain brown carbonate soils dominate. These well-drained, carbonate-rich soils have higher humus content than lowland serozems and support the region's characteristic "shiblyak" vegetation (wild apple, hawthorn, and pistachio). Mountain brown typical soils also occur at higher elevations within this belt.

High-Altitude Zones

Above the treeline, soils transition to high-mountain meadow-steppe soils, high-mountain steppe soils, and high-mountain desert soils. These thin, underdeveloped, stony soils are classified as Leptosols or Regosols in the WRB system. Soil formation is slow under harsh climatic conditions, resulting in low organic matter content.

Soil Degradation and Conservation

Soil degradation poses a significant challenge in the region. According to the UN Food and Agriculture Organization (FAO), nearly 70% of the country's arable land shows signs of degradation, with roughly 10% of the population living on degraded territory. Intensive agricultural activities on mountain slopes inevitably lead to soil erosion. It is estimated that 90% of rain-fed arable land shows signs of degradation, of which 40% are highly degraded. The share of irrigated land has also decreased, further stressing the remaining fertile soils. Approximately 67,000 hectares of irrigated land suffer from various degrees of salinization, with another 2,880 hectares waterlogged and 1,400 hectares affected by water erosion. The Tajik government and international organizations are working to promote sustainable land management practices, including terracing and improved irrigation techniques, to combat these issues.

Flora

The Districts of Republican Subordination, encompassing a vast altitudinal range from the low-lying Hisor Valley to the high peaks of the Pamir Mountains, host a remarkably diverse and significant flora. This region lies within the Mountains of Central Asia global biodiversity hotspot and is characterized by a high level of plant endemism. Tajikistan as a whole has the highest species density and endemism among the five Central Asian countries. The country's flora includes about 4,115 species of wild seed plants, with 770 endemic species.

Vegetation Types

The region's diverse topography supports a wide range of vegetation types, which vary significantly with altitude.

• Lowland Valleys (e.g., Hisor Valley): The vegetation includes xerophytic (dry-adapted) scrublands with almonds, pistachio bushes, and various species of wild rose and hawthorn. River valleys support dense riparian forests of poplar, willow, and walnut.
• Mid-Altitude Woodlands and Shrublands (Shiblyak): Between approximately 1,600 and 2,600 meters, a significant vegetation type known as "shiblyak" occurs. This consists of mesophilous (moderately moist) scrub vegetation, including thickets with wild apple trees (Malus sieversii), hawthorn (Crataegus turkestanica), and various other shrubs.
• High-Altitude Zones: Above the treeline, the landscape transitions to subalpine and alpine meadows, and high-altitude xerophytes (dry-adapted plants). The highest peaks feature chionophilous (snow-loving) vegetation in the high alpine and subnival belts.
• Eastern Highlands (Pamir-Alai): The eastern part of the region, bordering the Pamir Mountains, features a distinct flora. Dominant plant genera include Artemisia, Seriphidium, Ceratoides, Acantholimon, Astragalus, Oxytropis, and Ephedra, with prominent families such as Poaceae (grasses), Cruciferae (mustards), Asteraceae (daisies), Rosaceae (roses), and Caryophyllaceae (pinks).

Fauna

The Districts of Republican Subordination host a diverse and significant fauna, reflecting the region's varied topography, which ranges from the low-lying Hisor Valley to the high peaks of the Pamir Mountains. This diversity makes the area a crucial haven for a wide array of species, including many that are rare and endemic to Central Asia.

The region's fauna is characterized by a rich variety of species. Across Tajikistan, the fauna includes 84 species of mammals, over 346 species of birds, 44 species of reptiles, and 49 species of fish. Romit Biosphere Reserve alone is home to 32 species of mammals, including the snow leopard, and numerous bird species.

Mammals

• 
  Bukharan markhor (Capra falconeri heptneri)
  A key endangered species with a dedicated breeding program in the Romit Biosphere Reserve.
• 
  Siberian ibex (Capra sibirica)
  The primary prey of the snow leopard, found in the high mountain ranges of the region.
• 
  Snow leopard (Panthera uncia)
  A flagship species for conservation, inhabiting the Hisor Range and other high-altitude areas.
• 
  Brown bear (Ursus arctos isabellinus)
  A large predator found in the region's forests and mountain slopes.
• 
  Wolf (Canis lupus)
  A common large predator in the region, inhabiting various terrains.
• 
  Eurasian lynx (Lynx lynx)
  A solitary predator found in the wooded areas and rocky terrains of the region.
• 
  Red fox (Vulpes vulpes)
  A widespread small predator in the region's diverse habitats.
• 
  Red marmot (Marmota caudata)
  A typical inhabitant of high-altitude meadows in the region.
• 
  Wild boar (Sus scrofa)
  Commonly found in the region's forests and valleys.
• 
  Pamir sheep (Ovis ammon polii)
  Found in the eastern highlands of the region, with a population exceeding 29,000 individuals.

The mammal population is particularly notable for its large predators and ungulates. The elusive snow leopard, a flagship species for conservation, inhabits the high mountain ranges of the region, including the Hisor Range. Its primary prey, the Siberian ibex, is also found in these mountains. Other large predators include the Brown bear (Ursus arctos isabellinus), wolves (Canis lupus), red foxes (Vulpes vulpes), and the lynx (Lynx lynx).

The region is a stronghold for several endangered ungulates. The Bukharan markhor (Capra falconeri heptneri), a wild goat with magnificent spiraling horns, is a key species, with a dedicated breeding program operating within the Romit Nature Reserve. Other notable species include the Bukhara urial (Ovis aries bochariensis), a wild sheep subspecies, and the Pamir sheep (Ovis ammon polii), which are found in the eastern highlands. The Pamir sheep population in Tajikistan has increased significantly, reaching over 29,000 individuals in recent years.

Smaller mammals are also abundant. The porcupine, wild boar (Sus scrofa), and several species of bats are commonly found in the region's forests and caves. The red marmot (Marmota caudata) is a typical inhabitant of the high-altitude meadows.

Birds

• 
  Golden eagle (Aquila chrysaetos)
  One of the impressive raptors that soar above the mountains of the region.
• 
  Griffon vulture (Gyps fulvus)
  A large raptor commonly seen soaring above the region's mountain ranges.
• 
  Himalayan snowcock (Tetraogallus himalayensis)
  A notable resident of the high-altitude rocky slopes in the region.
• 
  Bar-headed goose (Anser indicus)
  A waterfowl species found in the region's wetlands and lakes.
• 
  Northern wheatear (Oenanthe oenanthe)
  One of the wheatear species found in the region's diverse habitats.
• 
  Rock thrush (Monticola sp.)
  A species found in the rocky terrains of the region.
• 
  Hume's lark (Calandrella acutirostris)
  A bird species found in the region's open habitats.
• 
  Coot (Fulica atra)
  A waterbird commonly found in the region's lakes and wetlands.

The region's diverse habitats, from alpine meadows to river valleys, support a rich avifauna. Birds of prey are particularly well-represented. The golden eagle (Aquila chrysaetos) and griffon vulture (Gyps fulvus) are among the impressive raptors that soar above the mountains. The Himalayan snowcock (Tetraogallus himalayensis) is a notable resident of the high-altitude rocky slopes. The region's wetlands and lakes provide critical habitats for waterfowl, including the bar-headed goose (Anser indicus). Other bird species found in the area include various species of wheatears, rock thrushes, the Hume's lark, and the coot.

Reptiles, Amphibians, and Fish

The reptile and amphibian fauna, while less prominent than mammals and birds, is an integral part of the ecosystem. The region is home to several species of lizards, including agamid lizards, and snakes like the rat snake. The fish fauna is relatively limited due to the young age and mountainous nature of the region's rivers and lakes. However, species like the marinka fish (Schizothorax sp.) are found in the Shirkent River and other watercourses.

Protected Areas

To safeguard its unique biodiversity, the region hosts several important protected areas (PAs).

• Romit Biosphere Reserve: Established in 1959 as a State Nature Reserve, this protected area covers 16,139 hectares (161.6 km²) on the southern slopes of the Hisor Range. It was designated a UNESCO Biosphere Reserve in 2025. Its primary purpose is to protect the snow leopard, brown bear, and Siberian ibex, and it operates a breeding program for the endangered Bukharan markhor.
• Shirkent Historical-Nature Park: Established in 1991 (officially by decree in 1993), this is Tajikistan's first and only historical nature park. Covering 3,000 hectares (30 km²) in the western spurs of the Hisor Range, it protects juniper and walnut forests, as well as species like the snow leopard and urial. The park is also internationally renowned for its dinosaur footprint sites, with three distinct locations containing over 400 footprints.
• Sari-Khosor Nature Park: Established in 2003, this 3,085-hectare (30.85 km²) park is located in the region and aims to protect unique natural complexes and mountain forests.
• Komarov Sanctuary: This sanctuary is located in the Rasht district within the region.

Many of the region's animal species are under threat and are listed in the Red Book of Tajikistan, the country's official register of endangered species. The third edition of the Red Book, presented in 2025, includes 242 species of animals. The Tajik government has established hunting quotas for certain Red Book species to regulate their use. For instance, for the 2025–2026 period, quotas include 132 pamir sheep, 20 markhor, and 18 Bukhara urial. Conservation efforts are ongoing to protect these species and their habitats for future generations.

Climate

The Districts of Republican Subordination have a climate typical of central Tajikistan, characterised by significant regional variation due to the diverse topography. The climate is generally continental, with hot summers and cold winters.

In the lower valleys, such as the Hisor district, the average annual air temperature ranges from +14 to +17°C, with annual precipitation between 800 and 1,500 mm. The western valleys experience a milder climate, while the eastern mountainous areas are subject to harsher conditions. Summers can reach maximum temperatures of +40°C, while winter minimum temperatures can drop to −30°C.

Precipitation patterns vary significantly with altitude. In the valleys, most rainfall and snowfall occur during the winter–spring period. Snow begins to fall in October and may persist on the ground until May. At altitudes above 2,000 metres, snow cover can remain for up to 90 days per year. The eastern mountainous areas of the region, bordering the Western Pamirs, form a belt with a dry climate, moderately warm summers, and moderately harsh winters. Some areas, such as the Vanj River valley, receive annual rainfall ranging from 180–200 mm in lower areas to 800–1,200 mm at higher elevations near glaciers.

The Vakhsh river valley, encompassing areas such as Tojikobod, has a Köppen climate classification of Dsa (continental, dry-summer, humid continental), characterised by wet, cold winters and dry, cool summers.

According to the Köppen–Geiger climate classification, the region spans three distinct climate types. The majority of the region, comprising 103 locations, features a hot-summer Mediterranean climate (Csa). This climate is characterized by hot, dry summers and mild, wet winters. A second zone, covering 12 locations, has a hot humid continental climate (Dsa), with warm summers and cold, snowy winters. The remaining 3 locations experience a warm humid continental climate (Dsb), distinguished by cooler summers and very cold winters.

The following tables present climate data for three representative cities—one from each climate zone.

Vahdat – Hot-Summer Mediterranean Climate (Csa)

Vahdat, located in the Hisor Valley, experiences hot summers and relatively mild winters, with most precipitation falling in the winter and spring months. The average annual temperature is approximately 9.8 °C, and total annual precipitation is about 838 mm.

Climate data for Vahdat (1991–2020)
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Year
Mean daily maximum °C (°F)	3.6 (38.5)	5.2 (41.4)	11.5 (52.7)	17.1 (62.8)	21.7 (71.1)	26.3 (79.3)	29.5 (85.1)	29.0 (84.2)	25.0 (77.0)	18.4 (65.1)	11.1 (52.0)	5.3 (41.5)	17.0 (62.6)
Daily mean °C (°F)	−3.0 (26.6)	−1.0 (30.2)	5.2 (41.4)	11.2 (52.2)	16.0 (60.8)	20.3 (68.5)	23.5 (74.3)	22.7 (72.9)	18.2 (64.8)	11.6 (52.9)	4.3 (39.7)	−1.6 (29.1)	10.6 (51.1)
Mean daily minimum °C (°F)	−9.3 (15.3)	−7.4 (18.7)	−1.9 (28.6)	3.5 (38.3)	8.0 (46.4)	11.4 (52.5)	14.7 (58.5)	13.7 (56.7)	9.4 (48.9)	4.1 (39.4)	−1.9 (28.6)	−7.8 (18.0)	3.0 (37.5)
Average precipitation mm (inches)	89 (3.5)	119 (4.7)	142 (5.6)	138 (5.4)	107 (4.2)	32 (1.3)	10 (0.4)	4 (0.2)	11 (0.4)	36 (1.4)	71 (2.8)	79 (3.1)	838 (33)
Average relative humidity (%)	64	64	61	60	58	48	39	38	39	49	60	64	54
Source: Climate-Data.org

Roghun – Hot Humid Continental Climate (Dsa)

Roghun, situated at a higher elevation in the Rasht Valley, experiences a continental climate with cold, snowy winters and warm summers. Precipitation is abundant throughout the year, with a peak in spring. The average annual temperature is approximately 8.3 °C, and total annual precipitation is about 1,619 mm.

Climate data for Roghun (1991–2020)
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Year
Mean daily maximum °C (°F)	−0.7 (30.7)	1.2 (34.2)	6.4 (43.5)	11.3 (52.3)	17.9 (64.2)	22.4 (72.3)	25.4 (77.7)	25.4 (77.7)	21.5 (70.7)	14.2 (57.6)	5.9 (42.6)	0.6 (33.1)	12.6 (54.7)
Daily mean °C (°F)	−4.2 (24.4)	−2.3 (27.9)	2.6 (36.7)	6.9 (44.4)	13.0 (55.4)	17.5 (63.5)	20.7 (69.3)	20.5 (68.9)	16.4 (61.5)	9.1 (48.4)	1.6 (34.9)	−3.1 (26.4)	8.2 (46.8)
Mean daily minimum °C (°F)	−7.2 (19.0)	−5.5 (22.1)	−0.8 (30.6)	2.8 (37.0)	7.4 (45.3)	11.7 (53.1)	15.3 (59.5)	15.0 (59.0)	10.9 (51.6)	4.1 (39.4)	−2.3 (27.9)	−6.3 (20.7)	3.8 (38.8)
Average precipitation mm (inches)	140 (5.5)	180 (7.1)	213 (8.4)	220 (8.7)	217 (8.5)	131 (5.2)	78 (3.1)	50 (2.0)	43 (1.7)	93 (3.7)	121 (4.8)	133 (5.2)	1,619 (63.9)
Average relative humidity (%)	57	61	61	60	64	59	52	48	48	57	59	56	57
Source: Climate-Data.org

Lakhsh – Warm Humid Continental Climate (Dsb)

Lakhsh, the administrative centre of Lakhsh District, lies in the eastern highlands near the Pamir mountains and experiences the coldest conditions in the region. Winters are long and severe, while summers are short and mild. Precipitation is significant year-round, with a peak in spring. The average annual temperature is approximately 4.2 °C, and total annual precipitation is about 1,704 mm.

Climate data for Lakhsh (1991–2020)
Month	Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec	Year
Mean daily maximum °C (°F)	−4.7 (23.5)	−2.3 (27.9)	3.0 (37.4)	7.7 (45.9)	12.6 (54.7)	18.0 (64.4)	21.2 (70.2)	21.2 (70.2)	17.3 (63.1)	9.5 (49.1)	1.6 (34.9)	−3.5 (25.7)	8.5 (47.3)
Daily mean °C (°F)	−8.4 (16.9)	−6.0 (21.2)	−0.8 (30.6)	3.9 (39.0)	8.2 (46.8)	13.6 (56.5)	16.9 (62.4)	16.8 (62.2)	12.7 (54.9)	4.8 (40.6)	−2.6 (27.3)	−7.1 (19.2)	4.3 (39.8)
Mean daily minimum °C (°F)	−11.9 (10.6)	−9.7 (14.5)	−4.8 (23.4)	−0.3 (31.5)	2.9 (37.2)	7.7 (45.9)	11.5 (52.7)	11.3 (52.3)	7.4 (45.3)	−0.1 (31.8)	−6.7 (19.9)	−10.6 (12.9)	−0.3 (31.5)
Average precipitation mm (inches)	134 (5.3)	167 (6.6)	192 (7.6)	178 (7.0)	202 (8.0)	172 (6.8)	129 (5.1)	83 (3.3)	68 (2.7)	116 (4.6)	123 (4.8)	142 (5.6)	1,706 (67.4)
Average relative humidity (%)	61	64	62	62	67	65	59	54	53	60	62	59	61
Source: Climate-Data.org

The climate tables above illustrate the marked contrast between the relatively mild Hisor Valley (Vahdat), the colder but still warm-summer Rasht Valley (Roghun), and the high-altitude, cold-summer eastern highlands (Lakhsh). The average annual temperature decreases by nearly 14 °C from Vahdat to Lakhsh, while annual precipitation more than doubles, reflecting the influence of elevation and the region's complex orography.

Administrative divisions

The Districts under Central Government Jurisdiction (Tajik: Ноҳияҳои тобеи ҷумҳурӣ, romanized: Nohiyahoyi tobe’i jumhuriy) comprise 9 districts (Tajik: ноҳия, romanized: nohiya) and 4 district-level cities (Tajik: шаҳр, romanized: shahr) that are directly administered by the central government. The administrative centre of the region is the national capital, Dushanbe, which is geographically surrounded by the region but administratively separate from it. The region covers an area of approximately 28,500 km².

The following table lists the districts and district-level cities, along with their estimated populations as of 2024 and their former names where applicable.

Districts and district-level cities

Name	Native name (Cyrillic)	Status	Population (2024 est.)
Fayzobod	Файзобод	District	116,700
Hisor	Ҳисор	City	346,800
Lakhsh	Лахш	District	56,800
Nurobod	Нуробод	District	75,700
Rasht	Рашт	District	136,600
Roghun	Роғун	City	28,092 (2020 census)
Rudaki	Рӯдакӣ	District	449,600
Sangvor	Сангвор	District	21,000
Shahrinav	Шаҳринав	District	42,800
Tojikobod	Тоҷикобод	District	41,000
Tursunzoda	Турсунзода	City	114,586
Vahdat	Ваҳдат	City	133,740
Varzob	Варзоб	District	72,700

The region's administrative structure has evolved over time. After the dissolution of Stalinabad Oblast in 1951, the territories of the former province became directly subordinate to the government of the Tajik SSR, which is how the name came about. In 1955, the Gharm Oblast was dissolved and its territories became subordinate to the Republican Jurisdiction in the same manner. Today, the Districts under Central Government Jurisdiction cover much of the territory of those previously dissolved regions, except for Darvoz District which was moved to the Kuhistoni Badakhshon Region.

Demographics

The Districts under Central Government Jurisdiction are the most populous region in Tajikistan. According to the latest estimates, the region's population has grown steadily over the past decades, reaching approximately 2.2 million in 2024, up from 2.05 million in 2020. This rapid growth reflects both natural increase and internal migration from other parts of the country.

The region's population is predominantly ethnic Tajik. According to the 2010 census, Tajiks made up 85% of the population, while Uzbeks accounted for 11.7%. Other minority groups, including Kyrgyz, Russians, and Lakais, constitute the remainder. In 2006, the ethnic composition was reported as 81.4% Tajik and 14.5% Uzbek, indicating a gradual increase in the Tajik share of the population.

The official languages of the region are Tajik and Russian, which is widely used for interethnic communication. The majority of the population adheres to Islam, with Sunni Islam being the dominant denomination. In some eastern districts, such as those near the Pamir mountains, there is a significant Ismaili Shia minority.

The table below shows the historical population of the region based on census data and official estimates.

Historical population

Year	Pop.	±% p.a.
1979	757,976	—
1989	1,083,043	+3.63%
1999	1,337,479	+2.13%
2010	1,722,908	+2.33%
2020	2,045,157	+1.73%
2024	2,197,000	+1.81%
Source: Citypopulation.de

Urban and Rural Population

The region remains predominantly rural. In 2024, the estimated rural population was over 1.9 million, while the urban population was approximately 228,700. The largest urban centres are Hisor (population 346,800), Rudaki (404,800, includes urban and rural areas), and Tursunzoda (114,586). The region's administrative centre, Dushanbe, is geographically surrounded by the region but is administratively separate from it and not included in these figures.

Culture

• Mausoleum of Hodja Nashron

External links

• City Population – Tajikistan administrative units