| Pagri Phari |
|
|---|---|
| Tibetan transcription(s) | |
| • Tibetan | ཕག་རི |
| • Wylie transliteration | phag ri |
| Chinese transcription(s) | |
| • Traditional | 帕里镇 |
| • Simplified | 帕里镇 |
| • Pinyin | Pàlǐ zhèn |
|
Pagri
|
|
| Coordinates: | |
| Country | China |
| Province | Tibet Autonomous Region |
| Prefecture | Shigatse Prefecture |
| County | Yadong County |
| Population (2004) | |
| • Total | 2,121 |
| Time zone | CST (UTC+8) |
Pagri or Phari (Tibetan: ཕག་རི, Wylie: phag ri; Chinese: 帕里镇; pinyin: Pàlǐ zhèn) is a town in Yadong County in the Tibet Autonomous Region, China, near the border with Bhutan. Population 2121 (2004).[1] It is one of the highest and coldest towns in the world, being 15,000 feet above sea-level.
Contents |
Thomas Manning, the first Englishman to reach Lhasa, visited Pagri from 21st September until 5th November 1811 and had this to say about his room: "Dirt, dirt, grease, smoke. Misery,but good mutton.", a verdict which probably could have applied to the whole town[2]. Pagri was of some military importance in the early 20th century when it was occupied by the British expedition under Francis Younghusband in 1904. The Pagri Fortress (Dzong) was located here and was important for the government as it stood between Tibet and Bhutan. Pagri was a staging area en route to Gyantse and ultimately Lhasa.
During the summer of 1912, the 13th Dalai Lama met Agvan Dorzhiev at Phari Dzong and then accompanied him to the Samding Monastery, before returning to Lhasa after his exile in India.
Thubten Ngodup, the current Nechung Oracle, was born in Phari in 1957.
The houses are mostly made of Tibetan traditional stone and wood. The Pagri Valley lies in an alpine steppe zone on the south side, with an average annual temperature -0.2 ℃, and an extreme maximum temperature of 19.3 ℃.[1] Annual precipitation is about 380 mm, snow and ice melt forming rich water resources, shrubs and meadows development, a good place for the development of animal husbandry. Pagri is rich in minerals, wild animals, plants, and tourism resources. It is also a trading centre but due to geographical location is prone to natural disasters.[1] Summer flash floods, mudslides, winter avalanches, snowstorms, etc. are common, and poor facilities makes it vulnerable to disaster.[1] During the rainy season, water levels rise causing serious flooding, reducing soil quality and arable land every year, damaging the ecological environment and a threat to the inhabitants of Pagri.[1] To the northeast of Pagri is Mount Jomolhari.
Owing to its extreme altitude, Pagri has an alpine climate (Köppen ETH) that is too cold to permit the grow of trees, even though the altitude is still marginally too low for the formation of permafrost. The winter is severe in spite of the fact that no month has daytime maxima below 0 °C (32 °F), and also very dry and long, extending as late as May. Snowfall, however, is rare because of the dryness. Summers, during which the great majority of precipitation occurs, are cool even at their warmest and consistently damp even though the Himalayas prevent falls from ever being heavy.
| Climate data for Pagri | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °C (°F) | 14.7 (58.5) |
13.8 (56.8) |
15.4 (59.7) |
16.6 (61.9) |
16.5 (61.7) |
18.1 (64.6) |
18.6 (65.5) |
17.3 (63.1) |
16.4 (61.5) |
16.8 (62.2) |
16.4 (61.5) |
13.2 (55.8) |
18.6 (65.5) |
| Average high °C (°F) | 0.9 (33.6) |
1.4 (34.5) |
3.9 (39.0) |
7.0 (44.6) |
10.0 (50.0) |
12.5 (54.5) |
12.8 (55.0) |
12.7 (54.9) |
11.4 (52.5) |
8.2 (46.8) |
5.3 (41.5) |
3.2 (37.8) |
7.44 (45.39) |
| Average low °C (°F) | −17.2 (1.0) |
−15 (5) |
−10.4 (13.3) |
−5.5 (22.1) |
−1.3 (29.7) |
3.0 (37.4) |
4.4 (39.9) |
4.0 (39.2) |
1.8 (35.2) |
−4.9 (23.2) |
−11.7 (10.9) |
−16.1 (3.0) |
−5.74 (21.67) |
| Record low °C (°F) | −28.7 (−19.7) |
−28.4 (−19.1) |
−29.8 (−21.6) |
−20.2 (−4.4) |
−12.5 (9.5) |
−5.7 (21.7) |
−1.1 (30.0) |
−2.1 (28.2) |
−6.5 (20.3) |
−21.5 (−6.7) |
−26.2 (−15.2) |
−27.4 (−17.3) |
−29.8 (−21.6) |
| Precipitation mm (inches) | 5.0 (0.197) |
8.8 (0.346) |
21.8 (0.858) |
27.9 (1.098) |
31.0 (1.22) |
57.1 (2.248) |
104.8 (4.126) |
95.7 (3.768) |
54.2 (2.134) |
27.9 (1.098) |
4.5 (0.177) |
2.8 (0.11) |
441.5 (17.382) |
| Avg. precipitation days | 2.8 | 4.9 | 9.4 | 12.9 | 17.4 | 21.7 | 27.3 | 27.4 | 21.5 | 7.1 | 1.9 | 1.4 | 155.7 |
| Source: Weather China [3] | |||||||||||||
This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press.
|
|||||||||||||