General Information

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Trekking in Tibet

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Tibet Tours

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Mt. Kailash Yatra

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Mt.Kailash Yatra

Tibet Information

Geography

Climate

History & Culture

Buddhism Established

Tibet Festivals

Practical Information

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AMS - Precaution & Treatment

 

 

Double Dorjee

Tibet Trek

Everest B. Camp Trek

Lilung Trek

Eastern Tibet Trek

Y. Tsangpo Gorge

Shalu - Nartang Trek

Ganden Samye Trek

Lhamo Lhatso Lake

Namtso Lake Trek

Tsurphu Yangpachen
   

Tibet Tours

Tibet Tours

Lhasa Tour

The Hub of Tibetan

Sacred City Adventure

Lhasa-Gyantse-Xigatse

Lhasa - Tsedang

Lhasa Ganden

Cycling Tour

Budget Tibet Tour

Super Budget Tour

Tibet Overland Tour
   

Mt.Kailash Yatra

Mt.Kailash Yatra

Mt. Kailash Mansarovar

Mt. Kailash - Lhasa I

Mt. Kailash - Lhasa II

Lhasa to Mt. Kailash

Mt. Kailash - Lhasa

Humla - Kailash
   
 
 
 
 
 

Tibet Information

 
 

Tibet Climate

The Tibet Plateau's various complex topographies and landforms engender a distinctive climate. Beyond the general tendency of a cold, dry northwest and a warm, wet southeast, can be found a wide variety of localized climates and distinct vertical climatic belts. Two sayings "different weather five kilometers apart" and "four seasons in one day" well describe this phenomenon.

Tibet has thinner air, more sunlight, lower temperatures and less precipitation than other areas in China. The air contains only 150 to 170 grams of oxygen per cubic meter, 62 to 65.4 percent the rate found in plains areas. Solar energy is more readily available than elsewhere nationally, with more than one-third to even double that available in plains area at the same latitude. There are also more hours of daylight than elsewhere in China; in Lhasa there are 3,021 hours of daylight annually. Daytime and nighttime temperature vary greatly, despite low average temperatures and low annual temperature differentials. Average temperatures and peak temperatures for the hottest month in Lhasa and Xigaze are 10-15 degrees centigrade lower than in Chongqing, Wuhan and Shanghai at about the same latitude. Annual temperatures in Lhasa, Qamdo, Xigaze and elsewhere in Tibet range 18 to 20 degrees centigrade over the yea! r. At elevations in excess of 5,000 meters in Ngari Prefecture, daytime temperatures in August climb above 10 degrees centigrade, only to fall below zero at night.

Seasonal precipitation is disproportionately distributed throughout the region. The dry season and the rainy season are clearly demarcated. Rain usually falls at night. Annual precipitation is 5,000 millimeters in the lower elevations to the southeast decreasing gradually to a mere 50 millimeters in the northwest. Precipitation from October to April accounts for only l0 to 20 percent of the yearly total. Rainfall is concentrated in the period between May and September, accounting for about 90 percent of the yearly precipitation.

 

Geological Features of Tibet
From the view of earth science, Tibet plateau is one of the most interesting regions in the world.

It is the highest plateau in the world, with an average altitude 4,500 meters. Tibet Plateau has many firsts as following: It has the highest mountains in the world Mt. Qomolangma 8,850 meters

It has the largest canyon in the world Yarlung Zangbo River Great Canyon with a total depth 5,382 meters. It has the largest scale of vertical eco-system zones, from the highest point on the earth 8,850 m, to the bottom of valley 900 meters elevation. It has numerous glaciers and originations of many important rivers are here. It has very unique environment and many unique plateaus.

Tibet Plateau is the main body of the Qinghai-Tibet Plateau, consisting of high mountains and great rivers, prairie and gorges. On the Tibet Plateau stands the world-famous Himalayas in southwest, the Kunlun Mountains and the Kalakunlun Mountains spread the northwest, the Gangdisi, Tanggula and Nyainqentanglha Mountains traverse the middle, and the Hengduan Mountains is its east barrier. There are 6 peaks of over 8,000 m! eters at sea level, 50 peaks of over 7,000 meters at sea level and numerous peaks of over 6,000 meters at sea level in Tibet, where the world's highest summit Mt. Everest erects with an elevation of 8848.13 meters.

Amidst the numerous high and gigantic mountains spread a range of hills, lakes and gorges, constituting undulation alpine prairie. The famous Qiangtang Grasslands on North Tibet spreads from east to west over 2,400 kilometers and from north to south over 700 kilometers, averaging 4,500 meters at sea level. The boundless grassland is the principal pastoral area in Tibet.

Tibet is also one of the regions in the world with the most gorges. These gorges mainly distribute in the east of the Tibet Plateau and the south outlying areas, culminated by the Yarlung Zangbo Great Gorge and East Tibet Three Rivers Gorges.

There are intensive rivers and lakes in Tibet. There are over 20 rivers with valley area larger than 10,000 Square kilometer, and over 100 river! s with valley larger than 2,000 square kilometers. The famous rivers include the Yarlung Zangbo, Jinsha, Nujiang and Lancang rivers. The Asia-famous Ganges River, Indian River and Mekong River all originate there. The region has over 1500 lakes including 47 with over 100 square kilometers. Lake area stands at 24,183 square kilometers, representing over one-third of the total lake area in China.

 
 
   

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