What are some recommended books and travel notes about traveling in Tibet? Why does it rain so much in Lhasa, Tibet?

Because Tibet is full of plateaus and hillsides, and towns are built in river valleys near water sources, Lhasa is located in the Lhasa River Valley. On the Tibetan Plateau, the temperature changes 24 hours a day are significantly affected by the solar radiation heat. At the same time, due to the large altitude difference between the hillside and the river valley, the temperature difference at different altitudes at the same time is also very obvious. The higher the altitude, the lower the temperature. Every morning, the plateau is subjected to the local unique strong radiation of the sun. The earth absorbs the radiant heat of the sun, and the temperature is generally rising. So what are some recommended books and travel notes about traveling in Tibet? Why does Lhasa, Tibet love to rain at night? Let's take a look at the introduction of Encyclopedia Knowledge Network!

Contents of this article

1. What are some recommended books and travel notes about traveling to Tibet?

2. Why does it rain at night in Lhasa, Tibet?

3. What are the stones piled up in Tibet?

4. Does the Yellow River flow through Tibet?

What are some recommended books and travel notes about traveling in Tibet?

1. "Tibet Horizon: A Travel Diary in the Heart of Tibet", written by Zhang Bo.

2. "Traveling in Tibet", written by Ning Xin.

3. "Tibet Self-guided Tour Guide", written by Jian Xin.

4. "Reading Tibet", written by Li Ye.

5. "A Strong Woman Meets Love in Tibet: Reincarnation", written by Piaosha.

6. "Traveling Across China Before Age 28", written by a travel photographer.

7. "Women on the Road: Diaries Printed by Wheels", written by Li Yan.

8. "Next Stop: Lhasa", written by Zhao Fengchao.

9. "My Solo Cycling Trip to Tibet", written by Ao Xiangying.

10. "Encounter in Tibet", written by Shui Yiyi.

Why does it rain at night in Lhasa, Tibet?

After noon, the ground temperature reaches its peak. Starting in the afternoon, the amount of radiant heat absorbed by the ground from the sun gradually decreases, and the ground dissipates heat faster. At this time, the high-altitude hillsides and plateaus begin to cool down first, and the atmospheric temperature at the same altitude as the hillsides and plateaus also decreases. The air becomes colder, the density increases, the weight of the air becomes heavier, and gradually decreases. The air at high altitudes cools and descends to the valley area at low altitudes, while the warm and humid air originally in the valley area has a low density and light weight, and begins to rise under the pressure of the cold air descending from the high slopes. When the warm and humid air continues to rise and reaches a certain height, the moisture in the air begins to condense into countless tiny water droplets suspended in the air. This is the cloud. The cold air on the high slopes continues to descend, and the warm and humid air in the valleys is constantly lifted; the warm and humid air continues to rise and condenses into small water droplets, so the clouds accumulate and become thicker; more and more small water droplets are condensed, and they gather together, and the water droplets gather and grow larger, and finally the rising airflow can no longer support the growing water droplets, and these water droplets can no longer float in the air and fall down, and then it rains. From the high slope dry cold air descending, the warm and humid air in the valley rising, to the warm and humid air condensing into clouds, and cumulus clouds into rain, it is a very long process, usually starting in the afternoon and lasting until the evening, and it is night when it rains. A night rain often brings all the moisture in the sky down in the form of raindrops, and by the next morning, it is good weather with no clouds and the sun shining. This kind of weather is sunny during the day and rainy at night, which is determined by the terrain of the high slopes and valleys with an altitude difference of thousands of meters.

What are the stones piled up in Tibet?

In Tibet, stones are piled up into a Mani pile, or Duobeng in Tibetan. Tibetans believe that stones have spirituality, so they pile stones into Mani piles at intersections, lakes or mountains to pray for blessings. When Tibetans pass by a Mani pile, they walk around it clockwise and add another stone, so the longer the Mani pile is, the larger it becomes.

Mani stones vary in size and shape, ranging from the big ones like mountains to the small ones that can fit in the palm of your hand, or round or square in their natural state. In addition to being mostly white in color, their textures are also very different, including limestone, siliceous rock, white marble, and so on.

The initial Mani pile may not be very large, but according to the traditional customs of the people on the plateau, when passing by the Mani pile, they will chant something, call on the gods, pray for the blessings of heaven and the gods, remove disasters, get happiness, and circle around the Mani pile and add another stone. Even if there is no stone, they will add animal heads or horns or wool, or even their own hair. In this way, after a long period of time, the scale of the Mani pile will become larger and larger.

Does the Yellow River flow through Tibet?

The Yellow River is a major river in northern China, with a total length of about 5,464 kilometers and a drainage area of ​​about 752,443 square kilometers. It is the fifth longest river in the world and the second longest river in China.

The Yellow River originates from the Zhaqu River in the Chahasila Mountain of the Bayankala Mountains on the Qinghai-Tibet Plateau in Qinghai Province, the Karji River in the northern foothills, and the Yuguzonglie River in the west of the Xingxiu Lake, forming a "J" shape. From west to east, it flows through nine provinces, including Qinghai, Sichuan, Gansu, Ningxia, Inner Mongolia, Shaanxi, Shanxi, Henan and Shandong, and finally flows into the Bohai Sea.

The upper and middle reaches of the Yellow River are mainly mountainous, while the lower and middle reaches are mainly plains and hills. Since the middle reaches of the river flow through the Loess Plateau in China, it carries a lot of silt, so it is also known as the river with the most sand in the world. However, in Chinese history, the diversion of the lower reaches of the Yellow River has had a huge impact on human civilization.