Where is the Tibetan Plateau and can you escape the big floods

Buy a ticket to Lhasa, it's on the Qinghai-Tibet Plateau, and never come back, you can definitely avoid the super flood!

In the southwest, if there is a particularly large flood, it should be avoided because of the high altitude.

The Qinghai-Tibet Plateau is in the western part of China, with an average altitude of 5,000 meters. But in the face of the apocalyptic flood....

It's hard to say, extreme areas like this are either the safest or the most dangerous, it is recommended that you go to the sea and build a suspended base in the sea, so that you can take advantage of the gentle nature of the sea water should help you avoid fighting disasters.

When there is a big flood, the earth's crust will definitely change, but it may not be the safest place, so let's stay honest.

Why don't you go to Noah's Ark?

The huge Qinghai-Tibet Plateau is like the influence of large stones on the river that are not exposed to the water, causing the westerly wind belt below 500 mb (3 4 km) to branch out and circulate in winter, and form two air currents in the north and south. Part of the northern branch airflow blows into the Tarim Basin along the Altun Mountains, and part of it blows into the Hexi Corridor along the Qilian Mountains to the west or northwest, and the two converge into the northwest airflow in the eastern part of the plateau, and the streamline is anticyclonic and curved, forming a dynamic high-pressure back, which further strengthens the cold high pressure on the plateau and is conducive to the southward movement of the winter monsoon. The constraints of the plateau make the winter monsoon stronger.

The southern branch airflow is a northwest airflow in the southwest of the plateau, bypassing the south side of the plateau and turning into a southwesterly airflow, and the streamline is a cyclonic bending, resulting in a dynamic low-pressure trough, and under the influence of the warm and humid airflow in front of the trough, the winter climate in southern China and northern China is quite different. The two air currents in the north and south converge in the middle and lower reaches of the Yangtze River, forming the most powerful westerly wind belt in the northern hemisphere.

The dynamic effect of the Tibetan Plateau is also manifested in its barrier effect on near-surface airflow. In the east-west direction, it blocks the weather system moving eastward with the westerly airflow, and in the north-south direction, it directly blocks the north-south communication of cold and warm air in the troposphere in the western part of China. The winter plateau blocks the southward movement of the winter monsoon, making India on the southern side warmer and lower in pressure compared to other regions at the same latitude, with a small annual temperature range.

At the same time, the westerly pressure system is blocked by the plateau to stay, weaken and die out on the west side, while the Sichuan Basin area on the east side is relatively calm, with less airflow disturbance and weak wind. The north side of the plateau is not susceptible to the influence of warm and humid airflows from the south. It is conducive to the accumulation of cold air, which further strengthens the power of the Mongolian high pressure, and then produces a strong cold snap in the eastern part of China.

However, the plateau blocks the moist ocean airflow from entering the northwest basin of China, forming a dry and hot weather with little rain, making Xinjiang extremely arid and becoming a rare area with little rain and no flow.