The climate in highland Tibet belongs to the typical downy special climate. Climates are much different in different areas in Tibet and temperatures vary greatly within a single day.
Climate in southeastern Tibet (e.g. Nyingchi) is gentle and temperate with the average temperature of eight degrees; In western Tibet (e.g. Nakqu), the average temperature is below zero degree; While in Lhasa and the central part of Tibet, the climate is normal and nice for traveling. Visitors would not feel cold in winter nor hot in summer, especially from March to October, the best seasons for traveling. Most annual rainfall comes in the rainy season that starts from May to September, when the precipitation covers 90 percent of the whole year. Usually it rains at night in Lhasa, Shigatse and Chamdo area. The precipitations gradually decrease from 5000 millimeters in the lower part of southeast to just 50 in the northwest.
So generaly speaking, the best time to travel Tibet is between April and October, and peak season is from May to September. The best months are May, June, September or October as July and August are rainy months. Those who travel in their own car or on foot should avoid the rainy season especialy when entering Tibet along the Sichuan-Tibet Highway, and the sections between Lhasa and Nyingchi and between Lhasa and Ngari. There will be mudslides, cave-ins and mire on certain sections of the road, blocking the passage of vehicles. However, if you are only planning several days in and around Lhasa and getting there by air. There will be no problem for you to travel at any time from April to October.
Savanna
Relief, or the physical landscape of an area, can influence climate by affecting factors such as temperature, precipitation, and wind patterns. For example, mountains can block weather systems and cause rain shadows, leading to different climate conditions on either side. Coastal areas may experience milder climates due to the moderating effects of the nearby ocean.
The five main factors affecting the British climate are latitude, distance from the sea, ocean currents, prevailing wind direction, and relief (topography). The latitude of Britain results in mild temperatures, while the surrounding sea influences the climate by moderating temperature fluctuations. Ocean currents also play a role in regulating temperatures, while prevailing winds bring moisture and affect weather patterns. Relief or topography influences local climate variations, such as the rain shadow effect.
The five soil factors that geographers study are parent material, relief, climate, organisms, and time. Parent material refers to the rock or sediment from which soil is formed, relief considers the landscape's shape and slope, climate influences temperature and precipitation patterns affecting soil formation, organisms refer to the living organisms that contribute to soil formation, and time is the duration for soils to develop.
Egypt has a desert climate in Lower Egypt, characterized by hot summers and mild winters. Rainfall is minimal, and temperatures can reach over 100 degrees Fahrenheit in the summer months. The region is influenced by the Mediterranean Sea, providing some relief from the extreme heat.
It is what westerners called "tibet". Xizang is one part of China
Lhasa...Xi-Zang is what Chinese call Tibet.
Xizang.
Chunya Chai has written: 'Xizang hong yang pi shu' 'Xizang liu lang ji'
climate condition
Savanna
Meifen. Yang has written: 'Xizang'
Jinshan. Hu has written: 'Xizang \\'
Shijiang Ling has written: 'Xizang shi jian' -- subject(s): Social life and customs, Chinese essays 'Shuo hao yi qi qu Xizang'
The distance between Lhasa, Xizang, China and Urumqi, Xinijiang, China is 1657.9 miles. The journey takes approximately 2 days and 4 hours. Xizang is better known as Tibet.
Gang Che has written: 'Mi jing Xizang'
Relief, or the physical landscape of an area, can influence climate by affecting factors such as temperature, precipitation, and wind patterns. For example, mountains can block weather systems and cause rain shadows, leading to different climate conditions on either side. Coastal areas may experience milder climates due to the moderating effects of the nearby ocean.