Asia River MapMap of Asia River
Asian Fluvials, Asian Landforms
Many important watercourses originate in Asia. In this section we emphasize some of the most important ones on the map and describe (briefly) some of them, among them the Ganges, Indus, Lena, Mekong, Ob, Yangtze and Yellow. The GangesThe Ganges is the holiest river for Hindus and is also a vital artery for tens of thousands of Indians who are living along its course and are dependent on it for their everyday needs.
Lena is the most eastern of the three major Serbian streams that run into the Arctic Ocean (the other two are the Ob River and the Yenisej River). At 4,400 km, it is the eleventh longest river in the whole canyon. Indus has its source in Tibet and runs through India and Pakistan.
River Ob is an important river in West Siberia, Russia. China's Yangtze is the longest river in Asia and, at 6,301 km, the 4th longest river in the canal. Yangtze dewaters one fifth of the territory of the People's Republic of China and its river basins are home to one third of the Chinese people.
With a length of 5,464 km, the Yellow River is the second longest river in China and the 6th longest in the whole wide range. It is known as "the cradles of China civilisation " because its basins - especially the Wei River valleys - were the birthplaces of old China civilisations and the wealthiest regions of early Tibet.
Wellcome to Rivers of Asia
Over the course of time, the river has been a source of electricity and heat. Utilize the top meal to discover some of Asia's most important canyons. Kindly be aware that flows from other jurisdictions will be added to this website step by step. Due to its unparalleled geography and climate, China also has the greatest hydropower production capacity along its watercourses in all parts of the globe.
China's problems with its waters and its relations with its watercourses are therefore of great importance to the whole planet. Utilize the top meal to discover two of China's most important rivers: the Yellow and the Yangtze. With a length of 6,418 kilometres, the Yangtze is of key importance for the economy of more peoples than the population of Russia and the United States put together.
The Yangtze studies serve not only as a gateway to China's geographical, ecological, economic, cultural and historical background, but also to its own futures. For more information about the Yangtze, click a pushbutton below. Discover different places along the Yangtze River by clicking on the map below and choosing the locations marked in orange. Yangtze did not always existed.
Indeed, the fluxes, hills, continents as well as seas on the planets today have been created over million and million and millions of years. This section tells us how the Yangtze was "born" through the study of Chinese soil and climatic conditions. Was the Yangtze "born"? Just think, you wanted to make a new river.
Firstly, of course, you need to get your river supplied with drinking and drinking mineralogy. There would be no river without it. Secondly, you need an area where your river could run and this country should be sloping and bumpy (e.g. with hills and valleys) so that your river has a clear downhill trail.
When your country is totally shallow, your waters would have no place to run and would never turn into a river. So in order to comprehend how the Yangtze was "born", we need to investigate two things: how the Yangtze got its waters and how the ground in China became so bumpy. What makes China so irregular?
China's country is very bumpy. Let's begin with China's country. Today, China's territory is full of hills and dales, especially in southern and western China, the areas nearest to India. The Yangtze also comes from the Tibetan plateau. As India clashed in Asia, it created huge quantities of country to move, lift and wrinkle - similar to a motor accident can move, lift and wrinkle the bonnet of a vehicle.
It was this fierce continental conflict that changed the country drastically, creating the vast Tibetan plateau, the Himalayas and several other mountains over the course of several million years. India has not yet ended its northernrift; it is still gradually collapsing into the remainder of Asia, increasing the country around it by a few centimetres every year and creating a number of catastrophic seismic events.
Now, that we have understood how the Yangtze has taken its course, we want to know how the Yangtze gets its run. Where does the Yangtze get its waters? It is a river system that flows down the hill, collects in a river system and finally flows into the ocean, and the area that a river system dewaters is known as a "catchment area" or "watershed".
" Large watercourses often have very large catchment areas. The Yangtze River valley, for example, occupies about one-fifth of China's entire area. Every drop of raindrops that fall in this area finally reaches the Yangtze. Below is the Yangtze River system and the catchment area. The Yangtze River has another important spring, the melting of glaciers, although the rains supply most of the Yangtze's waters.
The Yangtze River originates in the west highland of the Tibetian Plateau, where much of its spring flows from snow and glacial mass. Tibet's plateau is the third biggest icehold in the Arctic and Antarctic, and when these huge glacial and snow masses melts, their bodies of cold sea cold sea cold sea cold sea cold sea cold sea cold sea cold sea cold water flows into river basins like the Yangtze.
The city of Hankou was one of many Yangtze River coastal areas in China that were inundated. The Yangtze River, like other watercourses, sways. The Yangtze River's waters rise in spring and fall in spring and autumn. In a few seasons, when the river levels rise too high, the river can even break its banks and flooding near arable land, communities, towns as well as communities.
Flooding like this has often taken a huge toll, involving the destruction of lands, properties and even human life. How is the foreseeable Yangtze variation caused? Firstly, the glacier and glacier near the river spring rapidly melts in the hot summers, providing the Yangtze with more waters and increasing its levels.
There are different climatic zones in different parts of the globe, and each of them is characterised by many different conditions such as temperatures, prevailing and rain. The majority of all year round blowing in the same way. However, the seasonal rains of the monsoons are blowing in different ways. In China's summers, the monsoons blast from the ocean to the countryside and bring moist breezes to China.
The humid climate results in China's rain. However, in winters the wind changes directions and blasts from shore to shore. Whilst the wind is blowing into the ocean via China, it is being substituted by cool, arid wind from northern and western China (Siberia and Inner Asia). As this Siberian and Asian inner climate contains very little humidity, it is relatively seldom in China.
The monsoons are blowing on shore (from ocean to shore) in summers. The wind blows off the coast (from shore to sea) in cold weather. In order to comprehend why China's summers are blowing as opposed to its winters, we must first begin by understanding three principles: Soil temperatures can vary rapidly and strongly, but the changes in surface temperatures are slow and moderate.
As soon as we have understood the three principals, we will put them together to illustrate why the storms of the monsoons are changing. For this reason, the compressed atmosphere always travels from high pressures (i.e. areas with thick molecules) to low pressures (i.e. areas with few molecules). This means that the breeze always flies away from the high-pressure plants and towards the low-pressure plants.
Phrin 3: The ground can vary rapidly and strongly, but the surface changes gradually and only slightly. Shore temp. fluctuates more than ocean temp. throughout the year. Lands are made of many different kinds of stone, ground, sand, etc. While each of these has its own characteristics, overall they are rapidly changing in heat or cold.
If for example, if you had the outside of your house in the midday (after being heated in the hot air for several hours) and the midnight (after being cooled for several hours), you would get two significantly different numbers. Well, water's different.
Had you measured the temperatures of a marine or oceans in the midday and midnight, your two temperatures would have been very similar. After all, if you heat or cool it, your plumbing changes its temperatur gradually. As a result, the marine temperatures hardly ever vary during the course of a single full year.
Due to the changing season from season to season, shore temperature fluctuates faster and more dramatic than oceanic. The country gets warmer than the ocean in summers and cooler than the ocean in winters. What do these three basic reasons account for the regurgitation of monsoons? Monsoons blow on shore (from ocean to shore) in summers.
Molecule reds are warm, molecule greens are at a modest°C. First, we think about what happens in it. Onshore summers are higher than oceanic. This makes the terrestrial atmosphere - which we can call "continental air" - warmer than the oceanic ( "maritime air").
After all, because the atmosphere always flows from areas with higher pressures to areas with lower pressures, the winds blow from the ocean to the countryside. So we can understand why the summer monsoons blow from ocean to ocean. Monsoons blow off the coast (from country to sea) in winters. Bluish molecule is cool, whereas greens have a moderately high body heat.
This is the opposite of what happens in wintry times. As the temperature of the shore fluctuates more than the temperature of the ocean, the country is now getting cooler than the ocean. Refrigerated mainland European fresh water becomes tight and forms a high-pressure system overland. Thus the skies move away from the mainland and produce the windy winters of the monsoons that are blowing fromshore.
You can see that if we combine these three principals, we can understand why the direction of the month changes from sun to dark. 5. When it is expanded, it is created: The country gets warm and colder than the ocean in summers. The country gets warm in winters.
Discover China's geographical situation using the map below. For more information on current topics around the Yangtze, click on a theme below. Therefore, the use and distribution of irrigation waters is a pivotal element in the country's historical politics and emotions. The Yangtze is an area where flooding and drought are an integral part of our lives.
The Yangtze River has been flooded every ten years from the second millennium B.C. to the present day, with disastrous flooding every hundred years. Between the beginning of the Han Dyinasty in 206 BC and the end of the Qing Dyinasty in 1911, 214 large flooding occurred along the Yangtze River.
As a rule, the biggest devastation was in the central area, where the country is low and densely inhabited. Just four years later, in 1935, another 142,000 lives were lost when 3.74 million hectares were again inundated, diverting the waters to the densely inhabited fields in the northern hemisphere.
The Yangtze River again inundated in 1998, claiming 3,656 lives and destroying 5. Over the years, China's rulers were hoping that a large hydroelectric reservoir would not only alleviate the pain and devastation of uncontrolled water bodies in the summers, but also give strength for broadly based economical growth. Twenty large cascades of reservoirs are already using the Yellow River, another 18 are to be constructed by 2030.
More than $25 billion was spent on the construction, forcing more than 150 million displaced persons (almost half the US population) and sinking farm land, urban areas and some of China's most venerated landscapes and ancients. Nearly half of the Chinese inhabitants of North China live in this dry countryside, which contains only 15 per cent of the world' s waters.
It accounts for more than 25 per cent of China's entire GDP and produce most of its cereals. More than 400 of China's 660 towns are lacking enough drinking more. China's huge landscape - and its 738 million farmers, more than twice the size of the United States' populations - also bear the main burden of this shortfall.
Unlike northern China, most rainfall and ground waters are located in the southern regions, where demographic densities and levels of industry are significantly lower. The geographical disparity between populations, output and irrigation is a major cause of China's problems with irrigation. In order to meet the increasing serious hydrological challenge in the Nordic countries, the Chinese authorities have tried to meet the challenge with huge engineer-operations.
The $65 billion South-to-North Technology Transfer Program, started in 2002, is the biggest building venture in mankind's entirety. It will transport huge amounts of groundwater from the South Yangtze River to the water-hungry northern region through a range of large aqua products - an east, centre and west road that will be cut through hills and corroded through desert, redirecting the waters for centuries.
While the first stage of the operation, which will be completed in 2013, is expected to start supplying Beijing with drinking waters, many have argued that the following sections appear unsustainable in geological, structural and financial terms. A lot of pundits wonder whether already removed streams can conserve the waters, whether mud endangers the site and whether irreparable damage is done to delicate and singular eco-systems.
It is a short-term road to sustainable expansion that will support the country's economy and provide the necessary support for maintaining the viability of the Chinese people and the credibility of the state. It is indispensible for all living things and people. Only about 2.5 per cent of all waters on earth are fresh waters.
Fluvial waters are the most important system through which fresh waters are supplied to us all around the globe, but we endanger this valuable resourc. Using the mud that they transport and settle over many aeons, streams have transformed riverbeds and their broader basin into wealthy arable land on which many communities rely to feed their people and provide the necessary waters for agriculture.
Nile is just one example among many. Big and middle size watercourses have always been important traffic routes for the goods traffic, for the immigration of the population and for the cultural and linguistic movements that these immigrants involve. Before land traffic developed in recent century - railroads and motorways - the only way to carry heavier goods was by river and canal.
Even today, river transport is indispensable to the economies of many nations, even our own. Some of the world's largest towns lie where the Thames ( "London"), the Hudson ("New York") and the Yangtze ("Shanghai") meet. Lastly, in this short outline, fluxes are a source of force and a source of electricity.
China's problems with its waters and its relations with its watercourses are therefore of great importance to the whole planet. China is divided into approximately eight major areas by mountain, river and other geographic features. The nuclei are connected to river ecosystems in most areas. While flooding can be threatening and sometimes devastating, it does provide ample and reliable supply of drinking waters for watering and other people.
The river system was also an important route of migrations along which the Chineses expanded and settler. So it is no coincidence that China's biggest towns have always been in the region's centres, mostly near important watercourses - as in many other companies.
China's 6,418-kilometer-long Yangtze is unlike any other major river in the canal. The Nile and the Amazon are the only longer and its volumes of fresh waters are among the top five. The Yangtze, which originates from the Tibetan plateau and ends where it ends in the East China Sea, splits and links the state.
Yangtze River divides 19 counties and is of key importance to the economies of more peoples than the population of Russia and the United States put together. The Yangtze studies serve not only as a gateway to China's geographical, ecological, economical, cultural and historical background, but also to its own futures. which blow through the Gobi Desert and other dry areas of Inner Asia, have collected countless cu. mls. of powder and thin sands and deposited this cargo over large parts of northwestern and northern China.
The yellow, windy ground, known as loose, gives the river its colour. This high sludge load combined with unforeseeable sea level makes another important distinction between the Yellow and the Yangtze: the Yellow River is almost unusable for transportation.