The direct source of Danniang's sand dune

Danniang Sand Dune was located in Danniang Township, Milin County, Xizang, 90 kilometers away from the confluence of the two rivers. It was the largest sand dune in the middle of the Yarlung Zangbo River. The sand dunes were formed mainly because the sand grains from the nearby sandbars and floodplains were piled up on the slopes by the wind, forming the current sand dunes over time. Danniang Sand Dune was also known as the Buddha Palm Sand Dune because it was shaped like a Buddha's palm. The climate in this area is diverse, including tropical, sub-tropical, temperate-zone and frigid climate, and the annual rainfall is about 650 millimeters. The best season to view Danniang sand dunes was winter and spring. At this time, the water flow of the Yarlung Zangbo River slowed down, the riverbed was exposed, and the wind was strong, making the sand dunes more obvious.

Danniang sand dunes were formed in the winter and spring season (October to March of the following year). The climate was dry and windy. The area where the strong wind passed by had little vegetation. In addition, it passed through the river surface, so it was less blocked, forming a vortex ascending airflow. These airflows carried the sand on the sandbars and river banks, which were blocked by the mountainous terrain beside the river. The wind speed slowed down, and the sand piled up on the hillside. After a long time, it formed the Danniang sand dune.

The sand dune belt on the east coast of Hulun Lake was mainly formed by the sand at the bottom of the lake that was exposed to the surface when the lake water rose and retreated seasonally or shrank in large areas.

It could be inferred that the dominant wind direction of Danniang Dune was the southeast wind. According to the descriptions in documents 2 and 3, Danniang Sand Dune was located at the foothills of the north bank of the Yarlung Zangbo River in Milin County, Xizang, and the water level of the Yarlung Zangbo River varied greatly during the seasons. According to the descriptions in document 2 and document 3, there was less rainfall in winter and spring, the river level was low, and the beach and sandbar were exposed, providing sand for the formation of sand dunes. According to the descriptions in documents 2 and 4, the valley where the sand dunes were located had floodplains and sandbars. The valley was wide and curved, and the flow of water was slow. According to the description in document 4, the sand dune was located downwind of the sand source. Based on this information, it could be inferred that the dominant wind direction of Danniang Dune was the southeast wind.

Danniang sand dunes were formed by the accumulation of wind power. Every winter and spring, the climate in this area was dry, and the wind was strong. In addition, the vegetation was thin, so the wind was less blocked by the river surface, forming a vortex updraft. These air currents carried sand grains from the sandbars and floodplains, which were blocked by the mountainous terrain by the river. The wind speed slowed down, and the sand grains piled up on the hillside, forming Danniang sand dunes over time.

Six Songs of Dune was a series of novels by American science fiction writer Frank Herbert. There were six novels in the series. However, the search results provided did not provide a txt-download resource or information on reading the full text online. Therefore, it was impossible to provide a specific answer to the TMTs of the Six Songs of Dune.

The main cast of Dune 2 included Timothy Chalamet and Zandaya.

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