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glacier
The "old red sand" deposited in the period of 30-10 ka, the later Würm glacier substage (Q33), developed on the largest scale with the widest distribution.
      
The decreased net-accumulation is coincident with glacier retreat, which is associated with recent temperature increase in the region that intensified the ablation.
      
Under the background of global warming, such glacier variation trends will aggravate.
      
It is characterized by the earlier glacier broad in scale.
      
Under the precondition of continental snow and glacier cover existing over part of the Tibetan Plateau at the mid-Holocene, the authors examined the regional climate response to the Tibetan Plateau cooling.
      
The simulation results suggest that the snow and glacier environment over the Tibetan Plateau is an important factor for mid-Holocene climate change in the areas highly influenced by the Asian monsoon.
      
Significant achievements have been made by continuous investigation of glacier inventories, frozen ground observations, paleo-climate analyses of ice cores, process studies and the modeling of cryopsheric/atmospheric interactions.
      
Impacts of Yulong Mountain glacier on tourism in Lijiang
      
The glacier on the Yulong Mountain is one of the most important attractions in Lijiang, Yunnan, China.
      
This study estimates the effects of the glacier retreat of the Yulong Mountains on tourism there.
      
These data were used to analyze the proportion of the contribution of glacier to the tourism in Lijiang and estimate the impact of glacier on the regional tourism quantitatively.
      
According to the survey, it could be concluded that three quarters of the tourists to Lijiang were interested in the Yulong Mountain glacier, indicating that the glacier possesses notable appeal for sightseeing tourists.
      
They are products of large debris flows induced by glacier and enabled by the presence of large amount of glacial debris on the landscape.
      
It was a part of the glacier system of the Himalaya and has communicated across transfluence passes with the neighbouring ice stream networks toward the W and E.
      
The ice thickness of the valley glacier sections, the surface of which was situated above the snow-line, amounted to 1000-1450 m.
      
70 km in length (Dudh Koshi glacier), 67 km (Barun-Arun glacier) and 80 km (Arun glacier).
      
The tongue end of the Arun glacier has flowed down to c.
      
From the maximum past glacier extension up to the current glacier margins, 13 (altogether 14) glacier stages have been differentiated and in part 14C-dated.
      
They were four glacier stages of the late glacial period, three of the neoglacial period and six of the historical period.
      
The number of the glacier stages since the maximum glaciation approx.
      
 

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