Reflection of climate changes in the structure and morphodynamics of talus slopes (the Tatra Mountains, Poland)
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- 作者：Bogdan Gądeka ; b ; bogdan.gadek@us.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Mariusz Grabieca ; b ; mariusz.grabiec@us.edu.pl" class="auth_mail" title="E-mail the corresponding author ; Stanisław Kędziac ; kedzia@zg.pan.krakow.pl" class="auth_mail" title="E-mail the corresponding author ; Zofia Rączkowskac ; raczk@zg.pan.krakow.pl" class="auth_mail" title="E-mail the corresponding author
- 关键词：Tatra Mountains ; Talus slopes ; Climate changes ; GPR surveys
- 刊名：Geomorphology
- 出版年：2016
- 出版时间：15 June 2016
- 年：2016
- 卷：263
- 期：Complete
- 页码：39-49
- 全文大小：2908 K
文摘
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In the Tatras maximum thickness of the talus slopes in view of the GPR soundings ranges from 20 to 35 meters.
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In the last 200 years, the talus slopes of the Tatras were most active at the end of the LIA, in the 1930s and 1940s, and in the 1970s.
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The daily total of rainfall is much less important than the intensity of rainfall.
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It can be assumed that with an intensity of 1,0–1,5 mm/min, debris flows may occur about 15 min after precipitation.