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TZID:Europe/Berlin
TZUNTIL:20211031T010000Z
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DTSTART:20191027T030000
TZOFFSETFROM:+0200
TZOFFSETTO:+0100
RDATE:20201025T030000
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DTSTART:20190331T020000
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RDATE:20210328T020000
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UID:www.bayceer.uni-bayreuth.de-bayceer-t150117id
DTSTAMP:20260816T054256Z
DESCRIPTION:High mountain regions are among the geomorphologically most act
 ive areas on earth. They are highly sensitive to climate change and associ
 ated processes (e.g. glacier melt\, permafrost degradation)\, which in tur
 n is reflected in modified (partly boosted) and highly non-linear geomorph
 ic process dynamics. High-resolution earth surface and subsurface analyses
  and various dating options dramatically improved the reconstruction\, mon
 itoring and modelling of related processes in the recent past and enable q
 uantitative answers to multiple geomorphological questions.\nThis talk wil
 l highlight climate-change driven process dynamics in alpine geosystems - 
 and demonstrate the potential of selected techniques through some recent g
 eomorphological research from the Alps and the Himalayas. These include ro
 ckfall\, debris flow and landslide monitoring studies\, the reconstruction
  of giant rockslides\, as well as comparative analyses of short and long-t
 erm (Holocene) sediment dynamics in an inner-alpine sedimentary basin.
DTSTART;TZID=Europe/Berlin:20191128T120000
DTEND;TZID=Europe/Berlin:20191128T133000
SUMMARY:Dr. Joachim Götz\, Department of Geomorphology\, BayCEER\, Universi
 ty of Bayreuth (Homepage): Rates and Dates in Alpine geosystems - Monitori
 ng and reconstruction of geomorphologic processes
TRANSP:TRANSPARENT
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