کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8914864 | 1640748 | 2018 | 27 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Last Glacial Maximum and Lateglacial in the Polish High Tatra Mountains - Revised deglaciation chronology based on the 10Be exposure age dating
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
LGM ELAs reconstructed for the BiaÅa Woda and Sucha Woda/PaÅszczyca glaciers were located at 1460-1480â¯m a.s.l. During the Oldest Dryas stages, the ELA in the High Tatras rose from 1600 to 1650â¯m a.s.l. in the Rybi Potok Valley and from 1700 to 1800â¯m a.s.l. in the Roztoka/PiÄÄ Stawów Polskich Valley. The Younger Dryas ELA, depending on glacier's exposition, was located between 1950 and 2000 m a.s.l. Climate modelling results show that the LGM glaciers (maximum advance) could have advanced in the High Tatras when the mean annual temperature was lower than today by 11-12â¯Â°C and precipitation was reduced by 40-60%. During the Lateglacial stages the temperature decrease in the study area changed from 10â¯Â°C during the Oldest Dryas to 6â¯Â°C during the Younger Dryas and precipitation lowering decreased from â50% to â30% or even â10%, respectively compare to modern conditions.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary Science Reviews - Volume 187, 1 May 2018, Pages 130-156
Journal: Quaternary Science Reviews - Volume 187, 1 May 2018, Pages 130-156
نویسندگان
MichaÅ Makos, Vincent Rinterknecht, Régis Braucher, Anna ToÅoczko-Pasek,