The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance
A modern research a:roach and working techniques in hitherto unexamined areas, produced the following results: 1). The tongues of decakilometre long Karakorum glaciers belong to temperate ice-streams with an annual meltwater output. The short Aghil glaciers on the contrary are continental, arid and...
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ftchinacadscimhe:oai:ir.imde.ac.cn:131551/6131 2023-05-15T16:40:51+02:00 The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance Matthias Kuhle 2005-03 http://ir.imde.ac.cn/handle/131551/6131 英语 eng JOURNAL OF MOUNTAIN SCIENCE Matthias Kuhle. The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance[J]. JOURNAL OF MOUNTAIN SCIENCE,2005,2(1):5–22. http://ir.imde.ac.cn/handle/131551/6131 4 Karakorum Tibet Ice Age Glaciation Paleoclimate Ice Age Theory High Mountain Geomorphology 期刊论文 2005 ftchinacadscimhe 2022-12-19T18:18:14Z A modern research a:roach and working techniques in hitherto unexamined areas, produced the following results: 1). The tongues of decakilometre long Karakorum glaciers belong to temperate ice-streams with an annual meltwater output. The short Aghil glaciers on the contrary are continental, arid and cold. 2). The present-day oscillations of the Karakorum glaciers are related to their own mass, and are contrary to and independent of the actual climate. Only the short glaciers, with steep tongue fronts, show a present-day positive balance. 3). 14C- dated Late Glacial moraines indicate a 400–800 m thick valley glacier at the former confluence point of the K2-, Sarpo Laggo- and Skamri glaciers. 4). From the evidence of transfluence passes with roches moutonnées, striae and the limits of glacial polishing, as well as moraines and erratics, a High Glacial at least 1200 m thick ice-stream network between the Karakorums and the Kuen Lun north slopes was reconstructed. The Shaksgam and Yarkand valleys were occupied by glaciers coming from west Tibet. The lowest-lying moraines are to be found in the foreland down to 2000 m, indicating a depression of the High Glacial (LGM) snowline (ELA) by 1300 m. 5). The a:roximately 10,000 measurements of the radiation balance at up to heights of 5500 m on K2 indicate that with incoming energy near the solar constant the reflection from snow- covered ice is up to 70% greater than from rock and rock waste surfaces. 6). These results confirm for the very dry western margins of Tibet an almost complete ice sheet cover in an area with subtropical energy balance, conforming with the Ice Age hypothesis of the author which is based upon the presence of a 2.4 million km2 Tibetan inland ice sheet. This inland ice developed for the first time when Tibet was uplifted over the snowline during the early Pleistocene. As the measured subtropical radiation balance shows, it was able to trigger the Quaternary Ice Ages. Report Ice Sheet IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) Ela ENVELOPE(9.642,9.642,63.170,63.170) |
institution |
Open Polar |
collection |
IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) |
op_collection_id |
ftchinacadscimhe |
language |
English |
topic |
Karakorum Tibet Ice Age Glaciation Paleoclimate Ice Age Theory High Mountain Geomorphology |
spellingShingle |
Karakorum Tibet Ice Age Glaciation Paleoclimate Ice Age Theory High Mountain Geomorphology Matthias Kuhle The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
topic_facet |
Karakorum Tibet Ice Age Glaciation Paleoclimate Ice Age Theory High Mountain Geomorphology |
description |
A modern research a:roach and working techniques in hitherto unexamined areas, produced the following results: 1). The tongues of decakilometre long Karakorum glaciers belong to temperate ice-streams with an annual meltwater output. The short Aghil glaciers on the contrary are continental, arid and cold. 2). The present-day oscillations of the Karakorum glaciers are related to their own mass, and are contrary to and independent of the actual climate. Only the short glaciers, with steep tongue fronts, show a present-day positive balance. 3). 14C- dated Late Glacial moraines indicate a 400–800 m thick valley glacier at the former confluence point of the K2-, Sarpo Laggo- and Skamri glaciers. 4). From the evidence of transfluence passes with roches moutonnées, striae and the limits of glacial polishing, as well as moraines and erratics, a High Glacial at least 1200 m thick ice-stream network between the Karakorums and the Kuen Lun north slopes was reconstructed. The Shaksgam and Yarkand valleys were occupied by glaciers coming from west Tibet. The lowest-lying moraines are to be found in the foreland down to 2000 m, indicating a depression of the High Glacial (LGM) snowline (ELA) by 1300 m. 5). The a:roximately 10,000 measurements of the radiation balance at up to heights of 5500 m on K2 indicate that with incoming energy near the solar constant the reflection from snow- covered ice is up to 70% greater than from rock and rock waste surfaces. 6). These results confirm for the very dry western margins of Tibet an almost complete ice sheet cover in an area with subtropical energy balance, conforming with the Ice Age hypothesis of the author which is based upon the presence of a 2.4 million km2 Tibetan inland ice sheet. This inland ice developed for the first time when Tibet was uplifted over the snowline during the early Pleistocene. As the measured subtropical radiation balance shows, it was able to trigger the Quaternary Ice Ages. |
format |
Report |
author |
Matthias Kuhle |
author_facet |
Matthias Kuhle |
author_sort |
Matthias Kuhle |
title |
The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
title_short |
The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
title_full |
The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
title_fullStr |
The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
title_full_unstemmed |
The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance |
title_sort |
maximum ice age glaciation between the karakorum main ridge (k_2) and the tarim basin and its influence on global energy balance |
publishDate |
2005 |
url |
http://ir.imde.ac.cn/handle/131551/6131 |
long_lat |
ENVELOPE(9.642,9.642,63.170,63.170) |
geographic |
Ela |
geographic_facet |
Ela |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
JOURNAL OF MOUNTAIN SCIENCE Matthias Kuhle. The maximum ice age glaciation between the karakorum main ridge (K_2) and the tarim basin and its influence on global energy balance[J]. JOURNAL OF MOUNTAIN SCIENCE,2005,2(1):5–22. http://ir.imde.ac.cn/handle/131551/6131 |
op_rights |
4 |
_version_ |
1766031278385135616 |