Subtropical mountain- and highland-glaciation as ice age triggers and the waning of the glacial periods in the pleistocene
Datos Bibliográficos
| ID | 11984809 |
|---|---|
| Autores | Matthias Kuhle (University of Göttingen, autor de correspondencia), Kuhle Matthias |
| Año | 1987 |
| Volumen | 14 |
| Número | 4 |
| Páginas | 393-421 |
| Fecha de publicación | 1987-06-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | GeoJournal (JOURNAL) |
| Identificadores de la revista | ISSN: 0343-2521 • E-ISSN: 1572-9893 |
| Editorial | Springer Science+Business Media (PUBLISHER • DE) |
| DOI | 10.1007/bf02602717 |
| OpenAlex | W2038519951 |
| Idioma | EN |
| Citas recibidas | 32 |
| Referencias citadas | 2 |
Deglaciation · Earth science · Geography · Glacial period · Glacier · Ice age · Physical geography · Pleistocene · Subtropics · Environmental and Cultural Studies in Latin America and Beyond · Geology and Paleoclimatology Research · Ecology · Geology · Paleontology
Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the Holocene and the last glaciation
Relative dating of Quaternary moraines, Rongbuk valley, Mount Everest, Tibet
Quaternary Glaciations in the Río Mendoza Valley, Argentine Andes
Controversy Regarding the Existence of a Large Ice Sheet on the Qinghai-Xizang (Tibetan) Plateau During the Quaternary Period
The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation
New Findings concerning the Ice Age (Last Glacial Maximum) Glacier Cover of the East-Pamir, of the Nanga Parbat up to the Central Himalaya and of Tibet, as well as the Age of the Tibetan Inland Ice
The sequence of Quaternary glaciation in the Bayan Har Mountains
Late pleistocene, Late-glacial and Holocene glacier advances on the Tibetan Plateau
Evolution of the arid climate in High Asia since ∼1 Ma
Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia
On the ice age glaciation of the Tibetan highlands and its transformation into a 3-D model
On the geoecology of Southern Tibet
An outline of physical geography including Pleistocene glacial landforms of Eastern Tibet (provinces Sichuan and Qinghai)
Topography as a fundamental element of glacial systems
Geomorphological findings on the build-up of pleistocene glaciation in Southern Tibet and on the problem of inland ice
Quantificational reductionism as a risk in geography and cartography
Glacial isostatic uplift of Tibet as a consequence of a former ice sheet
On the problem of Quaternary glaciations, and the extent and patterns of Pleistocene ice cover in the Qinghai-Xizang (Tibet) Plateau
Quaternary glaciation of Puruogangri—the largest modern ice field in Tibet
Reconstruction of the 2.4 million km2 late Pleistocene ice sheet on the Tibetan Plateau and its impact on the global climate
Problematic ice sheets
Equilibrium-line altitudes of Late Quaternary glaciers in the Oshtorankuh Mountain, Iran
Glacial environments on the Tibetan Plateau and global cooling
Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet
Wisconsin/W rm glacial stage ice in the subtropical dunde ice cap, China
Ice marginal ramps
The maximum Ice Age (LGM) glaciation of the Central- and South Karakorum
The pleistocene glaciation of Tibet and the onset of ice ages ? An autocycle hypothesis
The probability of proof in geomorphology —an example of the application of information theory to a new kind of glacigenetic morphological type, the ice-marginal ramp (Bortensander)
Investigations on the Quaternary Glaciation in the Khumbu Himal (Nepal, East-Himalaya)
Present and Pleistocene glaciation on the north-western margin of Tibet between the Karakorum main ridge and the Tarim Basin, supporting the evidence of a Pleistocene inland glaciation in Tibet
Last Glacial snowlines in the Tibetan Plateau
| Obras citantes distintas | 32 |
|---|---|
| Citas por año | 0,84 |
| Intervalo de citas | 1988 - 2015 (28) |
| Velocidad de citación | historical |
| Altamente citado | No |
| Tipos de cita | Neutras: 28 |