Baolin Pan
Datos Biográficos
| ID | 4130662 |
|---|---|
| NOMBRE | Baolin Pan |
| NOMBRES | Baolin |
| APELLIDO | Pan |
| FIRMA | PAN B |
| AFILIACIONES | Capital Normal University |
| ORCID | 0000-0003-2550-315X |
| VERIFICADO | Sí |
| TOTAL DE OBRAS | 6 |
| TOTAL DE CITAS | 3 |
| TOTAL COMO AUTOR | 6 |
| TOTAL COMO EDITOR | 0 |
| PRIMER AÑO DE PUBLICACIÓN | 1991 |
| AÑO MÁS RECIENTE DE PUBLICACIÓN | 2020 |
| ÍNDICE H | 1 |
Glacial events during the last glacial termination in the Pagele valley, Qiongmu Gangri peak, southern Tibetan Plateau, and their links to oceanic and atmospheric circulation
During the last glacial termination, a warming trend was generally interrupted by rapid millennium-scale cold reversals, such as the Greenland (Isotope) Stadial 1 (GS-1) and GS-2a events. To understand how glaciers on the Tibetan Plateau (TP) responded to these rapid climate events, this study constrained the timing and extent of three glacial events during the late-glacial period. Specifically, using a cosmogenic 10 Be exposure dating method, we…
Optically stimulated luminescence dating of Holocene palaeoflood deposits in the middle reach of the Yongding River, China
Late-Holocene glacier advances and related climate conditions in the Hailuogou catchment, Gongga Shan, eastern Tibetan Plateau
We present simulations for the late-Holocene glacier advances in the Hailuogou catchment, Gongga Shan, in attempts to test the glacier sensitivity to climate changes and constrain the climate conditions that support these glacier advances. We use a coupled mass-balance and ice-flow model parameterized using empirical glaciological and climatological data to simulate the glacier extents by fitting modeled glaciers to corresponding glacial landform…
Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau
Responses of two branches of Glacier No. 1 to climate change from 1993 to 2005, Tianshan, China
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Environmental change during the Holocene in western China on a millennial timescale
Recent data on the evolution of the inland lakes, loess-palaeosol sequences, and glacier variations in western China are briefly reviewed. The lake history shows three distinct stages in the Holocene, i.e., low water levels before 7500 BP, a stage of expansion during the climatic optimum between 7500 and 3500 BP, and contraction after 3500 BP. Three stages (wooded grassland, mixed woodland, wooded grassland becoming steppe) also appear indicated …
Responses of two branches of Glacier No. 1 to climate change from 1993 to 2005, Tianshan, China
Vegetation and climate changes during three interglacial periods represented in the Luochuan loess-paleosol section, on the Chinese Loess Plateau
Late-Holocene glacier advances and related climate conditions in the Hailuogou catchment, Gongga Shan, eastern Tibetan Plateau
We present simulations for the late-Holocene glacier advances in the Hailuogou catchment, Gongga Shan, in attempts to test the glacier sensitivity to climate changes and constrain the climate conditions that support these glacier advances. We use a coupled mass-balance and ice-flow model parameterized using empirical glaciological and climatological data to simulate the glacier extents by fitting modeled glaciers to corresponding glacial landform…
Optically stimulated luminescence dating of Holocene palaeoflood deposits in the middle reach of the Yongding River, China
Glacial events during the last glacial termination in the Pagele valley, Qiongmu Gangri peak, southern Tibetan Plateau, and their links to oceanic and atmospheric circulation
During the last glacial termination, a warming trend was generally interrupted by rapid millennium-scale cold reversals, such as the Greenland (Isotope) Stadial 1 (GS-1) and GS-2a events. To understand how glaciers on the Tibetan Plateau (TP) responded to these rapid climate events, this study constrained the timing and extent of three glacial events during the late-glacial period. Specifically, using a cosmogenic 10 Be exposure dating method, we…
Geography (6 obras) · Geology and Paleoclimatology Research (6 obras) · Physical geography (6 obras) · Climatology (5 obras) · Geology (5 obras) · Climate change (4 obras) · Glacier (4 obras) · Archaeology (3 obras) · China (3 obras) · Cryospheric studies and observations (3 obras)