Response of Tibetan Plateau lakes to climate change: Trends, patterns, and mechanisms
This article provides a comprehensive review of the global monsoon that encompasses
findings from studies of both modern monsoons and paleomonsoons. We introduce a …
findings from studies of both modern monsoons and paleomonsoons. We introduce a …
A data-model comparison pinpoints Holocene spatiotemporal pattern of East Asian summer monsoon
Conflicting reconstructions of Holocene variability of the East Asian summer monsoon
(EASM) from speleothem versus other types of proxy records have yielded widely divergent …
(EASM) from speleothem versus other types of proxy records have yielded widely divergent …
Holocene vegetation and climate dynamics of NE China based on the pollen record from Sihailongwan Maar Lake
M Stebich, K Rehfeld, F Schluetz, PE Tarasov… - Quaternary Science …, 2015 - Elsevier
High-resolution palynological analysis on annually laminated sediments of Sihailongwan
Maar Lake (SHL) provides new insights into the Holocene vegetation and climate dynamics …
Maar Lake (SHL) provides new insights into the Holocene vegetation and climate dynamics …
Role of seasonal transitions and westerly jets in East Asian paleoclimate
The summer rainfall climate of East Asia underwent large and abrupt changes during past
climates, in response to precessional forcing, glacial–interglacial cycles as well as abrupt …
climates, in response to precessional forcing, glacial–interglacial cycles as well as abrupt …
Climate change trends and impacts on vegetation greening over the Tibetan Plateau
Abstract The Tibetan Plateau (TP) is an ecologically fragile region that is sensitive to climate
change. In the context of global climate change, the climate change trends of the TP and the …
change. In the context of global climate change, the climate change trends of the TP and the …
Holocene moisture and East Asian summer monsoon evolution in the northeastern Tibetan Plateau recorded by Lake Qinghai and its environs: A review of conflicting …
Climatic and environmental changes in the northeastern Tibetan Plateau are controlled by
the Asian summer monsoon (ASM) and the westerlies, two key circulation components of the …
the Asian summer monsoon (ASM) and the westerlies, two key circulation components of the …