According to the textual research into the historical documents dominated by archives yearly, as well as the verification with several other kinds of data, the later or earlier starting time of the rainy seasons in Yunnan during 1711-1982 has been reconstructed. The analysis indicates that there are obvious fluctuations in the starting date of the rainy seasons in Yunnan in a year or years, and long fluctuation on the decadal scale. The rainy season comes earlier in the early 18th century, later in the 19th century and earlier again in the 20th century. This reflects to a certain degree the gradual change of the summer monsoon in Yunnan. There exists an obvious quasi-3 years cycle, which is related to El-Nino's quasi-3 years cycle, and a 11...
The East Asian summer monsoon (EASM) exhibits considerable decadal variations since the late 20th ce...
Phenological data obtained from historical documents constitute highly important ecological evidence...
Abstract. The precipitation variations of Longxi area, north-east margin of the Tibetan Plateau sinc...
The Yu-Xue-Fen-Cun (YXFC) is one of the government archives of the Qing Dynasty (1644-1911) in China...
Based on reconstructions of precipitation events from the rain and snowfall archives of the Qing Dyn...
Knowledge of late Holocene precipitation variability in the northwestern Yunnan Province is importan...
A millennium-long tree-ring-width chronology from the middle Qilian Mountains in northwestern China ...
The East Asian summer monsoon (EASM) plays a crucial role for ecosystems and societies in East Asia ...
Three tree-ring rainfall reconstructions from China and Korea are used in this paper to investigate ...
The rainy season is an important climate feature over Eastern China where anomaly in either its timi...
Based upon the effect of land-sea interaction on the paleomonsoon variation and the time series of c...
The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeocli...
The precipitation variations of Longxi area, northeast margin of the Tibetan Plateau since AD 960 ar...
Our understanding on the spatial-temporal patterns of climatic variability over the last few millenn...
Monthly precipitation datasets collected at 160 stations in China as well as the monthly winds and h...
The East Asian summer monsoon (EASM) exhibits considerable decadal variations since the late 20th ce...
Phenological data obtained from historical documents constitute highly important ecological evidence...
Abstract. The precipitation variations of Longxi area, north-east margin of the Tibetan Plateau sinc...
The Yu-Xue-Fen-Cun (YXFC) is one of the government archives of the Qing Dynasty (1644-1911) in China...
Based on reconstructions of precipitation events from the rain and snowfall archives of the Qing Dyn...
Knowledge of late Holocene precipitation variability in the northwestern Yunnan Province is importan...
A millennium-long tree-ring-width chronology from the middle Qilian Mountains in northwestern China ...
The East Asian summer monsoon (EASM) plays a crucial role for ecosystems and societies in East Asia ...
Three tree-ring rainfall reconstructions from China and Korea are used in this paper to investigate ...
The rainy season is an important climate feature over Eastern China where anomaly in either its timi...
Based upon the effect of land-sea interaction on the paleomonsoon variation and the time series of c...
The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeocli...
The precipitation variations of Longxi area, northeast margin of the Tibetan Plateau since AD 960 ar...
Our understanding on the spatial-temporal patterns of climatic variability over the last few millenn...
Monthly precipitation datasets collected at 160 stations in China as well as the monthly winds and h...
The East Asian summer monsoon (EASM) exhibits considerable decadal variations since the late 20th ce...
Phenological data obtained from historical documents constitute highly important ecological evidence...
Abstract. The precipitation variations of Longxi area, north-east margin of the Tibetan Plateau sinc...