Matches in SemOpenAlex for { <https://semopenalex.org/work/W2960986883> ?p ?o ?g. }
- W2960986883 endingPage "423" @default.
- W2960986883 startingPage "405" @default.
- W2960986883 abstract "The Ming-Qing transition (MQT) was a watershed in Chinese history. Events in three critical regions—North China Plain (NCP), southern Inner Mongolia (IM), and the Liaodong Peninsula (LP)—paved the way for political change in the latter years of the Ming dynasty. These developments occured in part as a response to climate change. Climate in these regions is controlled by topography and monsoon intensity (summer and winter). Here, we compare historical records with multi-proxy temperature and moisture reconstructions to understand the linkage between climate, the rise of the Manchu, and the collapse of the Ming dynasty and Mongolian steppe. In the last decades of the Ming, both the Ming and Mongolian steppe suffered from the most severe drought and winter cold of the past 500 years. Under the stress of this event, the political and economic systems of the Ming dynasty collapsed, although drought and cooling in the LP were not so intense, due to a maritime effect on climate. This allowed for enhanced precipitation by typhoons, and sustained agricultural development. During this period, the Later Jin (then Qing) seized an opportunity and occupied the LP. Simultaneously, a Manchu-Mongolian alliance formed. They defeated Lindan Khan and conquered North Korea, which removed the military threat from the east. This alleviated the economic pressure imposed by war, and rapid population expansion ensued. Finally, a new dynasty was established in the Central Plains." @default.
- W2960986883 created "2019-07-23" @default.
- W2960986883 creator A5006855039 @default.
- W2960986883 creator A5049533683 @default.
- W2960986883 creator A5050031153 @default.
- W2960986883 creator A5083258083 @default.
- W2960986883 creator A5087104366 @default.
- W2960986883 date "2019-06-06" @default.
- W2960986883 modified "2023-10-10" @default.
- W2960986883 title "Climatic change and the rise of the Manchu from Northeast China during AD 1600–1650" @default.
- W2960986883 cites W1573381451 @default.
- W2960986883 cites W1968832695 @default.
- W2960986883 cites W1969528736 @default.
- W2960986883 cites W1981733710 @default.
- W2960986883 cites W1984434762 @default.
- W2960986883 cites W1986787565 @default.
- W2960986883 cites W1993341938 @default.
- W2960986883 cites W1999710473 @default.
- W2960986883 cites W2009370431 @default.
- W2960986883 cites W2018178007 @default.
- W2960986883 cites W2020023072 @default.
- W2960986883 cites W2029530847 @default.
- W2960986883 cites W2029780198 @default.
- W2960986883 cites W2034795620 @default.
- W2960986883 cites W2040945899 @default.
- W2960986883 cites W2048101491 @default.
- W2960986883 cites W2048809535 @default.
- W2960986883 cites W2071179593 @default.
- W2960986883 cites W2074676184 @default.
- W2960986883 cites W2081276502 @default.
- W2960986883 cites W2089443235 @default.
- W2960986883 cites W2092446626 @default.
- W2960986883 cites W2104995723 @default.
- W2960986883 cites W2110238074 @default.
- W2960986883 cites W2122046874 @default.
- W2960986883 cites W2140259111 @default.
- W2960986883 cites W2148785784 @default.
- W2960986883 cites W2165391243 @default.
- W2960986883 cites W2171125351 @default.
- W2960986883 cites W2336953138 @default.
- W2960986883 cites W2529338474 @default.
- W2960986883 cites W2790768084 @default.
- W2960986883 cites W2802937228 @default.
- W2960986883 cites W2905015599 @default.
- W2960986883 cites W3194224608 @default.
- W2960986883 cites W346699550 @default.
- W2960986883 cites W4213421075 @default.
- W2960986883 cites W4251441456 @default.
- W2960986883 doi "https://doi.org/10.1007/s10584-019-02471-0" @default.
- W2960986883 hasPublicationYear "2019" @default.
- W2960986883 type Work @default.
- W2960986883 sameAs 2960986883 @default.
- W2960986883 citedByCount "10" @default.
- W2960986883 countsByYear W29609868832021 @default.
- W2960986883 countsByYear W29609868832022 @default.
- W2960986883 countsByYear W29609868832023 @default.
- W2960986883 crossrefType "journal-article" @default.
- W2960986883 hasAuthorship W2960986883A5006855039 @default.
- W2960986883 hasAuthorship W2960986883A5049533683 @default.
- W2960986883 hasAuthorship W2960986883A5050031153 @default.
- W2960986883 hasAuthorship W2960986883A5083258083 @default.
- W2960986883 hasAuthorship W2960986883A5087104366 @default.
- W2960986883 hasBestOaLocation W29609868832 @default.
- W2960986883 hasConcept C100970517 @default.
- W2960986883 hasConcept C105895522 @default.
- W2960986883 hasConcept C111368507 @default.
- W2960986883 hasConcept C121332964 @default.
- W2960986883 hasConcept C123588078 @default.
- W2960986883 hasConcept C127313418 @default.
- W2960986883 hasConcept C132651083 @default.
- W2960986883 hasConcept C136996986 @default.
- W2960986883 hasConcept C144024400 @default.
- W2960986883 hasConcept C149923435 @default.
- W2960986883 hasConcept C166957645 @default.
- W2960986883 hasConcept C191935318 @default.
- W2960986883 hasConcept C195244886 @default.
- W2960986883 hasConcept C205649164 @default.
- W2960986883 hasConcept C24890656 @default.
- W2960986883 hasConcept C2778431023 @default.
- W2960986883 hasConcept C2778589402 @default.
- W2960986883 hasConcept C2781291010 @default.
- W2960986883 hasConcept C2908647359 @default.
- W2960986883 hasConcept C49119912 @default.
- W2960986883 hasConcept C49204034 @default.
- W2960986883 hasConcept C76775654 @default.
- W2960986883 hasConcept C95457728 @default.
- W2960986883 hasConceptScore W2960986883C100970517 @default.
- W2960986883 hasConceptScore W2960986883C105895522 @default.
- W2960986883 hasConceptScore W2960986883C111368507 @default.
- W2960986883 hasConceptScore W2960986883C121332964 @default.
- W2960986883 hasConceptScore W2960986883C123588078 @default.
- W2960986883 hasConceptScore W2960986883C127313418 @default.
- W2960986883 hasConceptScore W2960986883C132651083 @default.
- W2960986883 hasConceptScore W2960986883C136996986 @default.
- W2960986883 hasConceptScore W2960986883C144024400 @default.
- W2960986883 hasConceptScore W2960986883C149923435 @default.
- W2960986883 hasConceptScore W2960986883C166957645 @default.
- W2960986883 hasConceptScore W2960986883C191935318 @default.