@article{chen_warm_2021,
	title = {Warm season temperature in the {Qinling} {Mountains} (north-central {China}) since 1740 {CE} recorded by tree-ring maximum latewood density of {Shensi} fir},
	issn = {0930-7575},
	doi = {10.1007/s00382-021-05827-4},
	abstract = {Land-surface temperature changes lead to thermal contrasts between the land and the sea and have significant water cycle impacts particularly within global monsoon regions. Whilst such influence may dominate in the East Asian summer monsoon region, the long-term warm-season temperature dynamics in monsoonal China have not been effectively explored. Here, an annually resolved maximum latewood density (MXD) record from annual tree rings of Shensi fir (A. chensiensis) in the Qinling Mountains (north-central China) provide an East Asian summer monsoon-region relevant 270-year long March-September temperature reconstruction. Our MXD-based temperature reconstruction shows good agreement with phases of observed warming in the 1920s-1950s and 1990s-2000s, a more recent warming hiatus and earlier volcanic-induced cooling phases. Our temperature reconstruction is also significantly correlated with sea surface temperatures in the North Atlantic Ocean and reveals that there is an unstable influence of the Atlantic Multidecadal Oscillation (AMO) on warm season temperature variability in north-central China. Our warm season temperature reconstruction is sensitive to summer monsoonal season moisture variations in north-central China and provides a multi century perspective on the region's climate which is useful to improving the understanding of monsoonal East Asian climate change and anticipated future extreme drought events in northern China.},
	language = {English},
	journal = {Climate Dynamics},
	author = {Chen, Feng and Gagen, Mary H. and Zhang, Heli and Chen, Youping and Fan, Ziang and Chen, Fahu},
	month = jun,
	year = {2021},
	note = {Place: New York
Publisher: Springer
WOS:000657440400002},
	keywords = {Abies chensiensis, China, Qinling mountains, maximum density, summer temperature, tree rings, volcanic forcing},
}

{"_id":"8tN8R76DbNqwxhQjP","bibbaseid":"chen-gagen-zhang-chen-fan-chen-warmseasontemperatureintheqinlingmountainsnorthcentralchinasince1740cerecordedbytreeringmaximumlatewooddensityofshensifir-2021","author_short":["Chen, F.","Gagen, M. H.","Zhang, H.","Chen, Y.","Fan, Z.","Chen, F."],"bibdata":{"bibtype":"article","type":"article","title":"Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir","issn":"0930-7575","doi":"10.1007/s00382-021-05827-4","abstract":"Land-surface temperature changes lead to thermal contrasts between the land and the sea and have significant water cycle impacts particularly within global monsoon regions. Whilst such influence may dominate in the East Asian summer monsoon region, the long-term warm-season temperature dynamics in monsoonal China have not been effectively explored. Here, an annually resolved maximum latewood density (MXD) record from annual tree rings of Shensi fir (A. chensiensis) in the Qinling Mountains (north-central China) provide an East Asian summer monsoon-region relevant 270-year long March-September temperature reconstruction. Our MXD-based temperature reconstruction shows good agreement with phases of observed warming in the 1920s-1950s and 1990s-2000s, a more recent warming hiatus and earlier volcanic-induced cooling phases. Our temperature reconstruction is also significantly correlated with sea surface temperatures in the North Atlantic Ocean and reveals that there is an unstable influence of the Atlantic Multidecadal Oscillation (AMO) on warm season temperature variability in north-central China. Our warm season temperature reconstruction is sensitive to summer monsoonal season moisture variations in north-central China and provides a multi century perspective on the region's climate which is useful to improving the understanding of monsoonal East Asian climate change and anticipated future extreme drought events in northern China.","language":"English","journal":"Climate Dynamics","author":[{"propositions":[],"lastnames":["Chen"],"firstnames":["Feng"],"suffixes":[]},{"propositions":[],"lastnames":["Gagen"],"firstnames":["Mary","H."],"suffixes":[]},{"propositions":[],"lastnames":["Zhang"],"firstnames":["Heli"],"suffixes":[]},{"propositions":[],"lastnames":["Chen"],"firstnames":["Youping"],"suffixes":[]},{"propositions":[],"lastnames":["Fan"],"firstnames":["Ziang"],"suffixes":[]},{"propositions":[],"lastnames":["Chen"],"firstnames":["Fahu"],"suffixes":[]}],"month":"June","year":"2021","note":"Place: New York Publisher: Springer WOS:000657440400002","keywords":"Abies chensiensis, China, Qinling mountains, maximum density, summer temperature, tree rings, volcanic forcing","bibtex":"@article{chen_warm_2021,\n\ttitle = {Warm season temperature in the {Qinling} {Mountains} (north-central {China}) since 1740 {CE} recorded by tree-ring maximum latewood density of {Shensi} fir},\n\tissn = {0930-7575},\n\tdoi = {10.1007/s00382-021-05827-4},\n\tabstract = {Land-surface temperature changes lead to thermal contrasts between the land and the sea and have significant water cycle impacts particularly within global monsoon regions. Whilst such influence may dominate in the East Asian summer monsoon region, the long-term warm-season temperature dynamics in monsoonal China have not been effectively explored. Here, an annually resolved maximum latewood density (MXD) record from annual tree rings of Shensi fir (A. chensiensis) in the Qinling Mountains (north-central China) provide an East Asian summer monsoon-region relevant 270-year long March-September temperature reconstruction. Our MXD-based temperature reconstruction shows good agreement with phases of observed warming in the 1920s-1950s and 1990s-2000s, a more recent warming hiatus and earlier volcanic-induced cooling phases. Our temperature reconstruction is also significantly correlated with sea surface temperatures in the North Atlantic Ocean and reveals that there is an unstable influence of the Atlantic Multidecadal Oscillation (AMO) on warm season temperature variability in north-central China. Our warm season temperature reconstruction is sensitive to summer monsoonal season moisture variations in north-central China and provides a multi century perspective on the region's climate which is useful to improving the understanding of monsoonal East Asian climate change and anticipated future extreme drought events in northern China.},\n\tlanguage = {English},\n\tjournal = {Climate Dynamics},\n\tauthor = {Chen, Feng and Gagen, Mary H. and Zhang, Heli and Chen, Youping and Fan, Ziang and Chen, Fahu},\n\tmonth = jun,\n\tyear = {2021},\n\tnote = {Place: New York\nPublisher: Springer\nWOS:000657440400002},\n\tkeywords = {Abies chensiensis, China, Qinling mountains, maximum density, summer temperature, tree rings, volcanic forcing},\n}\n\n","author_short":["Chen, F.","Gagen, M. H.","Zhang, H.","Chen, Y.","Fan, Z.","Chen, F."],"key":"chen_warm_2021","id":"chen_warm_2021","bibbaseid":"chen-gagen-zhang-chen-fan-chen-warmseasontemperatureintheqinlingmountainsnorthcentralchinasince1740cerecordedbytreeringmaximumlatewooddensityofshensifir-2021","role":"author","urls":{},"keyword":["Abies chensiensis","China","Qinling mountains","maximum density","summer temperature","tree rings","volcanic forcing"],"metadata":{"authorlinks":{}}},"bibtype":"article","biburl":"https://api.zotero.org/groups/22111/items?key=H9ArjTsLa0qzhllgMkIKGCHE&format=bibtex&limit=100","dataSources":["ugPKbmv5mxMoAW7Hh"],"keywords":["abies chensiensis","china","qinling mountains","maximum density","summer temperature","tree rings","volcanic forcing"],"search_terms":["warm","season","temperature","qinling","mountains","north","central","china","1740","recorded","tree","ring","maximum","latewood","density","shensi","fir","chen","gagen","zhang","chen","fan","chen"],"title":"Warm season temperature in the Qinling Mountains (north-central China) since 1740 CE recorded by tree-ring maximum latewood density of Shensi fir","year":2021}