Mingyuan Du

Dr. Mingyuan Du

orcid

Research Focus & Metrics

Academic Career Length

38Years (1989-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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22 May 2006 in Global Change Biology
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Journal Article
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TKTomomichi Kato
Tomomichi Kato
YTYanhong Tang
Yanhong Tang
SGSong Gu
Song Gu
MHMitsuru Hirota
Mitsuru Hirota
MDMingyuan Du
Mingyuan Du
XZXinquan Zhao
Xinquan Zhao

20 July 2017 in Global Change Biology
Verified
Journal Article
Open access
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YYYitong Yao
Yitong Yao
XWXuhui Wang
Xuhui Wang
YLYue Li
Yue Li
Tao WangTao Wang
Tao Wang
MSMiaogen Shen
Miaogen Shen
SPShilong Piao
Shilong Piao
The uncertainties of China's gross primary productivity (GPP) estimates by global data‐oriented products and ecosystem models justify a development of high‐resolution data‐oriented GPP dataset over China. We applied a machine learning algorithm developing a new GPP dataset for China with 0.1° spatial resolution and monthly temporal frequency based on eddy flux measurements from 40 sites in China and surrounding countries, most of which have not been explored in previous global GPP datasets. According to our estimates, mean annual GPP over China is 6.62 ± 0.23 PgC/year during 1982–2015 with a clear gradient from southeast to northwest. The trend of GPP estimated by this study (0.020 ± 0.002 PgC/year2 from 1982 to 2015) is almost two times of that estimated by the previous global dataset. The GPP increment is widely spread with 60% area showing significant increasing trend (p < .05), except for Inner Mongolia. Most ecosystem models overestimated the GPP magnitudes but underestimated the temporal trend of GPP. The monsoon affected eastern China, in particular the area surrounding Qinling Mountain, seems having larger contribution to interannual variability (IAV) of China's GPP than the semiarid northwestern China and Tibetan Plateau. At country scale, temperature is the dominant climatic driver for IAV of GPP. The area where IAV of GPP dominated by temperature is about 42%, while precipitation and solar radiation dominate 31% and 27% respectively over semiarid area and cold‐wet area. Such spatial pattern was generally consistent with global GPP dataset, except over the Tibetan Plateau and northeastern forests, but not captured by most ecosystem models, highlighting future research needs to improve the modeling of ecosystem response to climate variations.

14 April 2010 in Global Change Biology
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Journal Article
Closed access
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CLCaiyun Luo
Caiyun Luo
GXGuangping Xu
Guangping Xu
ZCZengguo Chao
Zengguo Chao
SWShiping Wang
Shiping Wang
XLXingwu Lin
Xingwu Lin
BKBruce Kimball
Bruce Kimball

1 July 2004 in Agricultural and Forest Meteorology
Verified
Journal Article
Closed access
TKTomomichi Kato
Tomomichi Kato
YTYanhong Tang
Yanhong Tang
SGSong Gu
Song Gu
XCXiaoyong Cui
Xiaoyong Cui
MHMitsuru Hirota
Mitsuru Hirota
TOTakehisa Oikawa
Takehisa Oikawa


1 July 2006 in Global and Planetary Change
Verified
Journal Article
Closed access
MMM. Mikami
M. Mikami
GSG.Y. Shi
G.Y. Shi
IUI. Uno
I. Uno
SYS. Yabuki
S. Yabuki
YIY. Iwasaka
Y. Iwasaka
JSJ. Suzuki
J. Suzuki