A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon precipitation changes in the middle Yangtze Valley
Quantitative reconstructions of the depth to water table (DWT) of ombrotrophic (rain-fed)
peatlands are important for understanding the palaeohydrological responses of peatlands to …
peatlands are important for understanding the palaeohydrological responses of peatlands to …
A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon precipitation changes in the middle Yangtze Valley
H Liu, Y Gu, X Huang, Z Yu, S Xie… - Quaternary Science …, 2019 - ui.adsabs.harvard.edu
Quantitative reconstructions of the depth to water table (DWT) of ombrotrophic (rain-fed)
peatlands are important for understanding the palaeohydrological responses of peatlands to …
peatlands are important for understanding the palaeohydrological responses of peatlands to …
[引用][C] A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon precipitation changes in the middle Yangtze Valley
H Liu, Y Gu, X Huang, Z Yu, S Xie… - Quaternary Science …, 2019 - cir.nii.ac.jp
A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon
precipitation changes in the middle Yangtze Valley | CiNii Research CiNii 国立情報学研究所 …
precipitation changes in the middle Yangtze Valley | CiNii Research CiNii 国立情報学研究所 …