Correlations between the reconstructed EASM and precedent winter (from December to February) global SSTs for the period of 1871–2014.
Dai Chen
Feifei Zhou
Zhipeng Dong
A’ying Zeng
Tinghai Ou
Keyan Fang
10.1371/journal.pone.0234421.g005
https://plos.figshare.com/articles/figure/Correlations_between_the_reconstructed_EASM_and_precedent_winter_from_December_to_February_global_SSTs_for_the_period_of_1871_2014_/12454967
<p>Correlations not significant at the 95% level have been masked out. <i>The maps were produced with <a href="http://cola.gmu.edu/grads/" target="_blank">GrADS v2.2.0</a> software (<a href="http://cola.gmu.edu/grads/" target="_blank">http://cola.gmu.edu/grads/</a>) in KNMI Climate Explorer</i>.</p>
2020-06-09 17:28:50
Pinus massoniana trees
middle Yangtze River basin
core EASM areas
El Ni ño Oscillation
ENSO variability coheres
anthropogenic impact
ENSO variability
tree-ring cellulose δ 18 O records
EASM reconstruction
monsoon intensity
200- year
aerosol emissions
decadal variations
EASM-ENSO connections
tree-ring δ 18 O
δ 18 O chronology accounts
core regions
summer monsoon
EASM-ENSO relationship
East Asia summer monsoon