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1. Chen, X. Y., and K.-K. Tung (2018), Global surface warming enhanced by weak Atlantic overturning circulation, Nature , 559, 387-391, doi:10.1038/s41586-018-0320.
2. Tung, K.-K., X. Y. Chen , J. S. Zhou, and K.-F. Li (2018), Interdecadal variabiltiy in pan-Pacific and global SST, revisited, Climate Dynamics , doi:10.1007/s00382-018-4240-1
3. Chen, X. Y., and K.-K. Tung (2018), Global mean surface temperature variability: space-time perspective from rotated EOFs, Climate Dynamics , 51, 1719-1732, doi:10.1007/s00382-017-3970-0.
4. Tung, K.-K., and X. Y. Chen (2018), Understanding the recent global surface warming slowdown: A Review, Climate , 6, doi:10.3390/cli6040082.
5. Wang, J. P., and X. Y. Chen (2018), Intercomparison of the Extended Reconstructed Sea Surface Temperature v4 and v3b Datasets, J. Ocean Univ. China , 17, 209-218 .
6. Chen, X. Y., X. B. Zhang, J. A. Church, C. S. Watson, M. A. King, D. Monselesan, B. Legresy, and C. Harig (2017), The increasing rate of global mean sea-level rise during 1993-2014, Nature Climate Change , 7, 492-495, doi:10.1038/nclimate3325.
7. Chen, X. Y., J. M.Wallace, and K.-K. Tung (2017), Pairwise-rotated EOFs of global SST, J. Climate , 30, 5473-5489, doi:10.1175/JCLI-D-16-0786.1.
8. Chen, X. Y., and K.-K. Tung (2016), Variations in ocean heat uptake during the surface warming hiatus, Nature Communications , doi:10.1038/ncomms12541.
9. Chen, X. Y., and J. M. Wallace (2016), Orthogonal PDO and ENSO indices, J. Climate , 29, 3883-3892.
10. Chen, X. Y., and J. M. Wallace (2015), ENSO-like variability: 1900-2013, J. Climate , 28, 9623-9641.
11. Feng, Y., X. Y. Chen, Q. Wang, and Y. Yuan (2015), Mesoscale characteristics of Antarctic Intermediate water in the South Pacific, Acta. Oceanol. Sin. , 34, 91-101.
12. Chen, X. Y. , and K. K. Tung (2014), Varying planetary heat sink led to global-warming slowdown and acceleration, Science , 345, 897-903, doi:10.1126/science.1254937.
13. Chen, X. Y. , Y. Feng, and N. E. Huang (2014), Global sea level trend during 1993-2012, Global Plan. Change, 112C , 26-32, doi:10.1016/j.gloplacha. 2013.11.001.
14. He, J. J., M. Zhang, X. Y. Chen , and M. Wang (2014), Intercomparison of seasonal variability and nonlinear trend between AERONET aerosol optical depth and PM10 mass concentrations in Hong Kong, Sci. China, Earth Sciences , 57, 2606-2615.
15. Chen, X. Y ., M. Wang, Y. L. Zhang, Y. Feng, Z. Wu, and N. E. Huang (2013), Detec t ings i gnals f rom d atawithno i se:t h eory a ndappl i ca ti ons, J.Atm o s.Sci ., 70, 1489-1504, doi:10.1175 / JAS-D-12-0213.1.
16. Zhang,M., J .M.Chen, X.Y.Chen ,T.T.Chen g ,Y.L.Zha n g,H.F.Zh a ng,A. J . Ding,M. W ang,and A.Mellouki(2013),Ur b anAerosolCharact e ri s t i csduring the W orld Expo 2010 in Shanghai. A erosol Air Q uali t y Res. ,2012, 13, 36-48.
17. Chen,X.Y . ,Y.L.Zhang,M.Zhang,Y.Feng,Z.H. W u,F.L.Qiao,andN.E. Huang(2013),In t erco m parison b e t weenObse r vedandS im ulatedVa r iab i l ity in GlobalOcean HeatContentusi n g E m pirical ModeDeco m position, PartI: Modula t edAnnual Cyc l e, Clim. Dyn., 41, No. 11-12, 2797-2815, doi: 10.1 0 07/s00382- 0 12-1554-2.
18. S h ao,Q.L., X .Y.Che n ,a n dR.H uan g( 20 1 2 ), E ffects o fDr ak ePas s a g e o n o cean circ u lati on :A bo x m od elst u d y , S ci.C h i naE a rth S ci. , 56, No. 9, 1588-1598 do i: 1 0 . 1 0 07 / s 11430 - 012 -4 571 - 4.
19. Y i n , X . Q. , F . L . Qi a o , Y . Z . Y an g , C . S . Xia , a n d X . Y . C h e n (2 0 1 2 ) , A r g o d a t a ass i m ilati o n i n o cea n g e nera l circ u la ti o n m od e l o f N o rt h wes t P acifi c Ocea n , Ocea n Dy n . 6 2 , d o i : 1 0 . 1 0 0 7 /s10 23 - 6 -0 12 - 0 5 49 - 1 , 1 0 59 - 1 0 7 1 .
20. Guo,J.S., X.Y.Chen ,J.Sprinta l l,B.H. G uo,F.L.Qiao,andY.L.Y u an(2011),Sur f acein fl owinto theSouthChinaSeat h rough theL u zon Stra i tinwi n ter, C h in. J. Oceanol.Limnol. , 30, 163-168.
21. W u,Z.,N.E.Huang,J.M. W a l lac e , B . S m oliak,and X.Y.Chen (2011 ),Onthe ti m e-varyi n gtrend i ngloba l- m eansurfacete m peratu r e, Cl i m.Dy n . , 37, No.3-4,759-773, doi:10.1007 / s00382-011 - 1128-8.
22. Huang, N. E., X.Y. Chen , M. Lo,and Z. W u (201 1 ),On Hilbertspe c tr a l repre s ent a t i on:Atr u eti m e- f requencyrep r esent a tion f ornonlin e arand nonsta t iona r y data, AADA, 3 , 63-93.
23. W u,Z.,N.E.Huang, a nd X.Y. C hen (2011),S o m econsidera t ionsonphysical analy s is da t a, AADA, 3 ,95-113.
24. Chen,X.Y . ,Z.H. W u,andN.E.Huang(2010),The t i m e-depende n tint r ins i c corr e la t ion b ased on thee m pirical m ode deco m p osition, A A DA, 2 , 233-265.
25. W ang,G., X.Y.Che n ,F.L.Qiao,Z.H.Wu,andN.E.Huang ( 2010 ) , O n int r ins i c m o de f unction, AADA, 2, 2 7 7-293.
26. W u, Z. H.,N. E. Huan g , and X. Y.Chen (2009 ) , The m ulti - di m ensional ense m ble e m pirical m ode deco m p osition m et h od, AADA, 1 , 339-372.
27. Chen,X.Y . ,F.L.Qiao,Q. W ang,X.H. W an g ,andY.L.Yuan(2008),Barri e r and co m pe n sationlay e rsin the Ea s tChina Sea, Acta Ocea n ol. Sin i ca, 2 7 , 70-78.
28. Chen, X.Y., F. L. Qiao, R.F.Ge,C.S.Xia,and Y. L.Yu a n (2006), Develop m e n tofsub-s u r f acewarmwaterinthe E astChinaS e ain f a l l, J.Geophys. Res.,111 , C11S10, doi:10.1029/2 0 05JC003163.
29. Qiao,F.L.,Y.Z.Yang,X.G.Lv,C.S. X i a, X .Y.Chen ,andY.L.Yuan(2006), Coastalup w el l ingin the EastChina Seainwi n t e r, J.Geoph y s.Res.,111 , C11S09, doi:10.1029/2005JC003264.
30. Chen,X.Y . ,X.H. W a ng,andJ. S .Guo(200 5 ),Seasonalvaria b i l ity o fthesea sur f aces a li n ity inthe E a stChinaS e a during19 9 0–2002, J. Geophys.Res.,111, C05008, doi:10.1029/ 2 0 05JC003078.
31. Liu, N., H. X. Chen, X. Y. Chen ,Z. D. Pan, Y. Tao (2005), A dynamic view of the tropospheric teleconnection between IOD and the Pacific Ocean, Chinese Science Bulletin , 50, 2249-2253.
32. Chen, X. Y. ,X. W a ng, X. H. W ang,and F.L.Qi a o (2004), Study of non-Boussi n esq e ff ect on sea sur f aceheight, J. H y dro., Ser B., 16, 518-524.
33. Chen,X.Y . ,F.L.Qiao,X.H. W a n g, W .Zhao,andY.L.Yuan(2004),Onthe studyonBoussinesq a n dhydrost a t i capproxi m ationin o ce a ncirc u l a ti o n m odel, Adv. Mar. S ci., 22 , 91 -96.