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Yves Guglielmi; Mark McClure; Jeffrey Burghardt; Joseph P. Morris; Thomas Doe; Pengcheng Fu; Hunter Knox; Vince Vermeul; Tim Kneafsey; J. Ajo-Franklin; T. Baumgartner; K. Beckers; D. Blankenship; A. Bonneville; L. Boyd; S. Brown; J.A. Burghardt; C. Chai; A. Chakravarty; T. Chen; Y. Chen; B. Chi; K. Condon; P.J. Cook; D. Crandall; P.F. Dobson; T. Doe; C.A. Doughty; D. Elsworth; J. Feldman; Z. Feng; A. Foris; L.P. Frash; Z. Frone; P. Fu; K. Gao; A. Ghassemi; Y. Guglielmi; B. Haimson; A. Hawkins; J. Heise; C. Hopp; M. Horn; R.N. Horne; J. Horner; M. Hu; H. Huang; L. Huang; K.J. Im; M. Ingraham; E. Jafarov; R.S. Jayne; T.C. Johnson; S.E. Johnson; B. Johnston; S. Karra; K. Kim; D.K. King; T. Kneafsey; H. Knox; J. Knox; D. Kumar; K. Kutun; M. Lee; D. Li; J. Li; K. Li; Z. Li; M. Maceira; P. Mackey; N. Makedonska; C.J. Marone; E. Mattson; M.W. McClure; J. McLennan; T. McLing; C. Medler; R.J. Mellors; E. Metcalfe; J. Miskimins; J. Moore; C.E. Morency; J.P. Morris; T. Myers; S. Nakagawa; G. Neupane; G. Newman; A. Nieto; T. Paronish; R. Pawar; P. Petrov; B. Pietzyk; R. Podgorney; Y. Polsky; J. Pope; S. Porse; J.C. Primo; T. Pyatina; C. Reimers; B.Q. Roberts; M. Robertson; V. Rodríguez-Tribaldos; W. Roggenthen; J. Rutqvist; D. Rynders; M. Schoenball; P. Schwering; V. Sesetty; C.S. Sherman; A. Singh; M.M. Smith; H. Sone; E.L. Sonnenthal; F.A. Soom; D.P. Sprinkle; S. Sprinkle; C.E. Strickland; J. Su; D. Templeton; J.N. Thomle; C. Ulrich; N. Uzunlar; A. Vachaparampil; C.A. Valladao; W. Vandermeer; G. Vandine; D. Vardiman; V.R. Vermeul; J.L. Wagoner; H.F. Wang; J. Weers; N. Welch; J. White; M.D. White; P. Winterfeld; T. Wood; S. Workman; H. Wu; Y.S. Wu; E.C. Yildirim; Y. Zhang; Y.Q. Zhang; Q. Zhou; M.D. Zoback
International Journal of Climatology · 2023 · Vol. 43 · Issue 3 · Wiley
The Pacific‐Japan (PJ) pattern is the dominant teleconnection over East Asia, closely related to the summer precipitation on various time scales. However, studies on the connection between the interdecadal variations of the PJ pattern and sea surface temperature (SST) forcing are still limited. This study indicates that the relationship between the PJ pattern and ENSO presents a pronounced interdecadal change around 1997/1998....