2013
DOI: 10.1073/pnas.1215582110
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Origin of seasonal predictability for summer climate over the Northwestern Pacific

Abstract: Summer climate in the Northwestern Pacific (NWP) displays large year-to-year variability, affecting densely populated Southeast and East Asia by impacting precipitation, temperature, and tropical cyclones. The Pacific-Japan (PJ) teleconnection pattern provides a crucial link of high predictability from the tropics to East Asia. Using coupled climate model experiments, we show that the PJ pattern is the atmospheric manifestation of an air-sea coupled mode spanning the Indo-NWP warm pool. The PJ pattern forces t… Show more

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Cited by 271 publications
(251 citation statements)
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“…It is noted that this mechanism tends to amplify both the SAM and EAM precipitation simultaneously in the boreal summer. The ENSO efficiently excites the PJ teleconnection pattern associated with the WNPSH by inducing IO SST anomalies as an initial perturbation (Kosaka et al 2013;Chowdary et al 2014).…”
Section: Relative Role Of Tropical Sst Forcing In Numerical Experimentsmentioning
confidence: 99%
See 1 more Smart Citation
“…It is noted that this mechanism tends to amplify both the SAM and EAM precipitation simultaneously in the boreal summer. The ENSO efficiently excites the PJ teleconnection pattern associated with the WNPSH by inducing IO SST anomalies as an initial perturbation (Kosaka et al 2013;Chowdary et al 2014).…”
Section: Relative Role Of Tropical Sst Forcing In Numerical Experimentsmentioning
confidence: 99%
“…The tropical teleconnection is called the western North Pacific-North America (WPNA) pattern, including the WPSH as an important factor bridging the SAM and EAM climate (Wang et al 2001;Kosaka et al 2013;Lee et al 2013a, b).…”
Section: Decaying Ensomentioning
confidence: 99%
“…The most pronounced feature of the C-mode circulation pattern is the anomalous lowlevel Northwest Pacific anticyclone (NWP-AC). This important large-scale atmospheric feature links ENSO impacts to the Asian Monsoon systems (20)(21)(22)(23)(24)(25) by shifting rainfall patterns (SI Appendix, Fig. S1B), and it drives sea level changes in the tropical Western Pacific that impact coastal systems (26).…”
mentioning
confidence: 99%
“…To account for possible transoceanic interactions addressed by some studies (Hong et al, 2014b), the NAO index, referred to as the meridional seesaw of the SLP field with the northern and southern centres near Iceland and the Azores, respectively, is also included. Furthermore, as the predictand of interest is highly related to summertime tropical cyclone (TC) activity, the list contains the QBO (Quasi-Biennial Oscillation, Baldwin et al, 2001), WP, and PJ indices (Choi et al, 2010;Kosaka et al, 2013). The QBO depicts a quasiperiodic oscillation between easterlies (positive) and westerlies (negative phase) over the lower tropical stratosphere, and the period is approximately 20-36 months.…”
Section: Streamflow Data Teleconnection Indices and Other Data Setsmentioning
confidence: 99%