The possible physical mechanism for the EAP–SR co-action

Handle URI:
http://hdl.handle.net/10754/626182
Title:
The possible physical mechanism for the EAP–SR co-action
Authors:
Gong, Zhiqiang; Feng, Guolin; Dogar, Muhammad Mubashar; Huang, Gang
Abstract:
The anomalous characteristics of summer precipitation and atmospheric circulation in the East Asia–West Pacific Region (EA–WP) associated with the co-action of East Asia/Pacific teleconnection–Silk Road teleconnection (EAP–SR) are investigated in this study. The compositions of EAP–SR phase anomalies can be expressed as pattern I (+ +), pattern II (+ −), pattern III (− −), and pattern IV (− +) using EAP and SR indices. It is found that the spatial distribution of summer precipitation anomalies in EA–WP corresponding to pattern I (III) shows a tripole structure in the meridional direction and a zonal dipole structure in the subtropical region, while pattern II (IV) presents a tripole pattern in meridional direction with compressed and continuous anomalies in the zonal direction over the subtropical region. The similar meridional and zonal structures are also found in the geopotential height anomalies at 500-hPa, as well as wind anomalies and moisture convergence at 850-hPa. Finally, a schematic mechanism for the EAP–SR co-action upon the summer precipitation in EA–WP is built: (1) Pattern I (III) exhibits that the negative (positive) sea surface temperature (SST) anomalies over tropical East Pacific may cause the enhanced (weakened) convective activity dominating the West Pacific, trigger the positive (negative) EAP teleconnection and produce more (less) precipitation. Besides, the negative (positive) SST anomalies over the Indonesia Maritime Continent (IMC) may further weaken (strengthen) anomalous downward (upward) motion over the South China Sea (SCS), cause negative (positive) geopotential height anomalies at the middle troposphere and surrounding regions through the function of the tropical Hadley circulation. Then the negative (positive) geopotential height anomalies could motivate the positive (negative) EAP teleconnection through the northward propagation of wave-activity perturbation. Meanwhile, a positive (negative) geopotential height anomalous pattern over Eastern Europe motivates a Rossby wave train propagation from Western Europe to west-central Asia. This circumstance can cause suppressed (enhanced) convection and less (more) precipitation over northwestern India and Pakistan, which could strengthen the negative (positive) geopotential height and positive (negative) vorticity anomalies over central East Asia, resulting in a negative (positive) SR teleconnection along the Asian jet stream. A positive (negative) lobe over the Korean Peninsula and Japan corresponding to SR overlaps with a positive (negative) lobe of EAP, which strengthens the anomalous phase contrast on both sides of 120°E. Accordingly, summer precipitation anomalies in EA–WP exhibit the meridional tripole pattern and the zonal dipole pattern. (2) Pattern II (IV) indicates that the normal SST anomalies over the tropical East Pacific cause the weak tele-impact on the tropical West Pacific, while the positive (negative) SST anomalies over the IMC will lead to a negative (positive) lobe of EAP over the subtropical region. This circumstance can weaken the positive (negative) lobe of SR over subtropical region, causing compressed and continuous negative (positive) anomalies of 500-hPa geopotential height and positive (negative) surface precipitation anomalies from central East China to Japan.
KAUST Department:
Earth Science and Engineering Program
Citation:
Gong Z, Feng G, Dogar MM, Huang G (2017) The possible physical mechanism for the EAP–SR co-action. Climate Dynamics. Available: http://dx.doi.org/10.1007/s00382-017-3967-4.
Publisher:
Springer Nature
Journal:
Climate Dynamics
Issue Date:
17-Nov-2017
DOI:
10.1007/s00382-017-3967-4
Type:
Article
ISSN:
0930-7575; 1432-0894
Sponsors:
The authors wish to thank anonymous reviewers’ meaningful comments that led to a much-improved manuscript. Thanks also are extended to Dr. Pete Saunders for his great help in improving the writing of this manuscript. This work is supported by the National Natural Science Foundation of China (Grant Nos. 41575082, 41530531, and 41475064), the Special Scientific Research Project for Public Interest (Grant No. GYHY201306021).
Additional Links:
http://link.springer.com/article/10.1007/s00382-017-3967-4
Appears in Collections:
Articles; Earth Science and Engineering Program

Full metadata record

DC FieldValue Language
dc.contributor.authorGong, Zhiqiangen
dc.contributor.authorFeng, Guolinen
dc.contributor.authorDogar, Muhammad Mubasharen
dc.contributor.authorHuang, Gangen
dc.date.accessioned2017-11-20T12:48:14Z-
dc.date.available2017-11-20T12:48:14Z-
dc.date.issued2017-11-17en
dc.identifier.citationGong Z, Feng G, Dogar MM, Huang G (2017) The possible physical mechanism for the EAP–SR co-action. Climate Dynamics. Available: http://dx.doi.org/10.1007/s00382-017-3967-4.en
dc.identifier.issn0930-7575en
dc.identifier.issn1432-0894en
dc.identifier.doi10.1007/s00382-017-3967-4en
dc.identifier.urihttp://hdl.handle.net/10754/626182-
dc.description.abstractThe anomalous characteristics of summer precipitation and atmospheric circulation in the East Asia–West Pacific Region (EA–WP) associated with the co-action of East Asia/Pacific teleconnection–Silk Road teleconnection (EAP–SR) are investigated in this study. The compositions of EAP–SR phase anomalies can be expressed as pattern I (+ +), pattern II (+ −), pattern III (− −), and pattern IV (− +) using EAP and SR indices. It is found that the spatial distribution of summer precipitation anomalies in EA–WP corresponding to pattern I (III) shows a tripole structure in the meridional direction and a zonal dipole structure in the subtropical region, while pattern II (IV) presents a tripole pattern in meridional direction with compressed and continuous anomalies in the zonal direction over the subtropical region. The similar meridional and zonal structures are also found in the geopotential height anomalies at 500-hPa, as well as wind anomalies and moisture convergence at 850-hPa. Finally, a schematic mechanism for the EAP–SR co-action upon the summer precipitation in EA–WP is built: (1) Pattern I (III) exhibits that the negative (positive) sea surface temperature (SST) anomalies over tropical East Pacific may cause the enhanced (weakened) convective activity dominating the West Pacific, trigger the positive (negative) EAP teleconnection and produce more (less) precipitation. Besides, the negative (positive) SST anomalies over the Indonesia Maritime Continent (IMC) may further weaken (strengthen) anomalous downward (upward) motion over the South China Sea (SCS), cause negative (positive) geopotential height anomalies at the middle troposphere and surrounding regions through the function of the tropical Hadley circulation. Then the negative (positive) geopotential height anomalies could motivate the positive (negative) EAP teleconnection through the northward propagation of wave-activity perturbation. Meanwhile, a positive (negative) geopotential height anomalous pattern over Eastern Europe motivates a Rossby wave train propagation from Western Europe to west-central Asia. This circumstance can cause suppressed (enhanced) convection and less (more) precipitation over northwestern India and Pakistan, which could strengthen the negative (positive) geopotential height and positive (negative) vorticity anomalies over central East Asia, resulting in a negative (positive) SR teleconnection along the Asian jet stream. A positive (negative) lobe over the Korean Peninsula and Japan corresponding to SR overlaps with a positive (negative) lobe of EAP, which strengthens the anomalous phase contrast on both sides of 120°E. Accordingly, summer precipitation anomalies in EA–WP exhibit the meridional tripole pattern and the zonal dipole pattern. (2) Pattern II (IV) indicates that the normal SST anomalies over the tropical East Pacific cause the weak tele-impact on the tropical West Pacific, while the positive (negative) SST anomalies over the IMC will lead to a negative (positive) lobe of EAP over the subtropical region. This circumstance can weaken the positive (negative) lobe of SR over subtropical region, causing compressed and continuous negative (positive) anomalies of 500-hPa geopotential height and positive (negative) surface precipitation anomalies from central East China to Japan.en
dc.description.sponsorshipThe authors wish to thank anonymous reviewers’ meaningful comments that led to a much-improved manuscript. Thanks also are extended to Dr. Pete Saunders for his great help in improving the writing of this manuscript. This work is supported by the National Natural Science Foundation of China (Grant Nos. 41575082, 41530531, and 41475064), the Special Scientific Research Project for Public Interest (Grant No. GYHY201306021).en
dc.publisherSpringer Natureen
dc.relation.urlhttp://link.springer.com/article/10.1007/s00382-017-3967-4en
dc.rightsThe final publication is available at Springer via http://dx.doi.org/10.1007/s00382-017-3967-4en
dc.subjectEast Asia/Pacific teleconnectionen
dc.subjectSilk Road teleconnectionen
dc.subjectCo-actionen
dc.subjectPrecipitationen
dc.titleThe possible physical mechanism for the EAP–SR co-actionen
dc.typeArticleen
dc.contributor.departmentEarth Science and Engineering Programen
dc.identifier.journalClimate Dynamicsen
dc.eprint.versionPost-printen
dc.contributor.institutionLaboratory for Climate Studies, National Climate Research Center CMA, Beijing, Chinaen
dc.contributor.institutionGlobal Change Impact Studies Centre, Ministry of Climate Change, Islamabad, Pakistanen
dc.contributor.institutionInstitute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, Chinaen
kaust.authorDogar, Muhammad Mubasharen
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