Abstract
AbstractAn idealized dataset that contains a background seasonal mean state, a reference intraseasonal oscillation (ISO) state and real‐strength tropical cyclones (TCs) was constructed, in order to examine to what extent the presence of the real‐strength TCs may impact the overall ISO strength over the western North Pacific. The averaged ISO strength (measured by combined 850‐hPa zonal and meridional wind fields) increases by 9% when the realistic TCs are included. The percentage increase of the overall ISO strength depends on the variable used. It is doubled (reduced to 3%) when the vorticity (stream function) is used as the estimated variable.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
