Search from over 60,000 research works

Advanced Search

Seasonal effects of the Tibetan plateau on the cyclonic transient eddies: a system-centered view

[thumbnail of Manu_track - Ren etal-revised-final2.pdf]
Preview
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Ren, Q., Hodges, K. I. orcid id iconORCID: https://orcid.org/0000-0003-0894-229X, Schiemann, R. orcid id iconORCID: https://orcid.org/0000-0003-3095-9856, Dai, Y., Jiang, X. and Yang, S. (2023) Seasonal effects of the Tibetan plateau on the cyclonic transient eddies: a system-centered view. Journal of Climate, 36 (17). pp. 6007-6020. ISSN 1520-0442 doi: 10.1175/JCLI-D-23-0067.1

Abstract/Summary

Using the objective feature tracking algorithm and hourly reanalysis data, seasonal behaviors of the cyclonic transient eddies (cyclones) at different levels around the Tibetan Plateau (TP) have been examined to reveal the effects of the TP on cyclones. Results show that TP tend to change moving directions of the remote cyclones when they are close to the TP, only some 250-hPa cyclones can directly pass the TP from west to east. Their moving speeds and relative vorticities suddenly weaken around the TP, suggesting the suppression effect of the TP. Over 70% of these cyclones die out over the TP regardless of the altitude, which slightly decreases to around 65% during summer, exhibiting a weak summertime suppression effect. On the other hand, TP has a strong excitation effect on local cyclones through dynamic forcing in winter, thermodynamic forcing in summer, and both in transitional seasons. Numbers of these local cyclones, especially at 500hPa that is almost the surface height of the TP, are greatly larger than that of the remote cyclones during all seasons. About half of these local cyclones dissipate over the TP. Nonetheless, cyclones moving off the TP are more than the cyclones entering the TP, with the differences ranging from 0 to 6 cyclones per month. Only the 250-hPa wintertime moving-off cyclones are less than the cyclones entering the TP, which may be caused by the relatively weak excitation and strong suppression effects of the TP on the wintertime upper-level cyclones.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/111619
Item Type Article
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Meteorological Society
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar