Extreme daily rainfall in Pakistan and north India: scale-interactions, mechanisms, and precursors

[thumbnail of Open Access]
Preview
Text (Open Access) - Published Version
· Please see our End User Agreement before downloading.
| Preview
[thumbnail of HuntTurnerShaffrey2018mwr_accepted.pdf]
Preview
Text - Accepted Version
· Please see our End User Agreement before downloading.
| Preview

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Hunt, K. M. R. orcid id iconORCID: https://orcid.org/0000-0003-1480-3755, Turner, A. G. orcid id iconORCID: https://orcid.org/0000-0002-0642-6876 and Shaffrey, L. C. orcid id iconORCID: https://orcid.org/0000-0003-2696-752X (2018) Extreme daily rainfall in Pakistan and north India: scale-interactions, mechanisms, and precursors. Monthly Weather Review, 146 (4). pp. 1005-1022. ISSN 0027-0644 doi: 10.1175/MWR-D-17-0258.1

Abstract/Summary

While much of India is used to heavy precipitation and frequent low-pressure systems during the summer monsoon, towards the northwest and into Pakistan, such events are uncommon. Here, as much as a third of the annual rainfall is delivered sporadically during the winter monsoon by western disturbances. Such events of sparse but heavy precipitation in this region of typically mountainous valleys in the north and desert in the south can be catastrophic, as in the case of the Pakistan floods of July 2010. In this study, we identify extreme precipitation events (EPEs) in a box approximately covering this region (65◦ -78◦W, 25◦ -38◦N) using the APHRODITE gauge-based precipitation product. The role of the large-scale circulation in causing EPEs is investigated: it is found that, during winter, they often coexist with an upper-tropospheric Rossby wave train that has prominent anomalous southerlies over the region of interest. These winter EPEs are also found to be strongly colocated with incident western disturbances whereas those occurring during the summer are found to have a less direct relationship. Conversely, summer EPEs are found to have a strong relationship with tropical lows. A detailed Lagrangian method is used to explore possible sources of moisture for such events, and suggests that in winter, the moisture is mostly drawn from the Arabian Sea, whereas during the summer, it comes from along the African coast and the Indian monsoon trough region.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/75584
Identification Number/DOI 10.1175/MWR-D-17-0258.1
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