Aerosol and Clouds
Characteristics of tropical cyclone precipitation features over the western Pacific warm pool
Article first published online: 18 AUG 2012
©2012. American Geophysical Union. All Rights Reserved.
Journal of Geophysical Research: Atmospheres (1984–2012)
Volume 117, Issue D16, 27 August 2012
How to Cite
2012), Characteristics of tropical cyclone precipitation features over the western Pacific warm pool, J. Geophys. Res., 117, D16208, doi:10.1029/2011JD017351., , , and (
- Issue published online: 18 AUG 2012
- Article first published online: 18 AUG 2012
- Manuscript Accepted: 10 JUL 2012
- Manuscript Revised: 9 JUL 2012
- Manuscript Received: 16 DEC 2011
- precipitation feature;
- tropical cyclone;
 In this study, ten years (1998–2007) of the Tropical Rainfall Measuring Mission (TRMM)-derivative radar precipitation feature (PF) product are analyzed in order to determine the differences between tropical cyclone-related precipitation characteristics compared with those of the tropical Pacific warm pool (10 to 30°N and 130 to 150°E) in general. The PF data, from the University of Utah's archive, are based on the TRMM precipitation radar's 2A25 product, where one PF consists of a single or group of contiguous pixels with near surface rainfall greater than zero. Using the PF database, the height and area of tropical background PFs versus those within 500 km of tropical cyclones (TCs) are compared. It is found that TC-related PFs are markedly more frequent from 5 to 10 km altitude than are background tropical PFs. The enhanced midlevel TC-related populations not only exist in stratiform precipitation around the melting level at 5.5 km, but also from 6 to 9 km in stratiform regions, in convective precipitation, and when culling the smallest features from the data set. This increase in congestus-like echoes in TC environments aligns well with observations regarding mesoscale convective systems (MCSs), in which the enhanced ice present in MCS (and TC) environments creates a stabilized melting layer through cooling immediately below 0°C. This stable layer appears to enhance the detrainment of convective PFs in our TC data set at and for a few kilometers above the melting level.