Comments on 'Influences of the Bermuda High and atmospheric moistening on changes in summer rainfall in the Atlanta, Georgia region, USA'

Published

Journal Article

In a recent article, Diem (2012) examined the impact of the North Atlantic Subtropical High (NASH) and atmospheric moistening on summer rainfall variability in the Atlanta, Georgia region. In his paper, he indicated that the results concerning the variability of the NASH western ridge discussed in Li et al. (2011) are incorrect. We present new evidence here to show that the comments by Diem (2012) are unjustified; the main conclusions in Li et al. (2011) were drawn according to the data over a 60-year (1948-2007) and 45-year (1958-2002) periods of NCEP/NCAR and ERA-40 reanalysis, whereas conclusions of Diem (2011) were based upon the trend analysis of a similar but different index of the NASH using sub-periods of 1948-2009 (since late 1970s). The comment emphases the importance of climate dynamics to study precipitation variability over the Southeastern US and further strengthens the conclusions originally put forth in Li et al. (2011): over the last 60 years (1948-2007), the NASH has shown a significant trend of westward movement, and the meridional movement of the NASH western-ridge (i.e. its latitudinal change) has enhanced in the recent three decades. © 2013 Royal Meteorological Society.

Full Text

Duke Authors

Cited Authors

  • Li, W; Li, L; Fu, R; Deng, Y; Wang, H

Published Date

  • November 30, 2013

Published In

Volume / Issue

  • 33 / 14

Start / End Page

  • 3083 - 3085

Electronic International Standard Serial Number (EISSN)

  • 1097-0088

International Standard Serial Number (ISSN)

  • 0899-8418

Digital Object Identifier (DOI)

  • 10.1002/joc.3675

Citation Source

  • Scopus