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Barotropic growth of monsoon depressions

Journal Article · · Quarterly Journal of the Royal Meteorological Society
DOI:https://doi.org/10.1002/qj.3467· OSTI ID:1542355
 [1];  [2]
  1. Univ. of California, Berkeley, CA (United States)
  2. Univ. of California, Berkeley, CA (United States); Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
While monsoon depressions are a principal synoptic-scale element of the South Asian monsoon, producing extreme rainfall over India and surrounding regions, there exists no widely accepted mechanism explaining their occurrence. This study presents a hierarchy of numerical experiments aimed at finding such an explanation. Using a perturbation-basic state decomposition, we derive an anelastic system of equations that can represent disturbances growing in the complex, three-dimensional monsoon basic state. We find that modal solutions to these equations linearized about this basic state can explain many features of observed monsoon depressions, including their warm-over-cold core structure, westward propagation, and lower-tropospheric wind maximum. For the zonally symmetric case, these modes are barotropically unstable, drawing energy from the meridional shear of the monsoon trough. For the zonally varying basic state, modal solutions still derive energy from barotropic conversion, but fail to achieve positive net growth rates when dissipative processes are included. For the nonlinear equation set, these modes can be excited by a heating impulse, and their energy then remains roughly constant over several days as barotropic energy transfers oppose dissipative losses. Our conclusions support the idea that the general concept of barotropic instability can explain the structure, propagation, and geographic distribution of monsoon depressions, but not their rapid growth rates. We suggest that condensational heating coupled to these waves is needed to obtain a positive growth rate.
Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
National Science Foundation (NSF); Office of Naval Research; USDOE; USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
Grant/Contract Number:
AC02-05CH11231; SC0019367
OSTI ID:
1542355
Alternate ID(s):
OSTI ID: 1494214
Journal Information:
Quarterly Journal of the Royal Meteorological Society, Journal Name: Quarterly Journal of the Royal Meteorological Society Journal Issue: 719 Vol. 145; ISSN 0035-9009
Publisher:
Royal Meteorological SocietyCopyright Statement
Country of Publication:
United States
Language:
English

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Cited By (3)

Monsoon depression amplification by moist barotropic instability in a vertically sheared environment journal June 2019
Mesoscale precipitation systems and their role in the rapid development of a monsoon depression over the Bay of Bengal
  • Fujinami, Hatsuki; Hirata, Hidetaka; Kato, Masaya
  • Quarterly Journal of the Royal Meteorological Society, Vol. 146, Issue 726 https://doi.org/10.1002/qj.3672
journal December 2019
Downstream and In Situ: Two Perspectives on the Initiation of Monsoon Low‐Pressure Systems Over the Bay of Bengal journal November 2019

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