DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Evolution of Idealized Vortices in Monsoon-Like Shears: Application to Monsoon Depressions

Abstract

Abstract This study examines processes fundamental to the development of South Asian monsoon depressions using an array of integrations of an idealized convection-permitting numerical model. In each integration, a wave of initially small amplitude is subjected to a different amount of vertical and meridional wind shear, with temperature and moisture fields constructed according to realistic constraints. Based on the evolution of this disturbance into monsoon depression–like vortices, two features of the background environment emerge as important: the low-level gradient of moist static energy (MSE) and the low-level meridional shear. As the low-level MSE gradient steepens, the disturbance becomes stronger and produces more rain. This strengthening results from the interaction of the vortex with latent heat release by convection that is in turn organized by positive MSE advection in the northerly flow west of the vortex. In this region of advection, moister air from the north ascends along upward-sloping isentropes, driving moist convection. The disturbance also becomes stronger with increasing meridional shear, which makes the environment more barotropically unstable. The absence of either of these two features of the background environment prevents substantial growth of the disturbance. Our results suggest that monsoon depression growth in South Asia is fostered by themore » coexistence of a strong low-level MSE gradient with strong meridional wind shear associated with the monsoon trough.« less

Authors:
 [1];  [2]
  1. a Department of Earth and Planetary Science, University of California, Berkeley, Berkeley, California
  2. a Department of Earth and Planetary Science, University of California, Berkeley, Berkeley, California, b Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, California
Publication Date:
Research Org.:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
2217394
Alternate Identifier(s):
OSTI ID: 1864539
Grant/Contract Number:  
AC02-05CH11231; SC0019367
Resource Type:
Published Article
Journal Name:
Journal of the Atmospheric Sciences
Additional Journal Information:
Journal Name: Journal of the Atmospheric Sciences Journal Volume: 78 Journal Issue: 4; Journal ID: ISSN 0022-4928
Publisher:
American Meteorological Society
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Asia; baroclinic flows; convection; cyclogenesis; cyclolysis; monsoons; mesoscale models

Citation Formats

Diaz, Michael, and Boos, William R. Evolution of Idealized Vortices in Monsoon-Like Shears: Application to Monsoon Depressions. United States: N. p., 2021. Web. doi:10.1175/JAS-D-20-0286.1.
Diaz, Michael, & Boos, William R. Evolution of Idealized Vortices in Monsoon-Like Shears: Application to Monsoon Depressions. United States. https://doi.org/10.1175/JAS-D-20-0286.1
Diaz, Michael, and Boos, William R. Thu . "Evolution of Idealized Vortices in Monsoon-Like Shears: Application to Monsoon Depressions". United States. https://doi.org/10.1175/JAS-D-20-0286.1.
@article{osti_2217394,
title = {Evolution of Idealized Vortices in Monsoon-Like Shears: Application to Monsoon Depressions},
author = {Diaz, Michael and Boos, William R.},
abstractNote = {Abstract This study examines processes fundamental to the development of South Asian monsoon depressions using an array of integrations of an idealized convection-permitting numerical model. In each integration, a wave of initially small amplitude is subjected to a different amount of vertical and meridional wind shear, with temperature and moisture fields constructed according to realistic constraints. Based on the evolution of this disturbance into monsoon depression–like vortices, two features of the background environment emerge as important: the low-level gradient of moist static energy (MSE) and the low-level meridional shear. As the low-level MSE gradient steepens, the disturbance becomes stronger and produces more rain. This strengthening results from the interaction of the vortex with latent heat release by convection that is in turn organized by positive MSE advection in the northerly flow west of the vortex. In this region of advection, moister air from the north ascends along upward-sloping isentropes, driving moist convection. The disturbance also becomes stronger with increasing meridional shear, which makes the environment more barotropically unstable. The absence of either of these two features of the background environment prevents substantial growth of the disturbance. Our results suggest that monsoon depression growth in South Asia is fostered by the coexistence of a strong low-level MSE gradient with strong meridional wind shear associated with the monsoon trough.},
doi = {10.1175/JAS-D-20-0286.1},
journal = {Journal of the Atmospheric Sciences},
number = 4,
volume = 78,
place = {United States},
year = {Thu Apr 01 00:00:00 EDT 2021},
month = {Thu Apr 01 00:00:00 EDT 2021}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record
https://doi.org/10.1175/JAS-D-20-0286.1

Save / Share:

Works referenced in this record:

The Baroclinic Processes of Monsoon Depressions
journal, July 1983


Interactions between Water Vapor and Potential Vorticity in Synoptic-Scale Monsoonal Disturbances: Moisture Vortex Instability
journal, June 2018


Monsoon Low Pressure System–Like Variability in an Idealized Moist Model
journal, March 2020


Tropical cyclogenesis in a tropical wave critical layer: easterly waves
journal, January 2009

  • Dunkerton, T. J.; Montgomery, M. T.; Wang, Z.
  • Atmospheric Chemistry and Physics, Vol. 9, Issue 15
  • DOI: 10.5194/acp-9-5587-2009

The Weak Temperature Gradient Approximation and Balanced Tropical Moisture Waves*
journal, December 2001


Moisture and Moist Static Energy Budgets of South Asian Monsoon Low Pressure Systems in GFDL AM4.0
journal, June 2018


A Genesis Index for Monsoon Disturbances
journal, July 2016

  • Ditchek, Sarah D.; Boos, William R.; Camargo, Suzana J.
  • Journal of Climate, Vol. 29, Issue 14
  • DOI: 10.1175/JCLI-D-15-0704.1

Baroclinic Instability with Cumulus Heating
journal, October 1985


A Revised Approach to Ice Microphysical Processes for the Bulk Parameterization of Clouds and Precipitation
journal, January 2004


Monsoon depression amplification by moist barotropic instability in a vertically sheared environment
journal, June 2019

  • Diaz, Michael; Boos, William R.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 145, Issue 723
  • DOI: 10.1002/qj.3585

Quasi‐geostrophic dynamics in the presence of moisture gradients
journal, September 2015

  • Monteiro, Joy M.; Sukhatme, Jai
  • Quarterly Journal of the Royal Meteorological Society, Vol. 142, Issue 694
  • DOI: 10.1002/qj.2644

Barotropic growth of monsoon depressions
journal, January 2019

  • Diaz, Michael; Boos, William R.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 145, Issue 719
  • DOI: 10.1002/qj.3467

Mesoscale precipitation systems and their role in the rapid development of a monsoon depression over the Bay of Bengal
journal, December 2019

  • Fujinami, Hatsuki; Hirata, Hidetaka; Kato, Masaya
  • Quarterly Journal of the Royal Meteorological Society, Vol. 146, Issue 726
  • DOI: 10.1002/qj.3672

Nonlinear Balance and Potential-Vorticity Thinking At Large Rossby Number
journal, July 1992

  • Raymond, D. J.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 118, Issue 507
  • DOI: 10.1002/qj.49711850708

Assessing Historical Variability of South Asian Monsoon Lows and Depressions With an Optimized Tracking Algorithm
journal, August 2020

  • Vishnu, S.; Boos, W. R.; Ullrich, P. A.
  • Journal of Geophysical Research: Atmospheres, Vol. 125, Issue 15
  • DOI: 10.1029/2020JD032977

On the Distribution and Continuity of Water Substance in Atmospheric Circulations
book, January 1969