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

Title: Characteristics of Bay of Bengal Monsoon Depressions in the 21st Century

Abstract

Abstract We show that 21st century increase in radiative forcing does not significantly impact the frequency of South Asian summer monsoon depressions (MDs) or their trajectories in the Coupled Model Intercomparison Project Phase 5 general circulation models (GCMs). A significant relationship exists between the climatological occurrences of MDs and the strength of the background upper (lower) tropospheric meridional (zonal) winds and tropospheric moisture in the core genesis region of MDs. Likewise, there is a strong relationship between the strength of the meridional tropospheric temperature gradient in the GCMs and the trajectories of MDs over land. While monsoon dynamics progressively weakens in the future, atmospheric moisture exhibits a strong increase, limiting the impact of changes in dynamics on the frequency of MDs. Moreover, the weakening of meridional tropospheric temperature gradient in the future is substantially weaker than its inherent underestimation in the GCMs. Our results also indicate that future increases in the extreme wet events are dominated by nondepression day occurrences, which may render the monsoon extremes less predictable in the future.

Authors:
ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [3];  [3];  [4]; ORCiD logo [1]
  1. Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
  2. Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
  3. Indian Institute of Technology Bombay, Mumbai (India)
  4. Univ. of Reading, Reading (United Kingdom)
Publication Date:
Research Org.:
Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States). Oak Ridge Leadership Computing Facility (OLCF)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
1474867
Alternate Identifier(s):
OSTI ID: 1459445
Grant/Contract Number:  
AC05-00OR22725; DE‐AC05‐76RL01830; DE‐AC05‐00OR22725
Resource Type:
Accepted Manuscript
Journal Name:
Geophysical Research Letters
Additional Journal Information:
Journal Volume: 45; Journal Issue: 13; Journal ID: ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; monsoon depression; climate change; South Asian monsoon

Citation Formats

Rastogi, Deeksha, Ashfaq, Moetasim, Leung, L. Ruby, Ghosh, Subimal, Saha, Anamitra, Hodges, Kevin, and Evans, Katherine J. Characteristics of Bay of Bengal Monsoon Depressions in the 21st Century. United States: N. p., 2018. Web. doi:10.1029/2018GL078756.
Rastogi, Deeksha, Ashfaq, Moetasim, Leung, L. Ruby, Ghosh, Subimal, Saha, Anamitra, Hodges, Kevin, & Evans, Katherine J. Characteristics of Bay of Bengal Monsoon Depressions in the 21st Century. United States. https://doi.org/10.1029/2018GL078756
Rastogi, Deeksha, Ashfaq, Moetasim, Leung, L. Ruby, Ghosh, Subimal, Saha, Anamitra, Hodges, Kevin, and Evans, Katherine J. Thu . "Characteristics of Bay of Bengal Monsoon Depressions in the 21st Century". United States. https://doi.org/10.1029/2018GL078756. https://www.osti.gov/servlets/purl/1474867.
@article{osti_1474867,
title = {Characteristics of Bay of Bengal Monsoon Depressions in the 21st Century},
author = {Rastogi, Deeksha and Ashfaq, Moetasim and Leung, L. Ruby and Ghosh, Subimal and Saha, Anamitra and Hodges, Kevin and Evans, Katherine J.},
abstractNote = {Abstract We show that 21st century increase in radiative forcing does not significantly impact the frequency of South Asian summer monsoon depressions (MDs) or their trajectories in the Coupled Model Intercomparison Project Phase 5 general circulation models (GCMs). A significant relationship exists between the climatological occurrences of MDs and the strength of the background upper (lower) tropospheric meridional (zonal) winds and tropospheric moisture in the core genesis region of MDs. Likewise, there is a strong relationship between the strength of the meridional tropospheric temperature gradient in the GCMs and the trajectories of MDs over land. While monsoon dynamics progressively weakens in the future, atmospheric moisture exhibits a strong increase, limiting the impact of changes in dynamics on the frequency of MDs. Moreover, the weakening of meridional tropospheric temperature gradient in the future is substantially weaker than its inherent underestimation in the GCMs. Our results also indicate that future increases in the extreme wet events are dominated by nondepression day occurrences, which may render the monsoon extremes less predictable in the future.},
doi = {10.1029/2018GL078756},
journal = {Geophysical Research Letters},
number = 13,
volume = 45,
place = {United States},
year = {Thu Jun 21 00:00:00 EDT 2018},
month = {Thu Jun 21 00:00:00 EDT 2018}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Citation Metrics:
Cited by: 17 works
Citation information provided by
Web of Science

Figures / Tables:

Figure 1 Figure 1: Characteristics of monsoon depressions (MDs) in the historical period. (a) Individual trajectories of MDs in National Centers for Environmental Prediction R1, (b) ERA-Interim, and (c) Modern-Era Retrospective analysis for Research and Applications 2. The green stars represent the starting point of each MD, and the colored circles representmore » the magnitude of relative vorticity every 12 hr. (d) Time series of number of MDs per year in Reanalysis data sets. (e) Mean trajectory of MDs in the Reanalysis and Coupled Model Intercomparison Project Phase 5 global climate models (GCMs). (f) Number of MDs per year (red) and those that cross 20°N and move northwestward during their life span (blue). The color of each GCM name in (f) corresponds to the color of each line in (e). Historical period refers to 1965–2005 unless otherwise stated.« less

Save / Share:

Works referenced in this record:

A Multiscale Analysis of the Extreme Weather Events over Western Russia and Northern Pakistan during July 2010
journal, May 2012

  • Galarneau, Thomas J.; Hamill, Thomas M.; Dole, Randall M.
  • Monthly Weather Review, Vol. 140, Issue 5
  • DOI: 10.1175/MWR-D-11-00191.1

Moisture Vertical Structure, Column Water Vapor, and Tropical Deep Convection
journal, June 2009

  • Holloway, Christopher E.; Neelin, J. David
  • Journal of the Atmospheric Sciences, Vol. 66, Issue 6
  • DOI: 10.1175/2008JAS2806.1

Feature Tracking on the Unit Sphere
journal, December 1995


How Do Microphysical Processes Influence Large‐Scale Precipitation Variability and Extremes?
journal, February 2018

  • Hagos, Samson; Ruby Leung, L.; Zhao, Chun
  • Geophysical Research Letters, Vol. 45, Issue 3
  • DOI: 10.1002/2017GL076375

Some aspects of the life history, structure and movement of monsoon depressions
journal, January 1977

  • Sikka, D. R.
  • Pure and Applied Geophysics PAGEOPH, Vol. 115, Issue 5-6
  • DOI: 10.1007/BF00874421

Decline and poleward shift in Indian summer monsoon synoptic activity in a warming climate
journal, February 2018

  • Sandeep, S.; Ajayamohan, R. S.; Boos, William R.
  • Proceedings of the National Academy of Sciences, Vol. 115, Issue 11
  • DOI: 10.1073/pnas.1709031115

Thermodynamic Bias in the Multimodel Mean Boreal Summer Monsoon
journal, April 2013


On the decreasing trend of the number of monsoon depressions in the Bay of Bengal
journal, January 2016


The South Asian Summer Monsoon and Its Relationship with ENSO in the IPCC AR4 Simulations
journal, March 2007

  • Annamalai, H.; Hamilton, K.; Sperber, K. R.
  • Journal of Climate, Vol. 20, Issue 6
  • DOI: 10.1175/JCLI4035.1

Increasing Trend of Extreme Rain Events Over India in a Warming Environment
journal, December 2006


The Asian summer monsoon: an intercomparison of CMIP5 vs. CMIP3 simulations of the late 20th century
journal, December 2012


Falling monsoon depression frequency: A Gray-Sikka conditions perspective
journal, October 2013

  • Prajeesh, A. G.; Ashok, K.; Rao, D. V. Bhaskar
  • Scientific Reports, Vol. 3, Issue 1
  • DOI: 10.1038/srep02989

Dominating Controls for Wetter South Asian Summer Monsoon in the Twenty-First Century
journal, April 2015


The NCEP–NCAR 50–Year Reanalysis: Monthly Means CD–ROM and Documentation
journal, February 2001


On the Relationship between Mean Monsoon Precipitation and Low Pressure Systems in Climate Model Simulations
journal, July 2015


The spatiotemporal structure of precipitation in Indian monsoon depressions: Spatiotemporal Structure of Precipitation in MDs
journal, October 2016

  • Hunt, Kieran M. R.; Turner, Andrew G.; Parker, David E.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 142, Issue 701
  • DOI: 10.1002/qj.2901

A modified Mann-Kendall trend test for autocorrelated data
journal, January 1998


GPCP Pentad Precipitation Analyses: An Experimental Dataset Based on Gauge Observations and Satellite Estimates
journal, July 2003

  • Xie, Pingping; Janowiak, John E.; Arkin, Phillip A.
  • Journal of Climate, Vol. 16, Issue 13
  • DOI: 10.1175/2769.1

Suppression of south Asian summer monsoon precipitation in the 21st century
journal, January 2009

  • Ashfaq, Moetasim; Shi, Ying; Tung, Wen-wen
  • Geophysical Research Letters, Vol. 36, Issue 1
  • DOI: 10.1029/2008GL036500

The Modern-Era Retrospective Analysis for Research and Applications, Version 2 (MERRA-2)
journal, July 2017


Has the number of Indian summer monsoon depressions decreased over the last 30 years?
journal, November 2014

  • Cohen, Naftali Y.; Boos, William R.
  • Geophysical Research Letters, Vol. 41, Issue 22
  • DOI: 10.1002/2014GL061895

Adaptive Constraints for Feature Tracking
journal, June 1999


Updated high-resolution grids of monthly climatic observations - the CRU TS3.10 Dataset: UPDATED HIGH-RESOLUTION GRIDS OF MONTHLY CLIMATIC OBSERVATIONS
journal, May 2013

  • Harris, I.; Jones, P. D.; Osborn, T. J.
  • International Journal of Climatology, Vol. 34, Issue 3
  • DOI: 10.1002/joc.3711

Sources of errors in the simulation of south Asian summer monsoon in the CMIP5 GCMs
journal, September 2016


A global climatology of monsoon low-pressure systems: Global Climatology of Monsoon Low-Pressure Systems
journal, October 2014

  • Hurley, John V.; Boos, William R.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 141, Issue 689
  • DOI: 10.1002/qj.2447

The ERA-Interim reanalysis: configuration and performance of the data assimilation system
journal, April 2011

  • Dee, D. P.; Uppala, S. M.; Simmons, A. J.
  • Quarterly Journal of the Royal Meteorological Society, Vol. 137, Issue 656
  • DOI: 10.1002/qj.828

Assessing reliability of regional climate projections: the case of Indian monsoon
journal, February 2014

  • Ramesh, K. V.; Goswami, Prashant
  • Scientific Reports, Vol. 4, Issue 1
  • DOI: 10.1038/srep04071

Works referencing / citing this record:

Regional Climate Response of Middle Eastern, African, and South Asian Monsoon Regions to Explosive Volcanism and ENSO Forcing
journal, July 2019

  • Dogar, Muhammad Mubashar; Sato, Tomonori
  • Journal of Geophysical Research: Atmospheres, Vol. 124, Issue 14
  • DOI: 10.1029/2019jd030358

Tropical Lows in Southern Africa: Tracks, Rainfall Contributions, and the Role of ENSO
journal, November 2019

  • Howard, Emma; Washington, Richard; Hodges, Kevin I.
  • Journal of Geophysical Research: Atmospheres, Vol. 124, Issue 21
  • DOI: 10.1029/2019jd030803

Figures/Tables have been extracted from DOE-funded journal article accepted manuscripts.