The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP
Abstract
Some of the highest summer monsoon rainfall in South Asia falls on the windward slopes of the Western Ghats mountains on India's west coast and offshore over the eastern Arabian Sea. Understanding of the processes determining the spatial distribution and temporal variability of this region remains incomplete. In this paper, new Interaction of Convective Organization and Monsoon Precipitation, Atmosphere, Surface and Sea (INCOMPASS) aircraft and ground‐based measurements of the summer monsoon over the Western Ghats and upstream of them are presented and placed within the context of remote‐sensing observations and reanalysis. The transition from widespread rainfall over the eastern Arabian Sea to rainfall over the Western Ghats is documented in high spatial and temporal resolution. Heavy rainfall offshore during the campaign was associated primarily with mid‐tropospheric humidity, secondarily with sea surface temperature, and only weakly with orographic blocking. A mid‐tropospheric dry intrusion suppressed deep convection offshore in the latter half of the campaign, allowing the build‐up of low‐level humidity in the onshore flow and enhancing rainfall over the mountains. Rainfall on the lee side of the Western Ghats occurred during the latter half of the campaign in association with enhanced mesoscale easterly upslope flow. Diurnal cycles in rainfall offshore (maximummore »
- Authors:
-
- School of Earth and Environment University of Leeds Leeds UK
- Department of Meteorology University of Reading Reading UK, National Centre for Atmospheric Science University of Reading Reading UK
- Met Office Hadley Centre Exeter UK
- National Centre for Medium Range Weather Forecasting Noida India
- CSIR–National Aerospace Laboratories Bengaluru India
- Department of Meteorology University of Reading Reading UK
- Centre for Ecology and Hydrology Wallingford UK, National Centre for Earth Observation Wallingford UK
- Department of Atmospheric Sciences University of Washington Seattle WA USA, Pacific Northwest National Laboratory Richland SC USA
- National Centre for Earth Observation Wallingford UK
- Centre for Atmospheric and Oceanic Sciences Indian Institute of Science Bengaluru India
- Publication Date:
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1505645
- Alternate Identifier(s):
- OSTI ID: 1505646
- Resource Type:
- Published Article
- Journal Name:
- Quarterly Journal of the Royal Meteorological Society
- Additional Journal Information:
- Journal Name: Quarterly Journal of the Royal Meteorological Society Journal Volume: 146 Journal Issue: 731; Journal ID: ISSN 0035-9009
- Publisher:
- Wiley Blackwell (John Wiley & Sons)
- Country of Publication:
- United Kingdom
- Language:
- English
Citation Formats
Fletcher, Jennifer K., Parker, Douglas J., Turner, Andrew G., Menon, Arathy, Martin, Gill M., Birch, Cathryn E., Mitra, Ashis K., Mrudula, G., Hunt, Kieran M. R., Taylor, Christopher M., Houze, Robert A., Brodzik, Stella R., and Bhat, G. S. The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP. United Kingdom: N. p., 2019.
Web. doi:10.1002/qj.3439.
Fletcher, Jennifer K., Parker, Douglas J., Turner, Andrew G., Menon, Arathy, Martin, Gill M., Birch, Cathryn E., Mitra, Ashis K., Mrudula, G., Hunt, Kieran M. R., Taylor, Christopher M., Houze, Robert A., Brodzik, Stella R., & Bhat, G. S. The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP. United Kingdom. https://doi.org/10.1002/qj.3439
Fletcher, Jennifer K., Parker, Douglas J., Turner, Andrew G., Menon, Arathy, Martin, Gill M., Birch, Cathryn E., Mitra, Ashis K., Mrudula, G., Hunt, Kieran M. R., Taylor, Christopher M., Houze, Robert A., Brodzik, Stella R., and Bhat, G. S. Sun .
"The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP". United Kingdom. https://doi.org/10.1002/qj.3439.
@article{osti_1505645,
title = {The dynamic and thermodynamic structure of the monsoon over southern India: New observations from the INCOMPASS IOP},
author = {Fletcher, Jennifer K. and Parker, Douglas J. and Turner, Andrew G. and Menon, Arathy and Martin, Gill M. and Birch, Cathryn E. and Mitra, Ashis K. and Mrudula, G. and Hunt, Kieran M. R. and Taylor, Christopher M. and Houze, Robert A. and Brodzik, Stella R. and Bhat, G. S.},
abstractNote = {Some of the highest summer monsoon rainfall in South Asia falls on the windward slopes of the Western Ghats mountains on India's west coast and offshore over the eastern Arabian Sea. Understanding of the processes determining the spatial distribution and temporal variability of this region remains incomplete. In this paper, new Interaction of Convective Organization and Monsoon Precipitation, Atmosphere, Surface and Sea (INCOMPASS) aircraft and ground‐based measurements of the summer monsoon over the Western Ghats and upstream of them are presented and placed within the context of remote‐sensing observations and reanalysis. The transition from widespread rainfall over the eastern Arabian Sea to rainfall over the Western Ghats is documented in high spatial and temporal resolution. Heavy rainfall offshore during the campaign was associated primarily with mid‐tropospheric humidity, secondarily with sea surface temperature, and only weakly with orographic blocking. A mid‐tropospheric dry intrusion suppressed deep convection offshore in the latter half of the campaign, allowing the build‐up of low‐level humidity in the onshore flow and enhancing rainfall over the mountains. Rainfall on the lee side of the Western Ghats occurred during the latter half of the campaign in association with enhanced mesoscale easterly upslope flow. Diurnal cycles in rainfall offshore (maximum in the morning) and on the mountains (maximum in the afternoon) were observed. Considerable zonal and temporal variability was seen in the offshore boundary layer, suggesting the presence of convective downdraughts and cold pools. Persistent drying of the subcloud mixed layer several hundred kilometres off the coast was observed, suggesting strong mixing between the boundary layer and the free troposphere. These observations provide quantitative targets to test models and suggest hypotheses on the physical mechanisms determining the distribution and variability in rainfall in the Western Ghats region.},
doi = {10.1002/qj.3439},
journal = {Quarterly Journal of the Royal Meteorological Society},
number = 731,
volume = 146,
place = {United Kingdom},
year = {Sun Apr 07 00:00:00 EDT 2019},
month = {Sun Apr 07 00:00:00 EDT 2019}
}
https://doi.org/10.1002/qj.3439
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