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A moist-thermal quasigeostrophic model for monsoon depressions
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dc.contributor.author | Chaudhri, Alexander K. | |
dc.contributor.author | Byrne, Michael P. | |
dc.contributor.author | Scott, Richard K. | |
dc.date.accessioned | 2024-04-17T16:30:03Z | |
dc.date.available | 2024-04-17T16:30:03Z | |
dc.date.issued | 2024-03-31 | |
dc.identifier | 300254199 | |
dc.identifier | 2aa0a61a-c328-48fb-bd6b-f21b942489b2 | |
dc.identifier | 85189643084 | |
dc.identifier.citation | Chaudhri , A K , Byrne , M P & Scott , R K 2024 , ' A moist-thermal quasigeostrophic model for monsoon depressions ' , Quarterly Journal of the Royal Meteorological Society , vol. Early View . https://doi.org/10.1002/qj.4723 | en |
dc.identifier.issn | 0035-9009 | |
dc.identifier.other | ORCID: /0000-0001-5624-5128/work/157140224 | |
dc.identifier.other | ORCID: /0000-0001-9019-3915/work/157141120 | |
dc.identifier.uri | https://hdl.handle.net/10023/29706 | |
dc.description | Funding: AKC is supported by a St Leonard’s College Interdisciplinary Doctoral Scholarship awarded by the University of St Andrews. | en |
dc.description.abstract | Monsoon depressions (MDs) are synoptic-scale storms that occur during the summer phase of the global monsoon cycle and whose dynamical mechanisms remain incompletely understood. To gain insight into the dynamics governing the large-scale structure of MDs, we formulate an idealised moist-thermal quasi-geostrophic model that includes distinct thermal and moisture fields in simple forms. A linear-stability analysis of the model, with basic states corresponding to typical monsoon conditions, shows three distinct mode classifications: thermal-Rossby modes, heavy precipitating modes, and a moist-thermal mode. In the linearised model, the presence of a background precipitation gradient strengthens thermal-Rossby modes by coupling the dynamics to latent heating. The separation of heavy precipitating modes from fast-propagating thermal-Rossby modes is further examined with numerical experiments of large-amplitude MDs. Wind-induced evaporation is found to amplify large-amplitude MDs in conditions analogous to those over the northern Bay of Bengal. An energetic analysis shows the pathways by which the MDs derive energy from the background state. A further series of experiments through a continuum of meridional temperature gradients demonstrates the sensitivity of large-scale MD dynamics to the background state and suggests a possible mechanism to explain variations in the propagation direction of MDs. | |
dc.format.extent | 20 | |
dc.format.extent | 3783114 | |
dc.language.iso | eng | |
dc.relation.ispartof | Quarterly Journal of the Royal Meteorological Society | en |
dc.subject | Idealised modelling | en |
dc.subject | Moist-thermal quasi-gestrophic dynamics | en |
dc.subject | Monsoon depressions | en |
dc.subject | GB Physical geography | en |
dc.subject | RR-NDAS | en |
dc.subject.lcc | GB | en |
dc.title | A moist-thermal quasigeostrophic model for monsoon depressions | en |
dc.type | Journal article | en |
dc.contributor.institution | University of St Andrews. School of Earth & Environmental Sciences | en |
dc.contributor.institution | University of St Andrews. Centre for Energy Ethics | en |
dc.contributor.institution | University of St Andrews. Applied Mathematics | en |
dc.identifier.doi | 10.1002/qj.4723 | |
dc.description.status | Peer reviewed | en |
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