## Abstract A 70‐year record of daily monsoon‐season rainfall at a network of 13 stations in central western India is analyzed using a 4‐state homogeneous hidden Markov model. The diagnosed states are seen to play distinct roles in the seasonal march of the monsoon, can be associated with ‘active’
Downscaling projections of Indian monsoon rainfall using a non-homogeneous hidden Markov model
✍ Scribed by Arthur M. Greene; Andrew W. Robertson; Padhraic Smyth; Scott Triglia
- Publisher
- John Wiley and Sons
- Year
- 2011
- Tongue
- English
- Weight
- 412 KB
- Volume
- 137
- Category
- Article
- ISSN
- 0035-9009
- DOI
- 10.1002/qj.788
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✦ Synopsis
Abstract
Downscaled rainfall projections for the Indian summer monsoon are generated using a non‐homogeneous hidden Markov model (NHMM) and information from both a dense observational dataset and an ensemble of general circulation models (GCMs). The projections are conditioned on two types of GCM information, corresponding approximately to dynamic and thermodynamic components of precipitation change. These have opposing effects, with a weakening circulation compensating not quite half of the regional precipitation increase that might otherwise be expected. GCM information is taken at the largest spatial scales consistent with regional physics and modelling constraints, while the NHMM produces a disaggregation consistent with the observed fine‐scale spatiotemporal variability. Projections are generated using multimodel mean predictors, with intermodel dispersion providing a measure of the uncertainty due to GCM differences. The downscaled simulations exhibit small increases in the number of dry days, in the average length of dry spells, in mean daily intensity and in the exceedance frequency of nearly all daily rainfall percentiles. Copyright © 2011 Royal Meteorological Society
📜 SIMILAR VOLUMES
In attempting to model the random behaviour of the Indian summer monsoon, the possibility of using a generalized four-parameter Kappa distribution representing a family of distributions has been explored. An L-Moment procedure developed by Hosking (1994) IBM J. Res. De6., 38(3), 251 -258, has been u