Mean characteristics of the rainfall forecasts produced by the global data analysis -forecast system of India are examined for the summer monsoons of 1993-1996. Further, daily rainfall forecasts (accumulated for 24 h) extending from day 1 to day 5 are utilised to compute monthly/seasonal mean foreca
Seasonal forecasting of Thailand summer monsoon rainfall
β Scribed by Nkrintra Singhrattna; Balaji Rajagopalan; Martyn Clark; K. Krishna Kumar
- Publisher
- John Wiley and Sons
- Year
- 2005
- Tongue
- English
- Weight
- 339 KB
- Volume
- 25
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.1144
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β¦ Synopsis
This paper describes the development of a statistical forecasting method for summer monsoon rainfall over Thailand. Predictors of Thailand summer (August-October) monsoon rainfall are identified from the large-scale ocean-atmospheric circulation variables (i.e. sea-surface temperature and sea-level pressure) in the Indo-Pacific region. The predictors identified are part of the broader El NiΓ±o southern oscillation (ENSO) phenomenon. The predictors exhibit a significant relationship with the summer rainfall only during the post-1980 period, when the Thailand summer rainfall also shows a relationship with ENSO. Two methods for generating ensemble forecasts are adapted. The first is the traditional linear regression, and the second is a local polynomial-based nonparametric method. The associated predictive standard errors are used for generating ensembles. Both the methods exhibit significant comparable skills in a cross-validated mode. However, the nonparametric method shows improved skill during extreme years (i.e. wet and dry years). Furthermore, the models provide useful skill at 1-3 month lead time that can have a strong impact on resources planning and management.
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Association between the all-India summer monsoon (June to September) rainfall and an index of the Southern Oscillation (SO) is studied in relation to the vagaries of the monsoon rainfall and the seasonal characteristics of the SO. The Southern Oscillation index (SOI) used is the difference of normal
## Abstract In this study, 20 years (1961β1980) of rainfall data for 34 stations over Thailand are used to investigate and understand the intraseasonal and interannual variability of the summer monsoon. Dominant structures of 5βday and seasonal rainfall are determined through empirical orthogonal f
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