Dynamic and thermodynamic characteristics of the Asian summer monsoon during the onset phase over the Indian Peninsula (Kerala coast) and its variability are examined with reanalysis data sets. For this study, daily averaged (0000 and 1200 UTC) reanalysis data sets of National Centre for Environment
On the northward advance of the Itcz and the onset of the southwest monsoon rains over the southeast Bay of Bengal
β Scribed by Ananthakrishnan, R. ;Pathan, J. M. ;Aralikatti, S. S.
- Publisher
- Wiley (John Wiley & Sons)
- Year
- 1981
- Weight
- 708 KB
- Volume
- 1
- Category
- Article
- ISSN
- 2314-6214
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
The pentad rainfall data of six stations in the AndamanβNicobar group of islands for the period 1953β1978 have been analysed to study the northward advance of the ITCZ and the onset of the summer monsoon rainfall over the southeast Bay of Bengal. It is found that at the island stations south of 10Β°N the summer monsoon rains set in on the average towards the end of April which is a month in advance of the onset of the monsoon over the south Kerala coast of peninsular India. At the island stations to the north of 10Β°N the onset occurs about the first week of May. These dates are ahead of those shown in the existing diagrams giving the average onset dates of the summer monsoon over the southeast Bay of Bengal. Examination of the frequency and latitude of formation of cyclonic disturbances in the Bay of Bengal and the progressive seasonal variations of the tropospheric winds over the aerological station of Port Blair during AprilβMay lend support to the earlier onset dates.
π SIMILAR VOLUMES
Utilising daily mean rainfall from dense rain gauge networks, the dates of onset of the southwest monsoon over south and north Kerala have been derived on the basis of objective criteria for the years 1901 to 1980. These dates have been compared with the onset dates as per records of the India Meteo
Eight pentads before the monsoon onset over Kerala (MOK), a spatially large area of deep convection formed near the equator south of the Bay of Bengal, which moved to Southeast Asia marking the onset of the South China Sea monsoon (SCSM) for many years. Three pentads before MOK, a similar area of co
## Abstract Moisture fields derived from the TirosβN Operational Vertical Sounder (TOVS) data onboard previous National Oceanic and Atmospheric Administration (NOAA) series of satellites have been used to study monthly moisture fields over the Arabian Sea and the Bay of Bengal for the years 1979β19
## Abstract Utilizing 40 (1941β1980) years of daily monsoon rainfall data averaged over 52, 2.5Β° Γ 2.5Β° latitude and longitude contiguous blocks covering the whole of India, we have investigated the relationship between monsoon onset at nine locations in India with the monsoon rainfall during the f