Book contents
- Frontmatter
- Contents
- Contributors
- Editors' preface
- Keynote address to the 1977 Symposium SIR JAMES LIGHTHILL
- Part I The large-scale climatology of the tropical atmosphere
- Part II The summer monsoon over the Indian subcontinent and East Africa
- Part III The physics and dynamics of the Indian Ocean during the summer monsoon
- 29 Observations of the Somali Current and its relationship to the monsoon winds
- 30 Structure of currents and hydrographic conditions in the western equatorial Indian Ocean during the summer monsoon
- 31 Recent observations in the equatorial Indian Ocean
- 32 Sea temperature variations in the northeastern Arabian Sea in relation to the southwest monsoon
- 33 Heat budget of the north Indian oceanic surface during MONSOON-77
- 34 The energy budget at selected stations over the north Indian Ocean during MONSOON-77
- 35 Observations of coastal-water upwelling around India
- 36 A numerical study of surface cooling processes during summer in the Arabian Sea
- 37 Maximum simplification of nonlinear Somali Current dynamics
- 38 Laboratory modelling of the oceanic response to monsoonal winds
- Part IV Some important mathematical modelling techniques
- Part V Storm surges and flood forecasting
- Index
30 - Structure of currents and hydrographic conditions in the western equatorial Indian Ocean during the summer monsoon
Published online by Cambridge University Press: 05 November 2011
- Frontmatter
- Contents
- Contributors
- Editors' preface
- Keynote address to the 1977 Symposium SIR JAMES LIGHTHILL
- Part I The large-scale climatology of the tropical atmosphere
- Part II The summer monsoon over the Indian subcontinent and East Africa
- Part III The physics and dynamics of the Indian Ocean during the summer monsoon
- 29 Observations of the Somali Current and its relationship to the monsoon winds
- 30 Structure of currents and hydrographic conditions in the western equatorial Indian Ocean during the summer monsoon
- 31 Recent observations in the equatorial Indian Ocean
- 32 Sea temperature variations in the northeastern Arabian Sea in relation to the southwest monsoon
- 33 Heat budget of the north Indian oceanic surface during MONSOON-77
- 34 The energy budget at selected stations over the north Indian Ocean during MONSOON-77
- 35 Observations of coastal-water upwelling around India
- 36 A numerical study of surface cooling processes during summer in the Arabian Sea
- 37 Maximum simplification of nonlinear Somali Current dynamics
- 38 Laboratory modelling of the oceanic response to monsoonal winds
- Part IV Some important mathematical modelling techniques
- Part V Storm surges and flood forecasting
- Index
Summary
This chapter presents the results of studies on the currents and hydrography of the waters of the western equatorial Indian Ocean during the period 28 May to 3 June 1973. Studies of hydrographic conditions in the area after about one month (i.e. 25 June to 2 July 1973) are also discussed. Time-series data on horizontal currents were gathered by recording current meters attached to a buoy anchored at the Equator near 60° E during the Indo-Soviet Monsoon Experiment 1973. Hydrographic data were also obtained from repeated Nansen casts at 3-hourly intervals around the buoy. The time variation of currents (3-hour averages) at different depths (75 m, 100 m, 150 m, 200 m, 300 m, 500 m and 800 m) and the vertical time sections of temperature, salinity and density from the surface to 1000 m depth are presented and discussed.
The studies show a complex vertical structure of horizontal currents with predominant easterly components at 75 m and 100 m depth and predominant westerly components at 200 m, 300 m, 500 m and 800 m depth, and a zone of strong current shear between 100 m and 200 m depth. At 150 m depth, the current has been found to be oscillatory with a period of oscillation of about 2 hours. The currents are rather strong even at deeper levels, particularly at 200 m and 800 m depths where westward jets with speeds of the order of 0.35 m s-1 and 0.4 m s-1 respectively have been encountered. […]
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- Monsoon Dynamics , pp. 453 - 464Publisher: Cambridge University PressPrint publication year: 1981