Chebusev coefficients of thermohaline structure in the sea region of Central Vietnam
From the multi-daily observations of temperature and salinity at some stations in the sea region of Central Vietnam we recognize that: the vertical thermohaline structure may be approximated by polynom of Chebusev. The calculated results, based on the real data of temperature and salinity collected by the “Bien Dong Regular Survey Project” in summers of 2000 and 2001, have shown that: quantity of cases, in which error between calculated and observed data is less than 0.1C and 0.1‰, make up more than 93% of all observations. The polynomial coefficient A0 is the average field of thermohaline structure and A1 is a vertical mean gradient of temperature and salinity of the research station. This method may be used for data processing, schematizing, modelling and forecasting in oceanography.
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| Format: | Journal Contribution biblioteca |
| Language: | English |
| Published: |
2002
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| Subjects: | Thermohaline structure, Chebusev coefficient, |
| Online Access: | http://hdl.handle.net/1834/9249 |
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| Summary: | From the multi-daily observations of temperature and salinity at some
stations in the sea region of Central Vietnam we recognize that: the vertical
thermohaline structure may be approximated by polynom of Chebusev. The
calculated results, based on the real data of temperature and salinity
collected by the “Bien Dong Regular Survey Project” in summers of 2000 and
2001, have shown that: quantity of cases, in which error between calculated
and observed data is less than 0.1C and 0.1‰, make up more than 93% of
all observations. The polynomial coefficient A0 is the average field of
thermohaline structure and A1 is a vertical mean gradient of temperature and
salinity of the research station. This method may be used for data processing,
schematizing, modelling and forecasting in oceanography. |
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