Prognostic and Diagnostic Modes of Mathematical Model for the Pre-operation of Suspended Sediment Transport model in Estuaries and Coastal areas
Both prognostic and diagnostic modes of a 3D baroclinic
model in hydrodynamic and sediment transport models of
the Princeton Ocean Model (POM) were conducted to separate
prognose and diagnose effects of different hydrodynamic factors on
transport of suspended sediment discharged from the rivers to the
Gulf of Thailand (GoT). Both transport modes of suspended sediment
distribution in the GoT were numerically simulated. It could be
concluded that the suspended sediment discharged from the rivers
around the GoT. Most of sediments in estuaries and coastal areas are
deposited outside the GoT under the condition of wind-driven current,
and very small amount of the sediments of them are transported
faraway. On the basis of wind forcing, sediments from the lower
GoT to the upper GoT are mainly transported south-northwestward
and also continuously moved north-southwestward. An obvious 3D
characteristic of suspended sediment transport is produced in the
wind-driven current residual circulation condition. In this study, the
transport patterns at the third layer are generally consistent with
the typhoon-induced strong currents in two case studies of Typhoon
Linda 1997. The case studies presented the prognostic and diagnostic
modes during 00UTC28OCT1997 to 12UTC06NOV1997 in a short
period with the current condition for pre-operation of the suspended
sediment transport model in estuaries and coastal areas.
[1] A. F. Blumberg and G. L. Mellor, "A description of a threedimensional
coastal ocean circulation model, In N. S. Heaps, editor, Three-
dimensional coastal ocean models," Coastal and estuarine sciences,
American Geophysical Union, vol. 4, pp. 1-16, 1987.
[2] G. L. Mellor, "An Equation of State for Numerical Models of Oceans
and Estuaries," Journal of Atmospheric and Oceanic Technology, vol. 8,
pp. 609-611, 1991.
[3] K. F. Bowden, Physical Oceanography of Coastal Waters, Ellis Horwood,
Southampton, UK, 1983.
[4] C. Amante and B. W. Eakins, 1 ArcMinute Global Relief Model:
Procedures, Data Sources and Analysis (ETOPO1), NOAA, National
Geophysical Data Center, Boulder, Colorado, USA, 2008.
[5] P. Harr, R. Ellsberry, T. Hogan and W. Clune, "North Pacific cyclone
sea-level pressure errors with NOGAPS," Weather and Forecasting, vol.
7, pp. 3-4, 1992.
[6] S. Levitus, R. Burgett and T. Boyer, World Ocean Atlas: Salinity, NOAA
Atlas NESDIS 3, U. S. Government Printing Office, Washington DC,
USA, vol.3, 1994.
[7] S. Levitus and T. Boyer, World Ocean Atlas: Temperature, NOAA Atlas
NESDIS 4, U. S. Government Printing Office, Washington DC, USA, ,
vol.4, 1994.
[8] T. D. Pugh, Tides, Surges and Mean Sea-Level, a handbook for engineers
and scientists, Chichester: John Wiley & Sons Inc., London, UK, 1987.
[9] T. F. Hogan and T. E. Rosmond, "The description of the Navy Operational
Global Atmospheric System-s spectral forecast model," Monthly
Weather Review, vol. 119, pp. 1786-1815, 1991.
[10] W. Wannawong, U. W. Humphries and A. Luadsong, "The application
of curvilinear coordinate for primitive equation in the Gulf of Thailand,"
Thai Journal of Mathematics, vol. 6, pp. 89-108, 2008.
[11] W. Wannawong, U. W. Humphries and P. Wongwises, "Optimization
of bathymetry database for coastal areas," Journal of Mathematics and
Statistics, vol. 6, pp. 286-293, 2010.
[12] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "A two-dimensional wave prediction model along
the best track of Typhoon Linda 1997," American Journal of Environmental
Sciences, vol. 6, pp. 280-285, 2010.
[13] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "A numerical study of two coordinates for energy
balance equations by wave model," Thai Journal of Mathematics, vol.
8, pp. 197-214, 2010.
[14] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "Numerical analysis of wave and hydrodynamic
models for energy balance and primitive equations," International Journal
of Mathematical and Statistical Sciences, vol. 4, pp. 140-150, 2010.
[15] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "Numerical modeling and computation of storm
surge for primitive equation by hydrodynamic model," Thai Journal of
Mathematics, vol. 8, pp. 347-363, 2010.
[16] W. Wannawong, U. W. Humphries and P. Wongwises, "A study of temperature
and salinity changes of seawater by mathematical modeling,"
American-Eurasian Journal of Agricultural and Environmental Science,
vol. 4, pp. 446-451, 2010.
[17] W. Wannawong, U. W. Humphries, P. Wongwises and S. Vongvisessomjai,
"Mathematical modeling of storm surge in three dimensional
primitive equations," International Journal of Computational and Mathematical
Sciences, vol. 1, pp. 44-53, 2011.
[18] W. Wannawong, U. W. Humphries, P. Wongwises and S. Vongvisessomjai,
"Three steps of one-way nested grid for energy balance equation by
wave model," International Journal of Computational and Mathematical
Sciences, vol. 1, pp. 23-30, 2011.
[19] W. Wannawong, P. Wongwises, P. Ekphisutsuntorn, C. Ekkawatpanit and
U. W. Humphries, "Numerical study of the effect of wind-waves generated
by tropical cyclones using wave model: Storm surge and waves,
Solutions to coastal disasters," American Society of Civil Engineers
(ASCE), vol. 1, pp. 149-163, 2011.
[1] A. F. Blumberg and G. L. Mellor, "A description of a threedimensional
coastal ocean circulation model, In N. S. Heaps, editor, Three-
dimensional coastal ocean models," Coastal and estuarine sciences,
American Geophysical Union, vol. 4, pp. 1-16, 1987.
[2] G. L. Mellor, "An Equation of State for Numerical Models of Oceans
and Estuaries," Journal of Atmospheric and Oceanic Technology, vol. 8,
pp. 609-611, 1991.
[3] K. F. Bowden, Physical Oceanography of Coastal Waters, Ellis Horwood,
Southampton, UK, 1983.
[4] C. Amante and B. W. Eakins, 1 ArcMinute Global Relief Model:
Procedures, Data Sources and Analysis (ETOPO1), NOAA, National
Geophysical Data Center, Boulder, Colorado, USA, 2008.
[5] P. Harr, R. Ellsberry, T. Hogan and W. Clune, "North Pacific cyclone
sea-level pressure errors with NOGAPS," Weather and Forecasting, vol.
7, pp. 3-4, 1992.
[6] S. Levitus, R. Burgett and T. Boyer, World Ocean Atlas: Salinity, NOAA
Atlas NESDIS 3, U. S. Government Printing Office, Washington DC,
USA, vol.3, 1994.
[7] S. Levitus and T. Boyer, World Ocean Atlas: Temperature, NOAA Atlas
NESDIS 4, U. S. Government Printing Office, Washington DC, USA, ,
vol.4, 1994.
[8] T. D. Pugh, Tides, Surges and Mean Sea-Level, a handbook for engineers
and scientists, Chichester: John Wiley & Sons Inc., London, UK, 1987.
[9] T. F. Hogan and T. E. Rosmond, "The description of the Navy Operational
Global Atmospheric System-s spectral forecast model," Monthly
Weather Review, vol. 119, pp. 1786-1815, 1991.
[10] W. Wannawong, U. W. Humphries and A. Luadsong, "The application
of curvilinear coordinate for primitive equation in the Gulf of Thailand,"
Thai Journal of Mathematics, vol. 6, pp. 89-108, 2008.
[11] W. Wannawong, U. W. Humphries and P. Wongwises, "Optimization
of bathymetry database for coastal areas," Journal of Mathematics and
Statistics, vol. 6, pp. 286-293, 2010.
[12] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "A two-dimensional wave prediction model along
the best track of Typhoon Linda 1997," American Journal of Environmental
Sciences, vol. 6, pp. 280-285, 2010.
[13] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "A numerical study of two coordinates for energy
balance equations by wave model," Thai Journal of Mathematics, vol.
8, pp. 197-214, 2010.
[14] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "Numerical analysis of wave and hydrodynamic
models for energy balance and primitive equations," International Journal
of Mathematical and Statistical Sciences, vol. 4, pp. 140-150, 2010.
[15] W. Wannawong, U. W. Humphries, P. Wongwises, S. Vongvisessomjai
and W. Lueangaram, "Numerical modeling and computation of storm
surge for primitive equation by hydrodynamic model," Thai Journal of
Mathematics, vol. 8, pp. 347-363, 2010.
[16] W. Wannawong, U. W. Humphries and P. Wongwises, "A study of temperature
and salinity changes of seawater by mathematical modeling,"
American-Eurasian Journal of Agricultural and Environmental Science,
vol. 4, pp. 446-451, 2010.
[17] W. Wannawong, U. W. Humphries, P. Wongwises and S. Vongvisessomjai,
"Mathematical modeling of storm surge in three dimensional
primitive equations," International Journal of Computational and Mathematical
Sciences, vol. 1, pp. 44-53, 2011.
[18] W. Wannawong, U. W. Humphries, P. Wongwises and S. Vongvisessomjai,
"Three steps of one-way nested grid for energy balance equation by
wave model," International Journal of Computational and Mathematical
Sciences, vol. 1, pp. 23-30, 2011.
[19] W. Wannawong, P. Wongwises, P. Ekphisutsuntorn, C. Ekkawatpanit and
U. W. Humphries, "Numerical study of the effect of wind-waves generated
by tropical cyclones using wave model: Storm surge and waves,
Solutions to coastal disasters," American Society of Civil Engineers
(ASCE), vol. 1, pp. 149-163, 2011.
@article{"International Journal of Architectural, Civil and Construction Sciences:63065", author = "Worachat Wannawong and Chaiwat Ekkawatpanit and Sanit Wongsa", title = "Prognostic and Diagnostic Modes of Mathematical Model for the Pre-operation of Suspended Sediment Transport model in Estuaries and Coastal areas", abstract = "Both prognostic and diagnostic modes of a 3D baroclinic
model in hydrodynamic and sediment transport models of
the Princeton Ocean Model (POM) were conducted to separate
prognose and diagnose effects of different hydrodynamic factors on
transport of suspended sediment discharged from the rivers to the
Gulf of Thailand (GoT). Both transport modes of suspended sediment
distribution in the GoT were numerically simulated. It could be
concluded that the suspended sediment discharged from the rivers
around the GoT. Most of sediments in estuaries and coastal areas are
deposited outside the GoT under the condition of wind-driven current,
and very small amount of the sediments of them are transported
faraway. On the basis of wind forcing, sediments from the lower
GoT to the upper GoT are mainly transported south-northwestward
and also continuously moved north-southwestward. An obvious 3D
characteristic of suspended sediment transport is produced in the
wind-driven current residual circulation condition. In this study, the
transport patterns at the third layer are generally consistent with
the typhoon-induced strong currents in two case studies of Typhoon
Linda 1997. The case studies presented the prognostic and diagnostic
modes during 00UTC28OCT1997 to 12UTC06NOV1997 in a short
period with the current condition for pre-operation of the suspended
sediment transport model in estuaries and coastal areas.", keywords = "prognostic, diagnostic, baroclinic, sediment transport,
estuaries.", volume = "5", number = "12", pages = "763-11", }