Remote sensing of suspended sediment over Gulf of Martaban
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| collectionurl | https://intelek.unisza.edu.my/intelek/pages/search.php?search=!collection407072 |
| date | 2015-03-23 08:33:01 |
| format | Restricted Document |
| id | 11631 |
| institution | UniSZA |
| internalnotes | Acker, J.G. & Leptoukh G. (2007). Online analysis enhances use of NASA earth science data. Eos, Transactions American Geophysical Union, 88(2), 14−17. DOI: 10.1029/2007EO020003. Chen, Z., Hu, C. & Muller-Karger F. (2007). Monitoring turbidity in Tampa Bay using MODIS/Aqua 250-m imagery. Remote Sens. Environ., 109(2), 207−220. DOI: 10.1016/j.rse.2006.12.019. Chu, V.W., Smith, L.C., Rennermalm, A.K., Forster, R.R., Box, J.E. & Reehy N. (2009). Sediment plume response to surface melting and supraglacial lake drainages on the Greenland ice sheet. Journal of Glaciology, 55(194), 1072−1082. DOI: 10.3189/002214309790794904. Curran, P.J. & Novo E.M.M. (1988). The relationship between suspended sediment concentration and remotely sensed spectral radiance: a review. J. Coas. Res., 4(3), 351−368. URL: http://www.jstor.org/stable/4297423 Doxaran, D., Froidefond, J.M. & Castaing P. (2003). Remote-sensing reflectance of turbid sediment-dominated waters. Reduction of sediment type variations and changing illumination conditions effects by use of reflectance ratios. Applied Optics, 42(15), 2623−2634. http://www.opticsinfobase.org/ao/abstract.cfm?URI=ao-42-15-2623 Hadden, R.L. (2008).The Geology of Burma (Myanmar): An Annotated Bibliography of Burma’s Geology, Geography and Earth Science. Alexandria: Geospatial Information Library. Hedley, P. J., Bird, M.I. & Robinson R.A. (2010). Evolution of the Irrawaddy delta region since 1850.The Geographical Journal, 176(2), 138−149. DOI: 10.1111/j.1475-4959.2009.00346.x. Hu, C., Chen, Z., Clayton, T.D., Swarzenski, P., Brock, J.C. & Muller–Karger F.E. (2004). Assessment of estuarine water-quality indicators using MODIS medium-resolution bands: Initial results from Tampa Bay, FL. Remote Sens. Environ., 93(3), 423−441. DOI: 10.1016/j.rse.2004.08.007. Kirk, J.T.O. (1994). Light and photosynthesis in aquatic ecosystems. Cambridge: Cambridge University Press. Leptoukh, G., Cox, S., Farley, J., Gopalan, A., Mao, J. & Berrick S. (2007). Exploring NASA and ESA atmospheric data using Giovanni, the online visualization and analysis tool. ENVISATSymp., Montreux, Apr. 23−27, 2007. Long, C.M. & Pavelsky T. M. (2013). Remote sensing of suspended sediment concentration and hydrologic connec-tivity in a complex wetland environment. Remote Sens. Environ., 129, 197−209. DOI: 10.1016/j.rse.2012.10.019. Miller, R.L. & McKee B.A. (2004). Using MODIS Terra 250 m imagery to map concentrations of total suspended matter in coastal waters. Remote Sens. Environ., 93(1−2), 259−266. DOI: 10.1016/j.rse.2004.07.012. Mobley, C.D. & Mobley C.D. (1994). Light and water: Radiative transfer in natural waters (Vol. 592). San Diego: Academic Press. Moreno-Madrinan, M.J., Al-Hamdan, M.Z., Rickman, D.L. & Muller-Karger F.E. (2010). Using the surface reflectance MODIS Terra product to estimate turbidity in Tampa Bay, Florida. Remote Sensing, 2(12), 2713−2728. DOI: 10.3390/rs2122713. Pavelsky, T.M. & Smith L.C. (2009). Remote sensing of suspended sediment concentration, flow velocity, and lake re-charge in the Peace‐Athabasca Delta, Canada. Water Resources Research, 45(11). DOI: 10.1029/2008WR007424. Petus, C., Chust, G., Gohin, F., Doxaran, D., Froidefond, J.M. & Sagarminaga Y. (2010). Estimating turbidity and total suspended matter in the Adour River plume (South Bay of Biscay) using MODIS 250-m imagery. Continental Shelf Research, 30(5), 379−392. DOI: 10.1016/j.csr.2009.12.007. Ramaswamy, V., Rao, P.S., Rao, K.H., Thwin, S., Rao, N.S. & Raiker V. (2004). Tidal influence on suspended sediment distribution and dispersal in the northern Andaman Sea and Gulf of Martaban. Marine Geology, 208(1), 33−42. DOI: 10.1016/j.margeo.2004.04.019. Rao, P. S., Ramaswamy, V. & Thwin S. (2005). Sediment texture, distribution and transport on the Ayeyarwady con-tinental shelf, Andaman Sea. Marine Geology, 216(4), 239−247. DOI: 10.1016/j.margeo.2005.02.016. Ritchie, J.C., Schiebe, F.R. & McHenry J. (1976). Remote sensing of suspended sediments in surface waters. Photo-grammetric Engineering and Remote Sensing, 42(12), 1539−1545. Rizal, S., Damm, P., Wahid, M.A., Sundermann, J., Ilhamsyah, Y. & Iskandar T. (2012). General circulation in the Malacca strait and Andaman sea: a numerical model study. American Journal of Environmental Sciences, 8(5), 479−488. DOI: 10.3844/ajessp.2012.479.488. Robinson, R.A.J., Bird, M.I., Oo, N.W., Hoey, T.B., Aye, M.M., Higgitt, D.L. & Win S.L. (2007). The Irrawaddy River sediment flux to the Indian Ocean: the original nineteenth‐century data revisited.The Journal of Geology, 115(6), 629−640. DOI: 10.1086/521607. Rodolfo, K.S. (1969). Sediments of the Andaman basin, northeastern Indian Ocean. Marine Geology, 7(5), 371−402. DOI: 10.1016/0025-3227(69)90014-0. Rodríguez-Guzmán, V. & Gilbes-Santaella F. (2009). Using MODIS 250 m imagery to estimate total suspended sedi-ment in a tropical open bay. International Journal of Systems Applications Engineering and Development, 3(1), 36−44. Salomonson, V.V., Barnes, W., Maymon, P.W., Montgomery, H.E. & Ostrow H. (1989). MODIS: Advanced facility instrument for studies of the Earth as a system. Geoscience and Remote Sensing, IEEE Transactions on, 27(2), 145−153. DOI: 10.1109/36.20292. Wang, F., Zhou, B., Xu, J., Song, L. & Wang X. (2009). Application of neural network and MODIS 250 m imagery for estimating suspended sediments concentration in Hangzhou Bay, China. Environ. Geol., 56(6), 1093−1101. DOI: 10.1007/s00254-008-1209-0. Wyrtki, K. (1961). Physical oceanography of the southeast Asian waters. California: University of California |
| originalfilename | 5893-01-FH02-FIK-15-02672.jpg |
| person | UniSZA Unisza unisza |
| recordtype | oai_dc |
| resourceurl | https://intelek.unisza.edu.my/intelek/pages/view.php?ref=11631 |
| spelling | 11631 https://intelek.unisza.edu.my/intelek/pages/view.php?ref=11631 https://intelek.unisza.edu.my/intelek/pages/search.php?search=!collection407072 Restricted Document Article Journal UniSZA Unisza unisza image/jpeg inches 96 96 789 1422 60 60 2015-03-23 08:33:01 1422x789 5893-01-FH02-FIK-15-02672.jpg UniSZA Private Access Remote sensing of suspended sediment over Gulf of Martaban Ekologia Bratislava Gulf of Martaban is located at the north of Andaman, and is one of the world most turbid areas. e presence of suspended sediment concentration (SSC) in the water body could reduce the underwater transmittance. is study has been conducted to investigate the variation of SSC over the Gulf of Martaban. Remote sensing reectance (Rrs) of 667 nm is used as a proxy to represent the sediment SSC variation over the study area. e data for the period of July 2002 to March 2014 acquired from MODIS Aqua 4 km resolution are used in this study. As a result, there is no obvious yearly variation in the SSC cover area. e SSC variation over this study area is found to be sea-sonal. High homogenous SSC covers area observably during the northeast (NE) monsoon season that occurs from December to January. e sediment cover area could reach the latitude of 15°N that located at the south of the gulf. During southwest (SW) monsoon season that occurs from May to September, low and sparse SSC cover area is observed. As a consequence, the area covered by the SSC is higher during the NE monsoon season as compared to the SW monsoon season. Hence, the SSC cover area during the NE monsoon season is greater than the yearly averaged SSC cover area. Meanwhile the SSC cover area during the rainy SW monsoon season is less than the yearly and NE monsoon season. 34 1 54-64 Acker, J.G. & Leptoukh G. (2007). Online analysis enhances use of NASA earth science data. Eos, Transactions American Geophysical Union, 88(2), 14−17. DOI: 10.1029/2007EO020003. Chen, Z., Hu, C. & Muller-Karger F. (2007). Monitoring turbidity in Tampa Bay using MODIS/Aqua 250-m imagery. Remote Sens. Environ., 109(2), 207−220. DOI: 10.1016/j.rse.2006.12.019. Chu, V.W., Smith, L.C., Rennermalm, A.K., Forster, R.R., Box, J.E. & Reehy N. (2009). Sediment plume response to surface melting and supraglacial lake drainages on the Greenland ice sheet. Journal of Glaciology, 55(194), 1072−1082. DOI: 10.3189/002214309790794904. Curran, P.J. & Novo E.M.M. (1988). The relationship between suspended sediment concentration and remotely sensed spectral radiance: a review. J. Coas. Res., 4(3), 351−368. URL: http://www.jstor.org/stable/4297423 Doxaran, D., Froidefond, J.M. & Castaing P. (2003). Remote-sensing reflectance of turbid sediment-dominated waters. Reduction of sediment type variations and changing illumination conditions effects by use of reflectance ratios. Applied Optics, 42(15), 2623−2634. http://www.opticsinfobase.org/ao/abstract.cfm?URI=ao-42-15-2623 Hadden, R.L. (2008).The Geology of Burma (Myanmar): An Annotated Bibliography of Burma’s Geology, Geography and Earth Science. Alexandria: Geospatial Information Library. Hedley, P. J., Bird, M.I. & Robinson R.A. (2010). Evolution of the Irrawaddy delta region since 1850.The Geographical Journal, 176(2), 138−149. DOI: 10.1111/j.1475-4959.2009.00346.x. Hu, C., Chen, Z., Clayton, T.D., Swarzenski, P., Brock, J.C. & Muller–Karger F.E. (2004). Assessment of estuarine water-quality indicators using MODIS medium-resolution bands: Initial results from Tampa Bay, FL. Remote Sens. Environ., 93(3), 423−441. DOI: 10.1016/j.rse.2004.08.007. Kirk, J.T.O. (1994). Light and photosynthesis in aquatic ecosystems. Cambridge: Cambridge University Press. Leptoukh, G., Cox, S., Farley, J., Gopalan, A., Mao, J. & Berrick S. (2007). Exploring NASA and ESA atmospheric data using Giovanni, the online visualization and analysis tool. ENVISATSymp., Montreux, Apr. 23−27, 2007. Long, C.M. & Pavelsky T. M. (2013). Remote sensing of suspended sediment concentration and hydrologic connec-tivity in a complex wetland environment. Remote Sens. Environ., 129, 197−209. DOI: 10.1016/j.rse.2012.10.019. Miller, R.L. & McKee B.A. (2004). Using MODIS Terra 250 m imagery to map concentrations of total suspended matter in coastal waters. Remote Sens. Environ., 93(1−2), 259−266. DOI: 10.1016/j.rse.2004.07.012. Mobley, C.D. & Mobley C.D. (1994). Light and water: Radiative transfer in natural waters (Vol. 592). San Diego: Academic Press. Moreno-Madrinan, M.J., Al-Hamdan, M.Z., Rickman, D.L. & Muller-Karger F.E. (2010). Using the surface reflectance MODIS Terra product to estimate turbidity in Tampa Bay, Florida. Remote Sensing, 2(12), 2713−2728. DOI: 10.3390/rs2122713. Pavelsky, T.M. & Smith L.C. (2009). Remote sensing of suspended sediment concentration, flow velocity, and lake re-charge in the Peace‐Athabasca Delta, Canada. Water Resources Research, 45(11). DOI: 10.1029/2008WR007424. Petus, C., Chust, G., Gohin, F., Doxaran, D., Froidefond, J.M. & Sagarminaga Y. (2010). Estimating turbidity and total suspended matter in the Adour River plume (South Bay of Biscay) using MODIS 250-m imagery. Continental Shelf Research, 30(5), 379−392. DOI: 10.1016/j.csr.2009.12.007. Ramaswamy, V., Rao, P.S., Rao, K.H., Thwin, S., Rao, N.S. & Raiker V. (2004). Tidal influence on suspended sediment distribution and dispersal in the northern Andaman Sea and Gulf of Martaban. Marine Geology, 208(1), 33−42. DOI: 10.1016/j.margeo.2004.04.019. Rao, P. S., Ramaswamy, V. & Thwin S. (2005). Sediment texture, distribution and transport on the Ayeyarwady con-tinental shelf, Andaman Sea. Marine Geology, 216(4), 239−247. DOI: 10.1016/j.margeo.2005.02.016. Ritchie, J.C., Schiebe, F.R. & McHenry J. (1976). Remote sensing of suspended sediments in surface waters. Photo-grammetric Engineering and Remote Sensing, 42(12), 1539−1545. Rizal, S., Damm, P., Wahid, M.A., Sundermann, J., Ilhamsyah, Y. & Iskandar T. (2012). General circulation in the Malacca strait and Andaman sea: a numerical model study. American Journal of Environmental Sciences, 8(5), 479−488. DOI: 10.3844/ajessp.2012.479.488. Robinson, R.A.J., Bird, M.I., Oo, N.W., Hoey, T.B., Aye, M.M., Higgitt, D.L. & Win S.L. (2007). The Irrawaddy River sediment flux to the Indian Ocean: the original nineteenth‐century data revisited.The Journal of Geology, 115(6), 629−640. DOI: 10.1086/521607. Rodolfo, K.S. (1969). Sediments of the Andaman basin, northeastern Indian Ocean. Marine Geology, 7(5), 371−402. DOI: 10.1016/0025-3227(69)90014-0. Rodríguez-Guzmán, V. & Gilbes-Santaella F. (2009). Using MODIS 250 m imagery to estimate total suspended sedi-ment in a tropical open bay. International Journal of Systems Applications Engineering and Development, 3(1), 36−44. Salomonson, V.V., Barnes, W., Maymon, P.W., Montgomery, H.E. & Ostrow H. (1989). MODIS: Advanced facility instrument for studies of the Earth as a system. Geoscience and Remote Sensing, IEEE Transactions on, 27(2), 145−153. DOI: 10.1109/36.20292. Wang, F., Zhou, B., Xu, J., Song, L. & Wang X. (2009). Application of neural network and MODIS 250 m imagery for estimating suspended sediments concentration in Hangzhou Bay, China. Environ. Geol., 56(6), 1093−1101. DOI: 10.1007/s00254-008-1209-0. Wyrtki, K. (1961). Physical oceanography of the southeast Asian waters. California: University of California |
| spellingShingle | Remote sensing of suspended sediment over Gulf of Martaban |
| summary | Gulf of Martaban is located at the north of Andaman, and is one of the world most turbid areas. e presence of suspended sediment concentration (SSC) in the water body could reduce the underwater transmittance. is study has been conducted to investigate the variation of SSC over the Gulf of Martaban. Remote sensing reectance (Rrs) of 667 nm is used as a proxy to represent the sediment SSC variation over the study area. e data for the period of July 2002 to March 2014 acquired from MODIS Aqua 4 km resolution are used in this study. As a result, there is no obvious yearly variation in the SSC cover area. e SSC variation over this study area is found to be sea-sonal. High homogenous SSC covers area observably during the northeast (NE) monsoon season that occurs from December to January. e sediment cover area could reach the latitude of 15°N that located at the south of the gulf. During southwest (SW) monsoon season that occurs from May to September, low and sparse SSC cover area is observed. As a consequence, the area covered by the SSC is higher during the NE monsoon season as compared to the SW monsoon season. Hence, the SSC cover area during the NE monsoon season is greater than the yearly averaged SSC cover area. Meanwhile the SSC cover area during the rainy SW monsoon season is less than the yearly and NE monsoon season. |
| title | Remote sensing of suspended sediment over Gulf of Martaban |
| title_full | Remote sensing of suspended sediment over Gulf of Martaban |
| title_fullStr | Remote sensing of suspended sediment over Gulf of Martaban |
| title_full_unstemmed | Remote sensing of suspended sediment over Gulf of Martaban |
| title_short | Remote sensing of suspended sediment over Gulf of Martaban |
| title_sort | remote sensing of suspended sediment over gulf of martaban |