数据说明
EIO-WPO-SCS Total Suspended Matter (TSM)
上传时间：2019-05-22 14:01:57 浏览次数：作者与来源：admin
East India Ocean Total Suspended Matter (TSM)
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For East India Ocean, the regional scope is 80ºE ~118ºE、10ºS~21ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_EIO
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_EIO_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
West Pacific Total Suspended Matter (TSM)
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For West Pacific, the regional scope is 121ºE~160ºE, 2ºS~46ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_WPO
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_WPO_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
South China Sea Total Suspended Matter (TSM)
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For South China Sea, the regional scope is 98ºE~127ºE, 0~25ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_SCS
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_SCS_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For East India Ocean, the regional scope is 80ºE ~118ºE、10ºS~21ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_EIO
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_EIO_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
West Pacific Total Suspended Matter (TSM)
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For West Pacific, the regional scope is 121ºE~160ºE, 2ºS~46ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_WPO
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_WPO_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
South China Sea Total Suspended Matter (TSM)
Combining China's HY-1B and EOS/MODIS data to achieve daily average, ten-day average and monthly average products, total suspended matter, chlorophyll a concentration and secchi disk depth were produced. The duration of data is from May 30, 2010 to May 30, 2015, with the period of daily, 10-day and monthly. The scopes of the data include East India Ocean, West Pacific and South China Sea.
For South China Sea, the regional scope is 98ºE~127ºE, 0~25ºN.
It is the fusion product of the TSM retrieved by HY-1B and EOS/MODIS.
Unit: mg/l
Resolution: 1.8km
Duration: May 30, 2010 - May 30, 2015
Source: HY-1B L1 data are from the satellite ground station and the satellite data processing & sharing center of SOED/SIO. EOS/MODIS L2 data are from the NASA’s Ocean Biology Processing Group (OBPG) via site https://oceancolor.gsfc.nasa.gov/.
Version: 2018
Dataset Name: SIO_SAT_SENSOR_SCS
Product Name: SIO_SAT_SENSOR_yyyy-MM-ddTOyyyy-MM-dd_L3B_SCS_1KM_SSC_HE2016
Processing:
For coastal water, we retrieve TSM based on the retrieved normalized water-leaving radiance (or remote sensing reflectance, Rrs), the TSM was estimated using the empirical model developed by He et al. (2013).
Tassan model (1993) was used to deal with the inversion in low turbidity waters in the ocean and shelf.
Known Issues:
Reference
Xianqiang He, Yan Bai, Delu Pan, Qiankun Zhu. The atmospheric correction HY-1B/COCTS, Proc. SPIE, 2008,7147:714717. DOI: 10.1117/12.813244.
Yan Bai, Lianghong Jiang, Xianqiang He, Vittorio Barale. An introduction to optical remote sensing of the Asian Seas: Chinese dedicated satellite s and data processing techniques. Remote Sensing of the Asian Seas, Edited by V. Barale and M. Gade, Springer, 2019,61-79. DOI:10.1007/978-3-319-94067-0_3
Tassan, S. An Improved In-Water Algorithm for the Determination of Chlorophyll and Suspended Sediment Concentration from Thematic Mapper Data in Coastal Waters. International Journal of Remote Sensing - INT J REMOTE SENS. 1993,14: 1221-1229.
Acknowledgment
Please cite the above references if this dataset is used. Moreover, the satellite ground station and the satellite data processing & sharing center of the SOED/SIO should be acknowledged.
