Volume 39 Issue 4
Apr.  2020
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Qiong Wu, Xiaochun Wang, Wenhao Liang, Wenjun Zhang. Validation and application of soil moisture active passive sea surface salinity observation over the Changjiang River Estuary[J]. Acta Oceanologica Sinica, 2020, 39(4): 1-8. doi: 10.1007/s13131-020-1542-z
Citation: Qiong Wu, Xiaochun Wang, Wenhao Liang, Wenjun Zhang. Validation and application of soil moisture active passive sea surface salinity observation over the Changjiang River Estuary[J]. Acta Oceanologica Sinica, 2020, 39(4): 1-8. doi: 10.1007/s13131-020-1542-z

Validation and application of soil moisture active passive sea surface salinity observation over the Changjiang River Estuary

doi: 10.1007/s13131-020-1542-z
Funds:  The National Key Research and Development Program of China under contract No. 2016YFC1401600; the Public Science and Technology Research Fund Projects for Ocean Research under contract No. 201505003; the 2015 Jiangsu Program of Entrepreneurship and Innovation Group under contract No. 2191061503801/002.
More Information
  • Corresponding author: E-mail: xcwang@nuist.edu.cn
  • Received Date: 2019-04-19
  • Accepted Date: 2019-05-27
  • Available Online: 2020-12-28
  • Publish Date: 2020-04-25
  • Using sea surface salinity (SSS) observation from the soil moisture active passive (SMAP) mission, we analyzed the spatial distribution and seasonal variation of SSS around Changjiang River (Yangtze River) Estuary for the period of September 2015 to August 2018. First, we found that the SSS from SMAP is more accurate than soil moisture and ocean salinity (SMOS) mission observation when comparing with the in situ observations. Then, the SSS signature of the Changjiang River freshwater was analyzed using SMAP data and the river discharge data from the Datong hydrological station. The results show that the SSS around the Changjiang River Estuary is significantly lower than that of the open ocean, and shows significant seasonal variation. The minimum value of SSS appears in July and maximum SSS in December. The root mean square difference of daily SSS between SMAP observation and in situ observation is around 3 in both summer and winter, which is much lower than the annual range of SSS variation. In summer, the diffusion direction of the Changjiang River freshwater depicted by SSS from SMAP is consistent with the path of freshwater from in situ observation, suggesting that SMAP observation may be used in coastal seas in monitoring the diffusion and advection of freshwater discharge.
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  • [1]
    Bai Yan, He Xianqiang, Pan Delu, et al. 2014. Summertime Changjiang River plume variation during 1998–2010. Journal of Geophysical Research: Oceans, 119(9): 6238–6257. doi: 10.1002/2014JC009866
    [2]
    Bai Yan, Pan Delu, Cai Wenjun, et al. 2013. Remote sensing of salinity from satellite-derived CDOM in the Changjiang River dominated East China Sea. Journal of Geophysical Research: Oceans, 118(1): 227–243. doi: 10.1029/2012JC008467
    [3]
    Berger M, Camps A, Font J, et al. 2002. Measuring ocean salinity with ESA’s SMOS mission- advancing the science. ESA Bulletin-European Space Agency, (111): 113–121
    [4]
    Bingham F M, Foltz G R, McPhaden M J. 2011. Characteristics of the seasonal cycle of surface layer salinity in the global ocean. Ocean Science Discussions, 8(6): 2377–2415. doi: 10.5194/osd-8-2377-2011
    [5]
    Das N N, Entekhabi D, Njoku E G. 2011. An algorithm for merging SMAP radiometer and radar data for high-resolution soil-moisture retrieval. IEEE Transactions on Geoscience and Remote Sensing, 49(5): 1504–1512. doi: 10.1109/TGRS.2010.2089526
    [6]
    Dickson R R, Meincke J, Malmberg S A, et al. 1988. The “great salinity anomaly” in the northern North Atlantic 1968–1982. Progress in Oceanography, 20(2): 103–151. doi: 10.1016/0079-6611(88)90049-3
    [7]
    Durack P J, Wijffels S E. 2010. Fifty-year trends in global ocean salinities and their relationship to broad-scale warming. Journal of Climate, 23(16): 4342–4362. doi: 10.1175/2010JCLI3377.1
    [8]
    Entekhabi D, Das N, Yueh S, et al. 2014. SMAP Handbook Soil Moisture Active Passive: Mapping Soil Moisture and Freeze/Thaw from Space. Pasadena, CA: JPL Publication, 31–46
    [9]
    Entekhabi D, Njoku E G, O’Neill P E, et al. 2010. The soil moisture active passive (SMAP) mission. Proceedings of the IEEE, 98(5): 704–716. doi: 10.1109/JPROC.2010.2043918
    [10]
    Font J, Camps A, Borges A, et al. 2010. SMOS: the challenging sea surface salinity measurement from space. Proceedings of the IEEE, 98(5): 649–665. doi: 10.1109/JPROC.2009.2033096
    [11]
    Fournier S, Reager J T, Lee T, et al. 2016. SMAP observes flooding from land to sea: the Texas event of 2015. Geophysical Research Letters, 43(19): 10338–10346. doi: 10.1002/2016GL070821
    [12]
    Guimbard S, Reul N, Chapron B, et al. 2017. Seasonal and interannual variability of the Eastern Tropical Pacific Fresh Pool. Journal of Geophysical Research: Oceans, 122(3): 1749–1771. doi: 10.1002/2016JC012130
    [13]
    Hasson A, Puy M, Boutin J, et al. 2018. Northward pathway across the tropical North Pacific Ocean revealed by surface salinity: how do El Niño anomalies reach Hawaii?. Journal of Geophysical Research: Oceans, 123(4): 2697–2715. doi: 10.1002/2017JC013423
    [14]
    Kim K, Kim K R, Rhee T S, et al. 1991. Identification of water masses in the Yellow Sea and the East China Sea by cluster analysis. Elsevier Oceanography Series, 54: 253–267. doi: 10.1016/S0422-9894(08)70100-4
    [15]
    Lagerloef G, Colomb F R, Le Vine D, et al. 2008. The Aquarius/SAC-D mission: designed to meet the salinity remote-sensing challenge. Oceanography, 21(1): 68–81. doi: 10.5670/oceanog.2008.68
    [16]
    Le Vine D M, Lagerloef G S E, Colomb F R, et al. 2007. Aquarius: an instrument to monitor sea surface salinity from space. IEEE Transactions on Geoscience and Remote Sensing, 45(7): 2040–2050. doi: 10.1109/TGRS.2007.898092
    [17]
    Liu Baochao, Feng Licheng. 2012. An observational analysis of the relationship between wind and the expansion of the Changjiang River diluted water during summer. Atmospheric and Oceanic Science Letters, 5(5): 384–388. doi: 10.1080/16742834.2012.11447027
    [18]
    Mao H L, Kan T C, Lan Shufang. 1963. A preliminary study of the Yangtze diluted water and its mixing processes. Oceanologia et Limnologia Sinica (in Chinese), 5(3): 183–206
    [19]
    Subrahmanyam B, Murty V S N, Heffner D M. 2011. Sea surface salinity variability in the tropical Indian Ocean. Remote Sensing of Environment, 115(3): 944–956. doi: 10.1016/j.rse.2010.12.004
    [20]
    Xuan Jiliang, Huang Daji, Zhou Feng, et al. 2012. The role of wind on the detachment of low salinity water in the Changjiang Estuary in summer. Journal of Geophysical Research: Oceans, 117(C10): C10004. doi: 10.1029/2012jc008121
    [21]
    Yueh S, Fore A, Tang Wenqing, et al. 2016. Applications of SMAP data to retrieval of ocean surface wind and salinity. In: Proceedings of SPIE 9999, Remote Sensing of the Ocean, Sea Ice, Coastal Waters, and Large Water Regions 2016. Edinburgh, United Kingdom: SPIE,
    [22]
    Yueh S, Tang Wenqing, Fore A, et al. 2014. Aquarius geophysical model function and combined active passive algorithm for ocean surface salinity and wind retrieval. Journal of Geophysical Research: Oceans, 119(8): 5360–5379. doi: 10.1002/2014JC009939
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