2012
DOI: 10.1016/j.csr.2011.11.010
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Evidence for submarine groundwater discharge on the Southwestern shelf of Taiwan

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Cited by 9 publications
(8 citation statements)
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“…In the vicinity of the SG seepage (marked by solid squared in Figure 1), CTD measurements revealed salinity inversions on profiles in the 2 m bottom layer (Figure 2(b)), where the magnitude of the salinity drop reached 0.06 psu. For such salinity drop, the SGD rate, as was estimated by [21], should be in range between 0.1 and 1 gm -2 •s -1 . The estimation was based on the advection-diffusion balance of salinity in the water column affected groundwater inflow,…”
Section: Study Regionmentioning
confidence: 96%
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“…In the vicinity of the SG seepage (marked by solid squared in Figure 1), CTD measurements revealed salinity inversions on profiles in the 2 m bottom layer (Figure 2(b)), where the magnitude of the salinity drop reached 0.06 psu. For such salinity drop, the SGD rate, as was estimated by [21], should be in range between 0.1 and 1 gm -2 •s -1 . The estimation was based on the advection-diffusion balance of salinity in the water column affected groundwater inflow,…”
Section: Study Regionmentioning
confidence: 96%
“…The deviation of vertical velocity and magnitude of the SGD rate, obtained by [21], is associated with variations of and S  H  estimated from field experiments. Besides uncertainties in estimation of and S  H  the rate, Q, depends on vertical diffusivity, K z , which was chosen from general assumptions.…”
Section: Study Regionmentioning
confidence: 97%
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