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b Geometries of the upper boundary of the PHS.
A lower temperature of the upper boundary can also lead to an apparent increase in the total volumetric water content.
The thin solid curves are the isodepth contours of the upper boundary surface for the descending Philippine Sea plate.
Therefore, the depth of the upper boundary of slab in the offshore areas was estimated using the OBS models.
Depths, strikes, and dips of subsources were adjusted to the shape of the upper boundary of the Philippine Sea plate.
Thin black contours show the depths of the upper boundary of the Philippine Sea slab (Hirose et al. 2008).
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Assuming the top of the PHS crust corresponds to the upper boundary of the PHS, the upper boundary is dipping toward the northwest, which is nearly parallel to the convergent direction of the PHS.
The upwelling of water at the upper boundary of BCL is provided by inflow of shelf modified Mediterranean waters in the same amount.
Based on the model of Ivanov and Samodurov [52], the vertical velocity of water at the upper boundary of BCL was estimated as 6.8 × 10−9 m s−1.
However, Pen-2 contains only two extracellular/lumenal lysine residues (one of which forms the upper boundary of TMD1 and may not be fully accessible for cross-linking), so isolation of Pen-2 iNP40/RIPAPA buffer was very limited.
Black bold lines indicate the location of the upper boundaries of the PAC (Nakajima et al. 2009) and PHS (Uchida et al. 2010) at each depth.
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