previous wet season out to sea.
The restoration study was conducted in Vam Ray Village, Binh
Son commune, Hon Dat district, 40 km north of Rach Gia city, Kien
Giang Province. This area has a low topography with site elevation
from
0.48 m (at the dyke’s foot) to
0.705 m (at seaward end
transect) relative to mean sea level while the nearby mangrove
area is consistently approximately 0.45 m higher from the coastline
out to 45 m from the shore(Fig. 1). The study area is characterized
by semi diurnally irregular regimes and coastal shorelines are
mainly influenced by SW wind-induced waves. The lowest tide is
in NE monsoon winds (0.2 m) and the highest is 1.5 m SW
monsoon. Although, storms and typhoon are rare, strong SW winds
in the wet season can create strong waves of 2–2.5 m offshore.
Average wind speed in NE season is 2 m/s and SW is 5 m/s (Russell
et al., 2013).
ฤดูฝนที่ก่อนหน้านี้ออกไปในทะเลprevious wet season out to sea.
ที่ได้รับการศึกษาที่ดำเนินการในการฟื้นฟู The restoration study was conducted in Vam Ray Village, Binh
จังหวัดบุตรที่รักดาดอำเภอ Son commune, Hon Dat district, 40 km north of Rach Gia city, Kien
Giang Giang Province. This area has a low topography with site elevation
from
0.48 m (at the dyke’s foot) to
0.705 m (at seaward end
transect) relative to mean sea level while the nearby mangrove
area is consistently approximately 0.45 m higher from the coastline
out to 45 m from the shore(Fig. 1). The study area is characterized
by semi diurnally irregular regimes and coastal shorelines are
mainly influenced by SW wind-induced waves. The lowest tide is
in NE monsoon winds (0.2 m) and the highest is 1.5 m SW
monsoon. Although, storms and typhoon are rare, strong SW winds
in the wet season can create strong waves of 2–2.5 m offshore.
Average wind speed in NE season is 2 m/s and SW is 5 m/s (Russell
et al., 2013).
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