cover
Article Per Year (5 Year)
All
Home Page
OAI Link
Editorial Team
Contact
Reviewer
Google Scholar
Contact Name
Aan J. Wahyudi
Contact Email
aanj001@lipi.go.id
Phone
-
Journal Mail Official
mri@mail.lipi.go.id
Editorial Address
-
Location
Kota adm. jakarta selatan,
Dki jakarta
INDONESIA
Marine Research in Indonesia
Published by Lembaga Ilmu Pengetahuan Indonesia
ISSN : 02162873     EISSN : 24432008     DOI : -
Core Subject : Science,
Earth & Planetary Sciences
MARINE RESEARCH IN INDONESIA (MRI) has been published since 1956 by Indonesia's oldest marine research institute, the Research Center for Oceanography of LIPI (Indonesian Institute of Sciences). MRI focuses on physical, chemical, biological, geological oceanographic as well as coastal management studies in the Indonesian seas and the adjacent Indo-Pacific region.
Arjuna Subject : -
Articles 4 Documents
 1 
Search results for , issue "Vol 1 (1956)" : 4 Documents clear
THE SUBTROPICAL LOWER WATER BETWEEN THE PHILIPPINES AND IRIAN (NEW GUINEA) Wyrtki, Klaus
Marine Research in Indonesia Vol 1 (1956)
Publisher : Research Center for Oceanography - Indonesian Institute of Sciences (LIPI)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3691.241 KB) | DOI: 10.14203/mri.v1i0.323

Abstract

Oceanographic observations are published, taken by the research vessel Siboela in 1949 at 57 stations in the Celebes Sea and around Halmahera. Basing on these observations, an analysis is made of the Subtropical Lower Water (salinity-Maximum) in this region and is compared with the observations of the Snellius and the Dana in 1929. The distribution of the oxygen content allows a distinction of the Lower Water into a northern and a southern water type, which regions of origion are situated in 23°N between 165°E and 165°W and in 15°S between 120° and 150°W respectively. It is shown that the temperature of the salinity maximum in 1949 is 1.4° higher and the salinity 0.11‰ lower than in 1929. The topography of the salinity maximum, which lies in about 100 to 200 m, is closely correlated with the surface currents.
SEASONAL FLUCTUATIONS IN THE SURFACE SALINITY OFF THE NORTH COAST OF JAVA Soeriaatmadja, Raden E.
Marine Research in Indonesia Vol 1 (1956)
Publisher : Research Center for Oceanography - Indonesian Institute of Sciences (LIPI)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3195.562 KB) | DOI: 10.14203/mri.v1i0.321

Abstract

The division of the region investigated according to P. CH. VEEN is redescribed. The micro salinity titration by means of the method described by G. H. ARNOLD with an accuracy of 0.1 ‰ was used for this investigation. This technique was adopted because of the large number of observations, and was sufficiently accurate since salinity in these waters varies widely. The annual range in salinity is large, caused by a considerable discharge of fresh water from the many big and small rivers, especially in the rainy-season as well as by the inequality of salinity of the oceanwaters coming from the East, and the South China Sea water coming from the West, during the dry and wet-sason respectively. In the east-monsoon, the eastern section is covered with ocean water over 34.0 ‰ and the western section with mixed waters ranging between 31.5 ‰ and 34.0 ‰, while in the west-monsoon, the area is covered with mixed water less than 32.5 ‰.
SEASONAL FLUCTUATIONS IN THE SURFACE SALINITY OFF THE NORTH COAST OF JAVA Soeriaatmadja, Raden E.
Marine Research in Indonesia Vol 1 (1956)
Publisher : Research Center for Oceanography - Indonesian Institute of Sciences (LIPI)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3195.562 KB) | DOI: 10.14203/mri.v1i0.321

Abstract

The division of the region investigated according to P. CH. VEEN is redescribed. The micro salinity titration by means of the method described by G. H. ARNOLD with an accuracy of 0.1 ? was used for this investigation. This technique was adopted because of the large number of observations, and was sufficiently accurate since salinity in these waters varies widely. The annual range in salinity is large, caused by a considerable discharge of fresh water from the many big and small rivers, especially in the rainy-season as well as by the inequality of salinity of the oceanwaters coming from the East, and the South China Sea water coming from the West, during the dry and wet-sason respectively. In the east-monsoon, the eastern section is covered with ocean water over 34.0 ? and the western section with mixed waters ranging between 31.5 ? and 34.0 ?, while in the west-monsoon, the area is covered with mixed water less than 32.5 ?.
THE SUBTROPICAL LOWER WATER BETWEEN THE PHILIPPINES AND IRIAN (NEW GUINEA) Wyrtki, Klaus
Marine Research in Indonesia Vol 1 (1956)
Publisher : Research Center for Oceanography - Indonesian Institute of Sciences (LIPI)

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3691.241 KB) | DOI: 10.14203/mri.v1i0.323

Abstract

Oceanographic observations are published, taken by the research vessel Siboela in 1949 at 57 stations in the Celebes Sea and around Halmahera. Basing on these observations, an analysis is made of the Subtropical Lower Water (salinity-Maximum) in this region and is compared with the observations of the Snellius and the Dana in 1929. The distribution of the oxygen content allows a distinction of the Lower Water into a northern and a southern water type, which regions of origion are situated in 23°N between 165°E and 165°W and in 15°S between 120° and 150°W respectively. It is shown that the temperature of the salinity maximum in 1949 is 1.4° higher and the salinity 0.11? lower than in 1929. The topography of the salinity maximum, which lies in about 100 to 200 m, is closely correlated with the surface currents.

Page 1 of 1 | Total Record : 4

 1 

Filter by Year

1956 1956


Reset
Filter By Issues
All Issue Vol 44 No 2 (2019) Vol 44 No 2 (2019) Vol 44 No 1 (2019) Vol 44 No 1 (2019) Vol 43 No 2 (2018) Vol 43, No 2 (2018) Vol 43, No 1 (2018) Vol 43 No 1 (2018) Vol 42 No 2 (2017) Vol 42, No 2 (2017) Vol 42, No 1 (2017) Vol 42 No 1 (2017) Vol 41 No 2 (2016) Vol 41, No 2 (2016) Vol 41, No 1 (2016) Vol 41 No 1 (2016) Vol 40, No 2 (2015) Vol 40 No 2 (2015) Vol 40, No 1 (2015) Vol 40 No 1 (2015) Vol 39 No 2 (2014) Vol 39, No 2 (2014) Vol 39, No 1 (2014) Vol 39 No 1 (2014) Vol 38 No 2 (2013) Vol 38, No 2 (2013) Vol 38 No 1 (2013) Vol 38, No 1 (2013) Vol 37, No 2 (2012) Vol 37 No 2 (2012) Vol 37 No 1 (2012) Vol 37, No 1 (2012) Vol 36 No 2 (2011) Vol 36, No 2 (2011) Vol 36, No 1 (2011) Vol 36 No 1 (2011) Vol 35 No 2 (2010) Vol 35, No 2 (2010) Vol 35 No 1 (2010) Vol 35, No 1 (2010) Vol 34, No 2 (2009) Vol 34 No 2 (2009) Vol 34, No 1 (2009) Vol 34 No 1 (2009) Vol 33 No 2 (2008) Vol 33, No 2 (2008) Vol 33, No 1 (2008) Vol 33 No 1 (2008) Vol 32, No 2 (2007) Vol 32 No 2 (2007) Vol 32, No 1 (2007) Vol 32 No 1 (2007) Vol 31 (2006) Vol 31 (2006) Vol 30 (2006) Vol 30 (2006) Vol 29 (1995) Vol 29 (1995) Vol 28 (1992) Vol 28 (1992) Vol 27 (1989) Vol 27 (1989) Vol 26 (1987) Vol 26 (1987) Vol 25 (1985) Vol 25 (1985) Vol 24 (1984) Vol 24 (1984) Vol 23 (1984) Vol 23 (1984) Vol 22 (1981) Vol 22 (1981) Vol 21 (1978) Vol 21 (1978) Vol 20 (1977) Vol 20 (1977) Vol 19 (1977) Vol 19 (1977) Vol 18 (1977) Vol 18 (1977) Vol 17 (1977) Vol 17 (1977) Vol 16 (1976) Vol 16 (1976) Vol 15 (1975) Vol 15 (1975) Vol 14 (1975) Vol 14 (1975) Vol 13 (1973) Vol 13 (1973) Vol 12 (1972) Vol 12 (1972) Vol 11 (1971) Vol 11 (1971) Vol 10 (1970) Vol 10 (1970) Vol 9 (1969) Vol 9 (1969) Vol 8 (1967) Vol 8 (1967) Vol 6 (1963) Vol 6 (1963) Vol 5 (1963) Vol 5 (1963) Vol 4 (1959) Vol 3 (1957) Vol 3 (1957) Vol 2 (1956) Vol 2 (1956) Vol 1 (1956) Vol 1 (1956) More Issue