=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 29-Jul-1993
Anomalously large value June 1946 and low values at end of 1946 (just before a data gap) - correct as received from authority.
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 04-Aug-1994
For a discussion of interannual variability of sea level along the coasts of Pakistan and India, see Clarke and Liu, Journal of Physical Oceanography, 24, 1224, 1994.
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 14-Jun-2002
Data for 1916-20 are MSL and were obtained from the Survey of India, Dehra Dun.   Data 1937-48 are MTL (Mean Tide Level) and were also obtained from the Survey of India. Data 57 onwards are MSL. 1957-65 were obtained from the Pakistan Meteorological Department, while 1966-85 from National Institute of Oceanography. 1986-87 were obtained from the University of
Hawaii Sea Level Center using data supplied by the NIO.
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 17-Jun-2002
Karachi             490/021 RLR(1947) is 9.7m below BM 1PP (circa 1920)
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 25-Sep-2002
New data from Pakistan Navy for 1987 replaces TOGA data for Jan-Apr and Dec
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 11-Mar-2009
The gauge at Karachi has been resited and is now no longer on Manora Island. The new gauge has been levelled in to the old one. 2007/8 one minute sea level data downloaded from the
IOC Sea Level Station Monitoring Facility Ostend. This is then converted to 15min. data for processing. 2007/8 monthly and annual mean sea level values have now been extracted from the data. As the relationship for the prime bench mark remains the same there is no need to alter RLR. Details of the bench marks has been derived from site installation information. Copies of these have been included in the port files and RLR file for reference.
=========================== FOLLOWING PSMSL DOCUMENTATION ADDED 26-Jan-2016
A value of MTL-MSL=10 mm has been applied to the RLR data for the period 1937-1948. Values were derived using values from the GESLA2 (high-frequency tide gauge) dataset. A value of 10 mm was used from the historic databank of harmonic tidal constants gathered by the International Hydrographic Organization.

