Part 1 of the Tuvalu Maritime Zones Act 2012 states that the territorial sea comprises those areas of the sea having
(a) as their inner limits, the baseline, which is measured from the low-water line of the seaward side of the reef fringing the coast of any part of Tuvalu or bounding any lagoon waters adjacent to any part of that coast, or where a reef is not present, the low-water line of the coast itself and
(b) as their outer limits, a line measured seaward from that baseline, every point of which is distant 12 nautical miles from the nearest point of that baseline.
Part 4 of the Tuvalu Maritime Zones Act 2012 states that the exclusive economic zone of Tuvalu comprises those areas of the sea, seabed and subsoil that are beyond and adjacent to the territorial sea, having as their outer limits a line measured seaward from the baseline; which is measured from the low-water line of the seaward side of the reef fringing the coast of any part of Tuvalu or bounding any lagoon waters adjacent to any part of that coast, or where a reef is not present, the low-water line of the coast itself every point of which is not more than 200 nautical miles from the neares
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the territorial sea of Kiribati comprises those waters having, as their inner limits, the baseline of Kiribati and, as their outer limits, a line measured seaward from that baseline, every point of which is at a distance of twelve (12) nautical miles from the nearest point of the baseline.
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the "Contiguous Zone" means waters beyond the territorial sea within a distance of twenty-four (24) nautical miles from the baselines from which the breadth of the territorial sea is measured.
Chapter 1 of Title 18 of the Code of the Federated States of Micronesia, as amended by Public Law No. 19-172 on April 28, 2017, states that the Territorial Sea is a line, every point of which is 12 M seaward of the nearest point of the baseline. Waters landward of the baseline, including the lagoons of atolls or islands, are internal waters.
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the territorial sea of Kiribati comprises those waters having, as their inner limits, the baseline of Kiribati and, as their outer limits, a line measured seaward from that baseline, every point of which is at a distance of twelve (12) nautical miles from the nearest point of the baseline.
The Marine Zones (Declaration) Act 2011 states that "Baseline" means the baseline from which the breadth of the territorial sea, contiguous zone, exclusive economic zone and continental shelf is measured. It contains the geographic coordinates that defines the baseline for the Line Group. The points are defined by geographic coordinates are determined by reference
to the World Geodetic System 1984 (WGS 84).
Maps and associated data from the Turtle Research and Monitoring Database System (TREDS). A summary of the database can be found below.
The Turtle Research and Monitoring Database System (TREDS) provides invaluable information for Pacific island countries and territories to manage their turtle resources. TREDS can be used to collate data from strandings, tagging, nesting, emergence and beach surveys as well as other biological data on turtles.
Map of predictions of relative probabilities of species occurence in a global grid of half-degree latitude and longitude cell dimensions.
Map of predictions of relative probabilities of benthic marine species occurence in a global grid of half-degree latitude and longitude cell dimensions.
Map of predictions of relative probabilities of pelagic species occurence in a global grid of half-degree latitude and longitude cell dimensions.
Map of artisanal fishing intensity based on data from the global map of human impacts (2008) (https://www.nceas.ucsb.edu/globalmarine2008/impacts).
Map developed by MACBIO for the bioregions workshop 2018. Chlorophyl-a concentration is an important proxy which is routinely measured and is considered a "core" parameter of global physical-biological oceanic models. Map is based on data from NASA's Aqua satellite.
The map contains the global distribution of habitat suitability for seven suborders of cold water octocoral found deeper than 50m. Map is based on data from Yesson et al (2012) Global habitat suitability of cold water Octocorals, Journal of Biogeography 39, 1278-1292.
The map displays the number of coral species that are expected to be found in each grid cell that contains coral reefs as identified by the Millenium Reefs project. The map is based on a spatial data base of geographic range boundaries compiled by the Australian Research Council Centre of Excellence for Coral Reef Studies compi
This map was developed by MACBIO as resource for the bioregions workshop 2017 and shows ocean surface currents based on data from NOAA Ocean Surface Current Analysis (http://www.oscar,noaa.gov/).
The map depicts paths and intensities of tropical cyclones in Solomon Islands EEZ from 1980 till 2015. Data of tropical cyclone best track data is provided by IBTrACS (International Best Track Archive for Climate Stewardship).
The map shows the diffuse attenuation coefficient (Kd490) which is an indicator of the turbidity of the water column. The grid is derived from MODIS (Moderate Resolution Imaging Spectoradiometer) images from NASA's Terra and Aqua satellites (http://oceancolor.gsfc.nasa.gov).
The map shows the domestic shipping routes in Solomon Islands EEZ. Data is based on information from Harbour Master of Ports Authority. The map was developed by MACBIO as resource for the bioregions workshop in Feb 2018.
Eddies are circular shaped or elongated rotating vortices of the sea surface, 300 - 500km wide. They are the oceanic analogy to storms in the atmosphere, and are clearly seen in maps of sea surface anomaly from altimeters. Positive anomaly features indicate the presence of anticyclonic eddies where the sea surface is doming upwards and causing downwelling. For downwelling features, strength and persistence are key determinants of increased primary productivity and thus aggregations of bioty.