200NM
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 Exclusive economic zone is contiguous to the territorial sea. The inner boundary of the exclusive economic zone of each island or atoll is the seaward boundary of the territorial sea, and the outer boundary is a line, every point of which is two hundred nautical miles seaward of the nearest point on the baseline.
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 exclusive economic zone comprises those waters beyond the territorial sea of Kiribati, but within a distance of two hundred (200) nautical miles from the baseline of Kiribati, shall be the exclusive economic zone of the Republic of Kiribati.
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.
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.
Part 2 of the Tuvalu Maritime Zones Act 2012 states that the contiguous zone comprises those areas of the sea that are beyond and adjacent to the territorial sea, having as their outer limits a line measured seaward from the baseline every point of which is distant 24 nautical miles from the nearest point of that baseline.
Where an archipelagic baseline is declared, the outer limits of the contiguous zone are a line measured seaward from that archipelagic baseline, every point of which is distant 24 nautical miles from the nearest point of that archipelagic baseline.
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.
Global EEZ layer are the layers gathered from gazetted datasets that the Pacific Community (SPC) has received from the project countries. In areas where there are no gazetted datasets provisional layers are being sourced from the Global Marine Regions database (https://www.marineregions.org/).
There are two layers available, he .shp file layer and the .kml layer which are being used by partners and member states in particular FFA for the Regional Fisheries Surveillance Center (RFSC).
"The impacts of the 1997-1998 El Nino are
fresh in our minds, and the latest reports from
the work of the Intergovernmental Panel on
Climate Change (IPCC) confirm tvhat all of you
already know changes in climate matter to
individuals, communities, businesses and
governments who call islands home. Your
valuable natural resources, traditional ways of
life, critical economic sectors, community support
infrastructure, atid, to a great extent, your
future, depend on developing an effective
Climate change is real and Asia is already experiencing its adverse impacts. Projections from the Intergovernmental Panel on Climate Change (IPCC) suggest that such impacts will become even more intense in the future. While the contribution of developing countries in Asia to global greenhouse gas (GHG) emissions is increasing rapidly, per capita emissions are still low and developmental challenges remain significant.
The Earth currently finds itself in the midst of what some have termed the "Anthropocene Era" - a period during which human activities have become a dominate force affecting not only the
planet's landscape, but also its atmosphere. Since the dawn of the industrial evolution of the mid-18th century, humans have contributed to substantial increases in the concentration of
greenhouse gases in the atmosphere. Carbon dioxide has increased by 36%, methane by 17%, and nitrous oxide by 151%. These changes in the global atmosphere are directly linked to over
The Fourth Assessment Report of the IPCC (IPCC AR4) Working Group II (2007) identifies small island states as being among the most vulnerable countries of the world to the adverse impacts of climate change. Hay, el al.y (2003) in discussing the Pacific's observed climate noted that compared to earlier historical records during the twentieth century, the southern Pacific had experienced a significantly drier and warmer climate (by 15 percent and 0.8°C, respectively).