The deliverable focuses on a categorized listing of key issues and available information plus a concise description of the major characteristics of the Tongatapu coast (see Appendix B). The evidence to support the recommendations presented in this report has been gathered from a literature review, interviews with key stakeholders of Tongan government agencies and consideration of existing institutional practices of coastal management planning from the international arena (see Deliverable 2).
Rising oceans, changing lives: Final report is the overview report in a series of technical reports that have been
written for the project on Lifuka Island. Accordingly the section titles in the final report correspond with the
names of the respective technical reports.
This was an integrated effort by all concerned with the coastline in Tonga.
Integrated Coastal management applied conscious management process that acknowledge the interrelationships among most coastal and ocean uses and the environment that potentially affected.
The study was a remarkably productive and enriching experience for all who were involved. It became a forum for critical reflections and analysis. It also built a knowledge and understanding amongst different communities, villages and the survey team.
Water Resources Report 1992, Appendices A-H
Water Resources Report 1992, Appendices I-K
Water Resources Report 1992 : Appendices L-O
Water Resources Report 1992, Figs 5.17-5.53
This report, one of a series of reports from the Tonga Water Supply Master Plan Study, presents the findings of a recent water resources study of the islands in the Kingdom of Tonga. It summarises previous work, documents recent and current investigations and recommends further investigations to gain a better understanding of the water resources. It also outlines details of a proposed national monitoring and protection programme and makes recommendations about legislation for water resource management and protection.
The following study by Mr Furness is his summation of these labours of three years. It is a valuable document for future water management in Tonga and testimony to his professional dedication and his commitment to the Tongan people.
"There is a window of opportunity for avoiding the most damaging climate change impacts, but that window is closing: the world has less than a decade to change course. Actions taken - or not taken -... will have a profound bearing on the future... The world lacks neither the financial resources nor the technological capabilities... What is missing is a sense of urgency, human solidarity and collective interest (2007/2008 Human Development Report).
Available online
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Physical Description: 126 p.
As of 1969, the scientific community had no general information on the natural history of Namoluk Atoll in the Eastern Caroline Islands of Micronesia. The only significant published source for the atoll was an ethnographic and linguistic account provided by the German physician.
Pacific Island Countries (PICs) are heavily dependent on natural resources and likely to remain so for the near future, making resource management an issue of critical importance for economic development. This chapter employs a simple neoclassical
growth model to diagnose deficiencies in current policy regimes and suggest possible alternatives. Current practices in the exploitation of the regions mineral, tuna, and forest resources are used to illustrate problems and suggest possible policy interventions.
Available online
Call Number: [EL]
In World Resources 2005 we have argued that environmental income is the wealth of the poor, with the potential to provide not just subsistence but a path out of poverty if the right gover-
nance conditions prevail. In many communities, this argument is borne out every day, in on-the-ground, village-level experience.
Available online|Village by Village: Recovering Fiji's coastal fisheries|Restoring coastal resources by linking traditional conservation practices with modern techniques to create locally managed marine areas. p.144
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Coral atolls are natural laboratories within which to examine ecological processes (Sachet, 1967; Lee, 1984). They are often isolated, in some cases little disturbed, and have a geologically recent history of terrestrial plant colonisation. Reef islands around the rim of most atolls are Holocene in age. They are composed of biogenic skeletal sediments and have developed since reef growth caught up with sea level which stabilized after post-glacial sea-level rise. Plant colonisation of most of these islands must have occurred over a period of no more than 6000 years.
Interpretation of SEASAT geoid anomaly data and improved seafloor mapping of the
south-central Pacific suggest a complex tectonic history for the islands of the Pitcairn
group. While Oeno atoll formed at ~ 16m.y.BP at a 'hotspot' now south of the Easter micro-
plate, subsequent progressive island development at Henderson (13m.y.), Ducie (8m.y.)
and Crough seamount (4m.y.) resulted from the lateral leakage of magma from the Oeno
lineation along an old fracture zone, itself originating during the Tertiary reorientation
Samoa, like other Least Developed Countries (LDCs) inherits high vulnerability to natural disasters and to external economic and trade developments for which it has no control. These natural disasters include tropical cyclones, prolonged periods of drought, extreme flooding, pests and sudden outbreak of diseases, storm surges and sea level rise.
Available online
Call Number: [EL]
Physical Description: 39 p.
Located at 148°15' West and 15°50' South, in the northwesternmost part of the Tuamotu archipelago (Central Pacific), Makatea island is isolated from its nearest
neighbouring atolls, Rangiroa and Tikehau by about 80 km, and it is 245 km from its closest volcanic neighbour, Tahiti. This island rises at least 3,500 m above the sea floor.