The guidelines for the design of conjunctive water supply systems to improve resilience to drought in Nauru have been developed as part of the Pacific Adaptation to Climate Change (PACC) demonstration project initiative. The PACC project involves 14 pacific countries and is aimed at building resilience to impacts of climate change in the key vulnerable socio-economic sectors. In Nauru, drought has been identified has one of the most threatening impact that could result from change in climate patterns.
National Communication reports represent the most standardized and comparable documents on the climate policies of different countries. This dataset hosts all national communications submissions by Nauru to the United Nations Framework Convention on Climate Change.
Government Report to UNCCD - prepared by the Dept. Economic Development and Environment. 2003
pdf 1 pager. graph downloaded from BOM 2021
Legislation
raw data on ozone depleting substance consumption for Nauru. OurWorldInData.org
4-page summary from the United Nations Framework Convention on Climate Change
Graph from OurWorldInData
Report presented to the Fourth Pacific Meteorological Council Meeting held in Honiara from 14-18 August, 2017.
Report - 9 pages
Report - 49 pages. Porduced with support from the European Union and the German Government (GIZ).
Map of the Nauru island landcover, with country-level summary of the different landcover classes and designation.
Tropical forestry and logging are complex subjects, encompassing a range of diffi cult issues, including land ownership, the sustainability of natural resources, the impact on climate change, the social and economic impact of logging on isolated and relatively untouched, subsistence sector communities, and the protection of the basic rights of the people concerned.
Papua New Guinea’s (PNG) forests and forestry have played an important role in the livelihoods of the people of the country for many years. Forests have provided a source for food, fruits and nuts, building materials, medicinal plants, habitats for refuge and a wealth of other services.
A summary of various datasets on logging concessions, exports, forest cover are presented here.
Oil palm prices may hold up in the medium term, with strong demand from India and China. Yet, like other non-oil commodities, oil palm prices are likely to remain volatile, and to experience a long term relative price decline. (Chapter 3). World prices are not the main problem for small farmers in PNG. Three factors are likely to place a ceiling on the economic benefits for small farmers: (i) small farmers remain at the highly competitive end of a large grower market, with little market power, keeping them as ‘price takers’; (ii) a large monopsony (all
Coupled climate and sea-level changes deduced from Huon Peninsula coral terraces of the last ice age
Huon Peninsula, Papua New Guinea, is a tectonically unstable, uplifting shoreline ringed by emergent coral terraces. The terraces were formed during episodes of rapid sea-level rise when corals constructed large, discrete coral platforms that were subsequently uplifted. Uranium series ages of four prominent Huon Peninsula last glacial (OIS 3) coral terraces coincide with the timing of major North Atlantic climate reversals at intervals of 6000^7000 yr between 30 000 yr and 60 000 yr ago.
Peatlands are common in montane areas above 1,000 m in New Guinea and become extensive above 3,000 m in the subalpine zone. In the montane mires, swamp forests and grass or sedge fens predominate on swampy alley bottoms. These mires may be 4–8 m in depth and up to 30,000 years in age. In Papua New Guinea (PNG) there is about 2,250 km2 of montane peatland, and Papua Province (the Indonesian western half of the island) probably contains much more. Above 3,000 m, peat soils form under blanket bog on slopes as well as on valley floors.
This chapter provides a brief description of Papua New Guinea, its past and present climate as well as projections for the future. The climate observation network and the availability of atmospheric and oceanic data records are outlined. The annual mean climate, seasonal cycles and the influences of large-scale climate features such as the West Pacific Monsoon and patterns of climate variability (e.g. the El Niño‑Southern Oscillation) are analysed and discussed.