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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.

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.

UNDP has been working during the last decade to support countries to transition to green, inclusive, climate-resilient development paths. More than US$790 million in grant financing from the Global Environment Facility-managed Least Developed Countries Fund and the Special Climate Change Fund, as well as the Kyoto Protocol’s Adaptation Fund and bilateral finance, have been mobilized to assist countries to achieve their adaptation
priorities. These resources build on and complement over US$2.5 billion in co-financing that has also been invested.

Forest

Forestry and climate change

Climate change and Marine

Ozon Depleting Substance

Information on PNG from the Proceedings of the Pacific Regional Consultation on Water in Small Island Countries – Country Briefing Papers at least 2003 or older.

Climate change and migration