The Papua New Guinea Government submits PNG’s first Biennial Update Report (BUR1) under the United Nations Framework Convention on Climate Change (UNFCCC). The report follows the BUR guidelines for developing countries according to paragraphs 39 to 42 of Decision 2/CP.17 and its Annex III.
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.
This technical note is intended to support climate risk assessment (CRA) experts, in particular, those undertaking the early stages of project development. Time and resources could be saved by attaching this document to terms of reference issued to CRA consultants. However, there is a limit to which globally accessible, open source
data can meet the detailed information needs of local adaptation projects. This note supplements rather than replaces efforts to gather relevant climate information from government agencies and counterparts, especially during the project concept phase.
Here we analyze rainfall data for the New Guinea region comprising station observations, reanalysis products and satellite-based estimates in order to better understand some of these details. We find that most gridded products are limited due to their relatively coarse horizontal resolutions that fail to resolve topographic effects. However, the relatively fine resolution TRMM satellite–based product appears to provide reliable estimates and linear correlations between the data and the NINO34 sea surface temperature index provides an insight into the pattern of ENSO rainfall impacts.
The 2020 State of Environment Report is the first for Papua New Guinea.
JICA Country Profile on Environment of Papua New Guinea (PNG) was carried out by the Planning and Evaluation Department Japan International Cooperation Agency in February 2002. This 37 paged report outlines PNG's fact sheets, organization structure, legislation, current environmental issues and international relations between PNG and overseas countries
Summarizes the findings to date, and places them in a regional and historical context. Discusses the SEAFRAME gauge in Manus Island, Papua New Guinea, which records sea level, air and water temperature, atmospheric pressure, wind speed and direction. It is one of an array designed to monitor changes in sea level and climate in the Pacific.
It is a Pre-Workshop In Country Review For Papua New Guinea 19th-23rd October 1999 in Nadi, Fiji Islands. Collaboration between NDMO, PNG NWS and Water Resources