“A mesei a delal a telid”
a taro field is the mother of life

-Palauan proverb

Understanding Climate Change

Climate change refers to significant, long-term shifts in global weather patterns and temperatures, primarily driven by increased concentrations of greenhouse gases like carbon dioxide in the atmosphere. These changes result from human activities such as burning fossil fuels, deforestation, and industrial processes. These greenhouse gases trap heat in the earth’s atmosphere resulting in the rise of global average temperature, melting polar ice, sea-level rise, and more frequent extreme weather events, all of which pose substantial risks to ecosystems and human societies. In Palau, these global changes manifest as higher temperatures, stronger typhoons, coral reef loss, and coastal flooding, presenting significant challenges to Palau’s economy, environment, and communities.

Climate variability refers to fluctuations in climate conditions over shorter timescales — seasons to decades — driven by natural cycles in the ocean-atmosphere system. Although natural climate cycles and other factors affect temperatures and weather patterns at regional scales, especially in the short term, the dominant mode of variability affecting Palau is the El Niño-Southern Oscillation (ENSO), an irregular two-to-seven-year oscillation between warm (El Niño) and cool (La Niña) sea surface temperature patterns across the tropical Pacific. El Niño conditions suppress rainfall, lower sea levels, and raise ocean temperatures in Palau’s region, significantly increasing coral bleaching risk; La Niña conditions have broadly opposite effects. At longer timescales, the Pacific Decadal Oscillation (PDO) and Madden-Julian Oscillation (MJO) further modulate rainfall, sea level, and tropical cyclone activity. As long-term climate change raises baseline temperatures, even moderate ENSO events are expected to produce impacts sectors in Palau that would previously have required stronger events.

First chart panel from the 2014 to 2016 El Niño assessment report for Palau. Second chart panel from the 2014 to 2016 El Niño assessment report for Palau.
Chronology of both the forcings and the impacts of the 2014-16 El Niño in Palau. The dashed line represents the “peak” of the event during which time the most anomalous conditions were observed. From Rupic, M., Wetzel, L., and Marra, J.J., Balwani, S. (2018). 2014-2016 El Niño Assessment Report: An Overview of the Impacts of the 2014-2016 El Niño on the U.S. Affiliated Pacific Islands (USAPI). NOAA National Centers for Environmental Information (NCEI) Technical Report, February 2018.

For information on climate variability, observed and projected changes, and projected impacts in the Pacific region, please visit the Pacific Climate Change Monitor. For a country-specific look at the impacts of climate change across sectors in Palau, please visit the Climate Change Monitor and Palau Pacific Islands Regional Climate Assessment (PIRCA).

Additional Climate Resources

  • McGree, S., G. Smith, E. Chandler, N. Herold, Z. Begg, Y. Kuleshov, P. Malsale, and M. Rittman, 2022: Climate Change in the Pacific 2022: Historical and Recent Variability, Extremes and Change. Pacific Community (SPC), Suva, Fiji.
  • CSIRO and SPREP (2021). ‘NextGen’ Projections for the Western Tropical Pacific: Current and Future Climate for Palau. Final report to the Australia-Pacific Climate Partnership for the Next Generation Climate Projections for the Western Tropical Pacific project. Commonwealth Scientific and Industrial Research Organisation (CSIRO) and Secretariat of the Pacific Regional Environment Programme (SPREP), CSIRO Technical Report, Melbourne, Australia. https://doi.org/10.25919/fmfh-ek72.
  • Frazier, A.G., M.-V.V. Johnson, L. Berio Fortini, C.P. Giardina, Z.N. Grecni, H.H. Kane, V.W. Keener, R. King, R.A. MacKenzie, M. Nobrega-Olivera, K.L.L. Oleson, C.K. Shuler, A.K. Singeo, C.D. Storlazzi, R.J. Wallsgrove, and P.A. Woodworth-Jefcoats, 2023: Ch. 30. Hawaiʻi and US-Affiliated Pacific Islands. In: Fifth National Climate Assessment. Crimmins, A.R., C.W. Avery, D.R. Easterling, K.E. Kunkel, B.C. Stewart, and T.K. Maycock, Eds. U.S. Global Change Research Program, Washington, DC, USA. https://doi.org/10.7930/NCA5.2023.CH30.
  • IPCC, 2023: Summary for Policymakers. In: Climate Change 2023: Synthesis Report. Contribution of Working Groups I, II and III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Core Writing Team, H. Lee and J. Romero (eds.)]. IPCC, Geneva, Switzerland, pp. 1-34, doi: 10.59327/IPCC/AR6-9789291691647.001.
  • IPCC, 2023: Climate Change 2023: Synthesis Report. Contribution of Working Groups I, II and III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Core Writing Team, H. Lee and J. Romero (eds.)]. IPCC, Geneva, Switzerland, 184 pp., doi: 10.59327/IPCC/AR6-9789291691647.

Climate & Kukau

Root crops are generally limited by disease and pets, which are expected to increase activity with the predicted rise in temperature. Many traditional taro patches are also in low-lying areas vulnerable to saltwater intrusion due to sea level rise. Several taro patches on Babeldaob are currently affected by this, especially during high tides. Salt water in taro patches can result in crop loss as high as 75-100%. A 2014 study to evaluate varietals for salt tolerance in Ngimis, Ngatpang, Ollei, and Ngarchelong, found that the Kirang, Dirrubong and Dungersuul varietals were most salt tolerant (Del Rosario et al. 2014). Efforts to preserve taro varieties and to conduct research to determine which varietals are salt-tolerant are led by institutions like Palau Community College’s Cooperative Research & Extension, which maintains 68 varieties.

Additional Kukau Resources

Key Contacts

Government offices and organizations with relevant information on Kukau