Raster data representing the mean levels of nitrate in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of phosphate in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of calcite in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of current velocities in meters/second for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of dissolved oxygen in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of iron in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of pH for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of phytoplankton in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of silicate in µmol/m3 for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Raster data representing the mean levels of temperature in degrees Celsius (°C) for the surface water layer. The data are available for global-scale applications at a spatial resolution of 5 arcmin (approximately 9.2 km at the equator).
Marine data layers for present conditions were produced with climate data describing monthly averages for the period 2000–2014, obtained from pre-processed global ocean re-analyses combining satellite and in situ observations at regular two- and three-dimensional spatial grids.
Climate change profoundly affects global agriculture, posing food security threats via extreme weather, temperature shifts, and rainfall variations. In the Pacific Islands, additional challenges like sea-level rise and ecosystem degradation exacerbate these issues. The American Samoa Extension Climate Forum, conducted on June 20-21, 2018, sought to address these concerns by engaging stakeholders in discussions about sustainable agriculture, climate adaptation, and food security.
Pacific Island Developing Countries (PIDCs) contribute a minuscule 0.03 percent to global carbon dioxide emissions, with residents producing only a quarter of the world's average emissions per person. However, despite their minimal emissions, these nations are expected to face some of the earliest and harshest consequences of climate change, with a particular focus on its impact on freshwater resources. This chapter delves into the potential threats posed by climate change to the already stressed freshwater supplies in PIDCs.
In response to climate change impacts like rising sea levels, efforts are being made in the Pacific Islands region to assess and adapt to the effects on mangroves. This includes improving management practices, reducing stress on mangroves, and integrating climate data into land-use planning to minimize risks to coastal ecosystems and human safety.
This chapter discusses advances in climate change impact, adaptation, and vulnerability assessment methods, emphasizing the growing use of risk management frameworks, stakeholder involvement, and diverse scenario approaches. These developments aim to provide policy-relevant information for effective decision-making in the face of climate change, recognizing the importance of considering non-climate factors and regional-scale scenarios.
This chapter explores the complex interactions within the climate system, emphasizing the significance of understanding climate's physical and social impacts at various scales. It underscores the importance of assessing vulnerability to climate conditions, focusing on sensitivity, exposure, and resilience, especially in Pacific Island communities facing climate-related challenges.
This report, part of the Pacific Islands Regional Climate Assessment (PIRCA), discusses climate change indicators and their impacts on key sectors in American Samoa. PIRCA, a collaborative effort involving various stakeholders, aims to inform and prioritize actions in response to climate change in the US-Affiliated Pacific Islands and the Hawaiian archipelago.
This project focuses on assessing American Samoa's vulnerability to natural hazards and the impacts of climate change. It engaged with the community through an online survey, interviews, and a preparedness workshop in Pago Pago. The goal is to help residents and professionals in American Samoa prepare for future hazard events and climate change impacts, providing information, stories, and guidance on disaster and climate change preparedness
Following the 2009 Samoa-Tonga earthquake, the Samoan islands, including Savai'i, Upolu, and Tutuila, have experienced accelerated sea-level rise, driven by subsidence and gravity changes, with American Samoa witnessing a 5 times faster rate than the global average. A viscoelastic model predicts a continued sea-level rise of 30-40 cm, intensifying coastal flooding.
The absence of historical sea-level data for the Pacific over the past 1,000 years hinders our understanding of late Neogene sea-level changes. Data from tectonically stable sites in various Pacific locations suggest that sea level was close to its present level around 1,000 years ago, rose to approximately 0.9 meters above present levels around 700 years ago during the Little Climatic Optimum, then fell during the Little Ice Age before gradually rising again over the past 200 years. Tags: Pacific, sea-level change, historical data, Little Climatic Optimum, Little Ice Age.
Climate services, which provide actionable information about climate impacts, are crucial for Pacific Islands' policy, planning, and decision-making. NOAA, in collaboration with regional partners, has undertaken projects to enhance climate services through capacity building, engagement with users, and tailored information delivery, resulting in better-informed decisions and increased regional coordination.