Climate Change

Covering almost one-third of the earth’s surface, the region of the Pacific islands is subject to a range of environmental stressors—including those deriving from volcanoes and earthquakes, and of course those attributable to atmospheric and oceanic processes. Most people living on the islands, peppered across this vast ocean, occupy island coasts, where food and water are generally most readily obtainable but where the impacts of many hazards focus. While popularly viewed as particularly vulnerable to disasters and climate change, Pacific Islanders have evolved formidable bodies of traditional and local knowledge (TLK) that have enabled their survival on comparatively small islands often thousands of kilometers from continental shores. While it is largely place-specific, this TLK is wide-ranging. It includes ensuring water and food security (especially in the aftermath of disasters), predicting and surviving extreme events (especially tropical cyclones), creating traditional pharmacopoeias, learning how to sail across thousands of kilometers of open ocean, and developing cultural resilience that could be adapted to changing circumstances. Detailed accounts are given of the use of Pacific TLK in disaster management and in climate-change adaptation. While much TLK has been lost and has suffered from being overwhelmed by a flood of outsider (science-based) solutions, it remains a potent force among many rural communities in the Pacific islands. Owing to its demonstrable effectiveness, its place-based nature, and its ability to accommodate change, Pacific TLK should be at the heart of future plans for helping Pacific Islanders cope with future climate change.

Tropical cyclones (TCs) in their most intense expression (hurricanes or typhoons) are the main natural hazards known to humankind. The impressive socioeconomic consequences for countries dealing with TCs make our ability to model these organized convective structures a key issue to better understanding their nature and their interaction with the climate system. The destructive effects of TCs are mainly caused by three factors: strong wind, storm surge, and extreme precipitation. These TC-induced effects contribute to the annual worldwide damage of the order of billions of dollars and a death toll of thousands of people. Together with the development of tools able to simulate TCs, an accurate estimate of the impact of global warming on TC activity is thus not only of academic interest but also has important implications from a societal and economic point of view. The aim of this article is to provide a description of the TC modeling implementations available to investigate present and future climate scenarios. The two main approaches to dynamically model TCs under a climate perspective are through hurricane models and climate models. Both classes of models evaluate the numerical equations governing the climate system. A hurricane model is an objective tool, designed to simulate the behavior of a tropical cyclone representing the detailed time evolution of the vortex. Considering the global scale, a climate model can be an atmosphere (or ocean)-only general circulation model (GCM) or a fully coupled general circulation model (CGCM). To improve the ability of a climate model in representing small-scale features, instead of a general circulation model, a regional model (RM) can be used: this approach makes it possible to increase the spatial resolution, reducing the extension of the domain considered. In order to be able to represent the tropical cyclone structure, a climate model needs a sufficiently high horizontal resolution (of the order of tens of kilometers) leading to the usage of a great deal of computational power. Both tools can be used to evaluate TC behavior under different climate conditions. The added value of a climate model is its ability to represent the interplay of TCs with the climate system, namely two-way relationships with both atmosphere and ocean dynamics and thermodynamics. In particular, CGCMs are able to take into account the well-known feedback between atmosphere and ocean components induced by TC activity and also the TC–related remote impacts on large-scale atmospheric circulation. The science surrounding TCs has developed in parallel with the increasing complexity of the mentioned tools, both in terms of progress in explaining the physical processes involved and the increased availability of computational power. Many climate research groups around the world, dealing with such numerical models, continuously provide data sets to the scientific community, feeding this branch of climate change science.