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Taiwan is located between the world's largest landmass, the continent of Asia, and its largest ocean, the Pacific Ocean. The Tropic of Cancer passes through the island of Taiwan, giving it a subtropical and tropical oceanic climate. High temperatures and rainfall and strong winds characterize the climate. Because of Taiwan's position in the Asian monsoon region, its climate is greatly influenced by monsoons as well as by its own complicated topography. The annual mean temperatures in the lowlands are 22–25°C, and the monthly mean temperature exceeds 20°C for eight months starting with April each year. The period from June to August is the hottest season with mean temperatures of 27–29°C. Temperatures are cooler between November and March; in most places, the coldest monthly mean temperature is above 15°C. The climate is mild rather than cold and temperatures only fall dramatically when a cold front affects the region. Average annual rainfall in the lowlands of Taiwan is in the range of 1,600–2,500mm. Due to the influences of topography and the monsoon climate, the rainfall differs greatly with different areas and seasons. In mountainous areas, average rainfall may exceed 4,000mm/yr. Rainfall is generally higher in mountainous areas than in lowland areas, higher in the east than in the west, and higher on windward slopes than on the leeward side. The northeast monsoon prevails during the winter; this is the rainy season in the north though rainfall is not intense. But the same winter period is the dry season in the south. During the summer, the southwest monsoon prevails, often giving rise to convective thunderstorms and bringing intense and copious rainfall. With added downpours brought by typhoons, this season often accounts for over 50% of annual rainfall in the south so that central and southern regions often suffer greatly. Relative humidity on the island of Taiwan, surrounded by ocean, is high, usually measuring in the range of 78–85%. In the north, relative humidity is higher during winter than during summer. The situation in the south is the opposite. Over the past 100 years, the rainfall in the north has increased, while the rainfall in the south has decreased. The trend is not as consistent as that of the temperature change (Environmental Protection Administration, Executive Yuan, R.O.C. (Taiwan), 2002).

Rivers flowing through the land are a source of life. They have different importance and functions such as for drinking, sailing, irrigating crops, generating electricity, sightseeing, fishing, and so on. In addition, animals like amphibians, birds, and mammals also live and propagate near the river environment. Therefore, rivers are ecosystems for some animals and plants that are special, rare, or on the brink of extinction (Water Resources Agency, Ministry of Economic Affairs, 2006).

Purpose – Many cities are located in coastal areas and many of them are identified as prone to climate change impacts, especially sea level rise and floods. Master plans of cities can feature responses to these challenges, as in the case of Jakarta's master plan 2010–2030. However, as this chapter will argue, the top-down nature of planning would likely produce, reproduce, or reaffirm unjust urban geographies in the name of climate change adaptation. North Jakarta and its coastal area, which were prone to climate change risks, has been home for more than 40,000 poor households, most of which live in houses less than 50m2 in informal settlements with lack of basic needs infrastructures. This chapter addresses the question, “How are poor communities in the north coast of Jakarta affected by extreme weather events, and how are their everyday experiences addressed in master plan Jakarta 2010–2030?”

Methodology/approach – Analysis is based on community profiles, census information, and a workshop with representatives of these communities. This chapter will also analyze relevant parts of Jakarta's 2010–2030 master plan. The discussion covers the following: (1) the making of place-based communities of the urban poor in the north coast of Jakarta compared to the master plan, and (2) the impact of climate change on the urban poor's livelihoods in the north coast.

Findings – The current master plan 2010–2030 features plans to mitigate climate change and environmental risks for the coastal area, especially sea level rise, land subsidence, and pollution. The study reveals that North Jakarta communities were unaware of what the city planners have drafted, but most of them realized climate challenges based on their everyday experience. They aspired to be involved in the planning process, but their informal status hampered their opportunity to be heard.

Originality/value of chapter – Rather than looking at how Jakarta as a city is affected by climate change, this chapter focuses on specific communities in North Jakarta that are prone to climate change-induced risks. Climate change impacts are spatially unequal, and even in the same region that theoretically bears the same risks, the impact distribution of climate change can be unequal for different social groups. The chapter also questions the ability of urban planning to respond to these challenges when planning practice itself has not yet taken into account citizens’ social awareness and participation meaningfully.

The southwest coastal region is part of an inactive delta of large Himalayan rivers and is protected from tidal surge by the Sundarbans mangrove forest. This area is the hub of all types of disasters such as cyclones, tidal surges, floods, drought, salinity intrusions, repeated waterlogging, and land subsidence. Cyclonic tidal surges and floods are the more common disasters, and their effects are frequently experienced at the local level. But silent and invisible disasters such as increased salinity, arsenic contamination, and drought affect local livelihoods, people, and environments in this region. The vulnerability of southwest region to increased salinity, arsenic contamination, and drought are the result of a complex interrelationship among biophysical, social, economical, and technological characteristics of the country. Moreover, in the current and foreseeable future, the country is likely to be affected by the biggest, most long-lasting, and global scale but silent disaster: increased salinity, natural arsenic contamination, and drought. Therefore, this region is thought to be the most disaster-prone region in Bangladesh because of natural disasters and highly vulnerable to the effects of climate change.

Climate change adaptation strategies are critical for long-term road infrastructure development (RID) because it is expected to put more land and transportation infrastructure at risk from stronger winds, more intense storms, and rising sea levels. Deformation and subsidence could occur if concrete pavements crumbled and asphalt roads softened due to higher temperatures, and changes in the frequency and intensity of precipitation could have far-reaching consequences for the smooth operation of transportation networks. The developed world is primarily responsible for the carbon emissions that contribute to global warming, while less developed countries are insignificant. The African Union sees climate change as a major threat to the continent’s economic development and is working with member states and key organizations to address it. It is critical for developing countries to establish frameworks for detecting climate change risks, developing adaptation strategies, and implementing plans. The sustainable development plan (SRIP) is critical for protecting transportation networks from the effects of climate change. Sustainable development principles are critical for clarifying the proposed project’s relationships with the local and larger society, economy, ecosystems, and various institutions. The ability of a system or structure to recover from disruption while continuing to function and adapt to new circumstances is referred to as resilient infrastructure. Low-carbon infrastructure coexists with resilient infrastructure, and the pursuit of resilient infrastructure necessitates a reduction in the likelihood of failure, a lessening of the negative consequences when failures do occur, and a reduction in the time required to recover due to an increase in the facilities’ capacity to endure, adapt, and change. As part of the implementation process, RID experts must consider how climate change will impact transportation infrastructure. Risk assessment is a systematic method of looking for things that could go wrong, determining how bad they could be, and determining how likely they are to happen. Adaptable designs must include multiple measures to prevent system breakdowns. Climate change’s effects on road infrastructure, as well as rising sea levels, continue to jeopardize low-lying transportation infrastructure. Implementing SRIP necessitates the development of a climate change response mechanism.

In recent years, a great deal of work has emerged on eco-cities in China. Specifically, writers have discussed the role of the entrepreneurial state in the construction of eco-cities and have noted the role of these cities in the production of high-end real estate and new forms of capital accumulation and land acquisition. Whilst this chapter supports these arguments, we argue that the emergence of eco-cities in China is tied up with broader socioeconomic and cultural discourses and discourses of governance. We explore these ideas through a qualitative investigation of an eco-city known as the North Lake (Beihu) Ecological New Town (NLENT) located in the city of Jining, Shandong province. Specifically, this project, which involved the collection of documents, photographs and 20 semi-structured interviews, aims to understand the role that discourses of class, taste and consumption play in the fashioning of Chinese eco-cities. In exploring discourses of ‘green conduct’, this chapter also seeks to understand the role of eco-cities in the governmental fashioning of Chinese subjects and bodies. In this regard, this chapter suggests that whilst new forms of green development have played a part in urban expansion, new green real estate zones such as the NLENT have a powerful role to play in the construction and shaping of Chinese identity and behaviour.

Purpose – To investigate the potential impacts of future climate change in the United Kingdom on its road and rail networks.

Methodology/approach – The climate change impacts of increasing summer temperatures, decreasing winter temperatures, increased heavy precipitation, greater numbers of extreme weather events and rises in sea level are reviewed.

Findings – Surface transportation is the most exposed element to the localised impacts of climate change. High summer temperatures will result in road rutting, rail buckling and decreased thermal comfort, whereas more intense winter precipitation will cause flooding, landslips and bridge scour across all modes. For all impacts, it is the extreme events (e.g. heat waves and storms) that are potentially the most devastating. As shown, there are some positive climate change impacts. For example, in the case of winter maintenance, all transport networks stand to benefit.

Originality/value – In order for transport to react appropriately to the potential changes in climate, it is essential to understand how the road and rail networks may be affected and to build strategies for both adaptation and mitigation into plans for future developments for both modes.

Ever since human society developed, environmental and social changes have led to major challenges that must be dealt with. Some of these major challenges are seen as “disasters,” for which a definition that is frequently used is similar to “A serious disruption of the functioning of a community or a society causing widespread human, material, economic or environmental losses which exceed the ability of the affected community or society to cope using its own resources” (UNISDR, 2004; see, e.g., Quarantelli, 1998, and Furedi, 2007, for discussions on the meaning(s) of “disaster”). From witnessing disasters and being forced to work through the aftermath, humanity has been shifting toward trying to reduce disasters’ impacts or to avert them entirely. This field has the modern-day interpretation of “disaster risk reduction,” defined as “The conceptual framework of elements considered with the possibilities to minimize vulnerabilities and disaster risks throughout a society, to avoid (prevention) or to limit (mitigation and preparedness) the adverse impacts of hazards, within the broad context of sustainable development” (UNISDR, 2004).

The Indus, Mekong, and Ganges River deltas, which have created one of the world’s largest delta and submarine fan system, currently contribute a major fraction of freshwater to East and South Asia. All these deltas are those regions in the world that face major challenges in their water sector due to population growth, urbanization, industrialization, sea-level rise, and salinity intrusion into inland and water bodies, all aggravated by climate change. Among them, salinity intrusion is currently one of the key issues that directly and indirectly cause water insecurity in East and South Asia, which ultimately hamper livelihood, agricultural production, and social interference. Hence, this chapter gives a comprehensive description on the nature and extent of the salinity problem, its adverse effects on livelihood and water sector, and then the focus goes to current and future sustainable water resource management within the delta to finally move on to conclusion and suggestions.