Staying Mobile in Postapocalyptic Cli-Fi

Author(s):  
Jeremy Withers

This chapter examines how the rising popularity since the 1990s of works of postapocalyptic cli-fi (i.e. climate change fiction) has provided science fiction writers a convenient opportunity to explore issues of mobility and transportation. After first examining an early postapocalyptic cli-fi work from the 1990s by Octavia E. Butler, the chapter then advances this book’s chronological analysis to some twenty-first century works of science fiction. In its discussion of a novel by Paolo Bacigalupi and one by Benjamin Parzybok, this chapter shows how more restrained modes of transport play a vital role during times of apocalypse in keeping a society functioning and keeping us as individuals from slipping into disempowerment.

2013 ◽  
Vol 3 (4) ◽  
pp. 27-34 ◽  
Author(s):  
Michael Ziser

This article looks at the California origins of much of Twentieth Century science fiction. It examines how the exploding growth and development of postwar California informed science fiction writers like Ray Bradbury, Robert Heinlein, and Philip K. Dick, and looks to their books for answers to twenty-first century dilemmas such as the uses of technology, the environment, and infrastructure.


Author(s):  
Paul Giles

The theme of The Planetary Clock is the representation of time in postmodern culture and the way temporality as a global phenomenon manifests itself differently across an antipodean axis. To trace postmodernism in an expansive spatial and temporal arc, from its formal experimentation in the 1960s to environmental concerns in the twenty-first century, is to describe a richer and more complex version of this cultural phenomenon. Exploring different scales of time from a Southern Hemisphere perspective, with a special emphasis on issues of Indigeneity and the Anthropocene, The Planetary Clock offers a wide-ranging, revisionist account of postmodernism, reinterpreting literature, film, music, and visual art of the post-1960 period within a planetary framework. By bringing the culture of Australia and New Zealand into dialogue with other Western narratives, it suggests how an antipodean impulse, involving the transposition of the world into different spatial and temporal dimensions, has long been an integral (if generally occluded) aspect of postmodernism. Taking its title from a clock designed in 1510 to measure worldly time alongside the rotation of the planets, The Planetary Clock ranges across well-known American postmodernists (John Barth, Toni Morrison) to more recent science fiction writers (Octavia Butler, Richard Powers), while bringing the US tradition into dialogue with both its English (Philip Larkin, Ian McEwan) and Australian (Les Murray, Alexis Wright) counterparts. By aligning cultural postmodernism with music (Messiaen, Ligeti, Birtwistle), the visual arts (Hockney, Blackman, Fiona Hall) and cinema (Rohmer, Haneke, Tarantino), The Planetary Clock enlarges our understanding of global postmodernism for the twenty-first century.


Author(s):  
Hyun Min Sung ◽  
Jisun Kim ◽  
Sungbo Shim ◽  
Jeong-byn Seo ◽  
Sang-Hoon Kwon ◽  
...  

AbstractThe National Institute of Meteorological Sciences-Korea Meteorological Administration (NIMS-KMA) has participated in the Coupled Model Inter-comparison Project (CMIP) and provided long-term simulations using the coupled climate model. The NIMS-KMA produces new future projections using the ensemble mean of KMA Advanced Community Earth system model (K-ACE) and UK Earth System Model version1 (UKESM1) simulations to provide scientific information of future climate changes. In this study, we analyze four experiments those conducted following the new shared socioeconomic pathway (SSP) based scenarios to examine projected climate change in the twenty-first century. Present day (PD) simulations show high performance skill in both climate mean and variability, which provide a reliability of the climate models and reduces the uncertainty in response to future forcing. In future projections, global temperature increases from 1.92 °C to 5.20 °C relative to the PD level (1995–2014). Global mean precipitation increases from 5.1% to 10.1% and sea ice extent decreases from 19% to 62% in the Arctic and from 18% to 54% in the Antarctic. In addition, climate changes are accelerating toward the late twenty-first century. Our CMIP6 simulations are released to the public through the Earth System Grid Federation (ESGF) international data sharing portal and are used to support the establishment of the national adaptation plan for climate change in South Korea.


2017 ◽  
Vol 30 (17) ◽  
pp. 6701-6722 ◽  
Author(s):  
Daniel Bannister ◽  
Michael Herzog ◽  
Hans-F. Graf ◽  
J. Scott Hosking ◽  
C. Alan Short

The Sichuan basin is one of the most densely populated regions of China, making the area particularly vulnerable to the adverse impacts associated with future climate change. As such, climate models are important for understanding regional and local impacts of climate change and variability, like heat stress and drought. In this study, climate models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) are validated over the Sichuan basin by evaluating how well each model can capture the phase, amplitude, and variability of the regionally observed mean, maximum, and minimum temperature between 1979 and 2005. The results reveal that the majority of the models do not capture the basic spatial pattern and observed means, trends, and probability distribution functions. In particular, mean and minimum temperatures are underestimated, especially during the winter, resulting in biases exceeding −3°C. Models that reasonably represent the complex basin topography are found to generally have lower biases overall. The five most skillful climate models with respect to the regional climate of the Sichuan basin are selected to explore twenty-first-century temperature projections for the region. Under the CMIP5 high-emission future climate change scenario, representative concentration pathway 8.5 (RCP8.5), the temperatures are projected to increase by approximately 4°C (with an average warming rate of +0.72°C decade−1), with the greatest warming located over the central plains of the Sichuan basin, by 2100. Moreover, the frequency of extreme months (where mean temperature exceeds 28°C) is shown to increase in the twenty-first century at a faster rate compared to the twentieth century.


2017 ◽  
Vol 56 (9) ◽  
pp. 2393-2409 ◽  
Author(s):  
Rick Lader ◽  
John E. Walsh ◽  
Uma S. Bhatt ◽  
Peter A. Bieniek

AbstractClimate change is expected to alter the frequencies and intensities of at least some types of extreme events. Although Alaska is already experiencing an amplified response to climate change, studies of extreme event occurrences have lagged those for other regions. Forced migration due to coastal erosion, failing infrastructure on thawing permafrost, more severe wildfire seasons, altered ocean chemistry, and an ever-shrinking season for snow and ice are among the most devastating effects, many of which are related to extreme climate events. This study uses regional dynamical downscaling with the Weather Research and Forecasting (WRF) Model to investigate projected twenty-first-century changes of daily maximum temperature, minimum temperature, and precipitation over Alaska. The forcing data used for the downscaling simulations include the European Centre for Medium-Range Weather Forecasts (ECMWF) interim reanalysis (ERA-Interim; 1981–2010), Geophysical Fluid Dynamics Laboratory Climate Model, version 3 (GFDL CM3), historical (1976–2005), and GFDL CM3 representative concentration pathway 8.5 (RCP8.5; 2006–2100). Observed trends of temperature and sea ice coverage in the Arctic are large, and the present trajectory of global emissions makes a continuation of these trends plausible. The future scenario is bias adjusted using a quantile-mapping procedure. Results indicate an asymmetric warming of climate extremes; namely, cold extremes rise fastest, and the greatest changes occur in winter. Maximum 1- and 5-day precipitation amounts are projected to increase by 53% and 50%, which is larger than the corresponding increases for the contiguous United States. When compared with the historical period, the shifts in temperature and precipitation indicate unprecedented heat and rainfall across Alaska during this century.


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