Making weather great again
Adverse Weather Evokes Nostalgia
Wijnand van Tilburg, Constantine Sedikides & Tim Wildschut
Personality and Social Psychology Bulletin, forthcoming
Abstract:
Four studies examined the link between adverse weather and the palliative role of nostalgia. We proposed and tested that (a) adverse weather evokes nostalgia (Hypothesis 1); (b) adverse weather causes distress, which predicts elevated nostalgia (Hypothesis 2); (c) preventing nostalgia exacerbates weather-induced distress (Hypothesis 3); and (d) weather-evoked nostalgia confers psychological benefits (Hypothesis 4). In Study 1, participants listened to recordings of wind, thunder, rain, and neutral sounds. Adverse weather evoked nostalgia. In Study 2, participants kept a 10-day diary recording weather conditions, distress, and nostalgia. We also obtained meteorological data. Adverse weather perceptions were positively correlated with distress, which predicted higher nostalgia. Also, adverse natural weather was associated with corresponding weather perceptions, which predicted elevated nostalgia. (Results were mixed for rain.) In Study 3, preventing nostalgia (via cognitive load) increased weather-evoked distress. In Study 4, weather-evoked nostalgia was positively associated with psychological benefits. The findings pioneer the relevance of nostalgia as source of comfort in adverse weather.
Believing in climate change, but not behaving sustainably: Evidence from a one-year longitudinal study
Michael Hall, Neil Lewis & Phoebe Ellsworth
Journal of Environmental Psychology, April 2018, Pages 55-62
Abstract:
We conducted a one-year longitudinal study in which 600 American adults regularly reported their climate change beliefs, pro-environmental behavior, and other climate-change related measures. Using latent class analyses, we uncovered three clusters of Americans with distinct climate belief trajectories: (1) the “Skeptical,” who believed least in climate change; (2) the “Cautiously Worried,” who had moderate beliefs in climate change; and (3) the “Highly Concerned,” who had the strongest beliefs and concern about climate change. Cluster membership predicted different outcomes: the “Highly Concerned” were most supportive of government climate policies, but least likely to report individual-level actions, whereas the “Skeptical” opposed policy solutions but were most likely to report engaging in individual-level pro-environmental behaviors. Implications for theory and practice are discussed.
Climate gentrification: From theory to empiricism in Miami-Dade County, Florida
Jesse Keenan, Thomas Hill & Anurag Gumber
Environmental Research Letters, May 2018
Abstract:
This article provides a conceptual model for the pathways by which climate change could operate to impact geographies and property markets whose inferior or superior qualities for supporting the built environment are subject to a descriptive theory known as 'Climate Gentrification.' The article utilizes Miami-Dade County, Florida (MDC) as a case study to explore the market mechanisms that speak to the operations and processes inherent in the theory. This article tests the hypothesis that the rate of price appreciation of single-family properties in MDC is positively related to and correlated with incremental measures of higher elevation (the 'Elevation Hypothesis'). As a reflection of an increase in observed nuisance flooding and relative SLR, the second hypothesis is that the rates of price appreciation in the lowest elevation cohorts have not kept up with the rates of appreciation of higher elevation cohorts since approximately 2000 (the 'Nuisance Hypothesis'). The findings support a validation of both hypotheses and suggest the potential existence of consumer preferences that are based, in part, on perceptions of flood risk and/or observations of flooding. These preferences and perceptions are anticipated to be amplified by climate change in a manner that reinforces the proposition that climate change impacts will affect the marketability and valuation of property with varying degrees of environmental exposure and resilience functionality. Uncovering these empirical relationships is a critical first step for understanding the occurrence and parameters of Climate Gentrification.
Going Green: Environmental Protest, Policy, and CO2 Emissions in U.S. States, 1990–2007
John Muñoz, Susan Olzak & Sarah Soule
Sociological Forum, forthcoming
Abstract:
A major goal of the environmental movement is to conserve or improve the natural environment, but evidence showing that environmental mobilization produces positive environmental outcomes is mixed. This article addresses a fundamental question about the relative impact of pro‐environmental mobilization and the scope of an environmental policy regime on the natural environment. Using panel data at the state level from 1990 through 2007, we explore how environmental protest and environmental policies independently (or jointly) reduce CO2 emissions in U.S. states. We find that the level of emissions in a state declines in states with increases in pro‐environmental protest, net of the effects of the range of environmental policies enacted, gasoline taxes, liberal attitudes, reliance on the fossil fuel industry, number of registered lobbyist organizations, gross state product, and population size.
Warm Arctic episodes linked with increased frequency of extreme winter weather in the United States
Judah Cohen, Karl Pfeiffer & Jennifer Francis Nature
Communications, March 2018
Abstract:
Recent boreal winters have exhibited a large-scale seesaw temperature pattern characterized by an unusually warm Arctic and cold continents. Whether there is any physical link between Arctic variability and Northern Hemisphere (NH) extreme weather is an active area of research. Using a recently developed index of severe winter weather, we show that the occurrence of severe winter weather in the United States is significantly related to anomalies in pan-Arctic geopotential heights and temperatures. As the Arctic transitions from a relatively cold state to a warmer one, the frequency of severe winter weather in mid-latitudes increases through the transition. However, this relationship is strongest in the eastern US and mixed to even opposite along the western US. We also show that during mid-winter to late-winter of recent decades, when the Arctic warming trend is greatest and extends into the upper troposphere and lower stratosphere, severe winter weather — including both cold spells and heavy snows — became more frequent in the eastern United States.
Sea Level Rise Impacts on Wastewater Treatment Systems along the U.S. Coasts
Michelle Hummel, Matthew Berry & Mark Stacey
Earth's Future, forthcoming
Abstract:
As sea levels rise, coastal communities will experience more frequent and persistent nuisance flooding, and some low‐lying areas may be permanently inundated. Critical components of lifeline infrastructure networks in these areas are also at risk of flooding, which could cause significant service disruptions that extend beyond the flooded zone. Thus, identifying critical infrastructure components that are exposed to sea level rise is an important first step in developing targeted investment in protective actions and enhancing the overall resilience of coastal communities. Wastewater treatment plants are typically located at low elevations near the coastline to minimize the cost of collecting consumed water and discharging treated effluent, which makes them particularly susceptible to coastal flooding. For this analysis, we used geographic information systems to assess the exposure of wastewater infrastructure to various sea level rise projections at the national level. We then estimated the number of people who would lose wastewater services, which could be more than five times as high as previous predictions of the number of people at risk of direct flooding due to sea level rise. We also performed a regional comparison of wastewater exposure to marine and groundwater flooding in the San Francisco Bay Area. Overall, this analysis highlights the widespread exposure of wastewater infrastructure in the U.S. and demonstrates that local disruptions to infrastructure networks may have far‐ranging impacts on areas that do not experience direct flooding.
Early emergence of anthropogenically forced heat waves in the western United States and Great Lakes
Hosmay Lopez et al.
Nature Climate Change, May 2018, Pages 414–420
Abstract:
Climate projections for the twenty-first century suggest an increase in the occurrence of heat waves. However, the time at which externally forced signals of anthropogenic climate change (ACC) emerge against background natural variability (time of emergence (ToE)) has been challenging to quantify, which makes future heat-wave projections uncertain. Here we combine observations and model simulations under present and future forcing to assess how internal variability and ACC modulate US heat waves. We show that ACC dominates heat-wave occurrence over the western United States and Great Lakes regions, with ToE that occurred as early as the 2020s and 2030s, respectively. In contrast, internal variability governs heat waves in the northern and southern Great Plains, where ToE occurs in the 2050s and 2070s; this later ToE is believed to be a result of a projected increase in circulation variability, namely the Great Plain low-level jet. Thus, greater mitigation and adaptation efforts are needed in the Great Lakes and western United States regions.
Climatic control of Mississippi River flood hazard amplified by river engineering
Samuel Munoz et al.
Nature, 5 April 2018, Pages 95–98
Abstract:
Over the past century, many of the world’s major rivers have been modified for the purposes of flood mitigation, power generation and commercial navigation. Engineering modifications to the Mississippi River system have altered the river’s sediment levels and channel morphology, but the influence of these modifications on flood hazard is debated. Detecting and attributing changes in river discharge is challenging because instrumental streamflow records are often too short to evaluate the range of natural hydrological variability before the establishment of flood mitigation infrastructure. Here we show that multi-decadal trends of flood hazard on the lower Mississippi River are strongly modulated by dynamical modes of climate variability, particularly the El Niño–Southern Oscillation and the Atlantic Multidecadal Oscillation, but that the artificial channelization (confinement to a straightened channel) has greatly amplified flood magnitudes over the past century. Our results, based on a multi-proxy reconstruction of flood frequency and magnitude spanning the past 500 years, reveal that the magnitude of the 100-year flood (a flood with a 1 per cent chance of being exceeded in any year) has increased by 20 per cent over those five centuries, with about 75 per cent of this increase attributed to river engineering. We conclude that the interaction of human alterations to the Mississippi River system with dynamical modes of climate variability has elevated the current flood hazard to levels that are unprecedented within the past five centuries.
Limited influence of climate change mitigation on short-term glacier mass loss
Ben Marzeion et al.
Nature Climate Change, April 2018, Pages 305–308
Abstract:
Glacier mass loss is a key contributor to sea-level change, slope instability in high-mountain regions, and the changing seasonality and volume of river flow. Understanding the causes, mechanisms and time scales of glacier change is therefore paramount to identifying successful strategies for mitigation and adaptation. Here, we use temperature and precipitation fields from the Coupled Model Intercomparison Project Phase 5 output to force a glacier evolution model, quantifying mass responses to future climatic change. We find that contemporary glacier mass is in disequilibrium with the current climate, and 36 ± 8% mass loss is already committed in response to past greenhouse gas emissions. Consequently, mitigating future emissions will have only very limited influence on glacier mass change in the twenty-first century. No significant differences between 1.5 and 2 K warming scenarios are detectable in the sea-level contribution of glaciers accumulated within the twenty-first century. In the long-term, however, mitigation will exert strong control, suggesting that ambitious measures are necessary for the long-term preservation of glaciers.
Temperature accelerates the rate fields become forests
Jason Fridley & Justin Wright
Proceedings of the National Academy of Sciences, forthcoming
Abstract:
Secondary succession, the postdisturbance transition of herbaceous to woody-dominated ecosystems, occurs faster at lower latitudes with important ramifications for ecosystem processes. This pattern could be driven by the direct effect of temperature on tree growth; however, an alternative mechanism is tree–herb competition, which may be more intense in more fertile northern soils. We manipulated soil fertility and herbaceous species composition in identical experiments at six sites spanning the Eastern United States (30–43° N) and monitored the growth and survival of four early successional trees. Tree seedling mass 2 years after sowing was strongly associated with site differences in mean growing season temperature, regardless of species or soil treatment. The effect of temperature was twofold: seedlings grew faster in response to warmer site temperatures, but also due to the reduction of competitive interference from the herbaceous community, which was inhibited in warmer sites. Our results suggest that increasing temperatures will promote a faster transition of fields to forests in temperate ecosystems.
Assessing the relative contribution of economic, political and environmental factors on past conflict and the displacement of people in East Africa
Erin Llwyd Owain & Mark Andrew Maslin
Palgrave Communications, April 2018
Abstract:
According to the UN Refugee Agency in 2016 there were over 20 million displaced people in Africa. There is considerable debate whether climate change will exacerbate this situation in the future by increasing conflict and thus displacement of people. To explore this climate-conflict-refugee nexus this study analyses whether climatic changes between 1963 and 2014 impacted the risk of conflict and displacement of people in East Africa. A new composite conflict database recording major episodes of political violence (MEPV) was compared with climatic, economic and political indicators using optimisation regression modelling. This study found that climate variations as recorded by the Palmer Drought Severity Index (PDSI) and the global temperature record did not significantly impact the level of regional conflict or the number of total displaced people (TDP). The major driving forces on the level of conflict were population growth, economic growth and the relative stability of the political regimes. Numbers of TDP seemed to be linked to population and economic growth. Within TDP, ‘refugees’ were recorded as people that were forced to cross borders between countries. In contrast to TDP and conflict, variations in refugee numbers were found to be significantly related to climatic variations as well as political stability, population and economic growth. This study suggests that climate variations played little or no part in the causation of conflict and displacement of people in East Africa over the last 50 years. Instead, we suggest rapid population growth, low or falling economic growth and political instability during the post-colonial transition were the more important controls. Nonetheless, during this period this study does shows that severe droughts were a contributing driver of refugees crossing international borders. This study demonstrates that within socially and geo-politically fragile systems, climate change may potentially exacerbate the situation particularly with regards to enforced migration.
Risks from climate extremes change differently from 1.5°C to 2.0°C depending on rarity
Viatcheslav Kharin et al.
Earth's Future, forthcoming
Abstract:
Parties to the United Nations Framework Convention on Climate Change (UNFCCC) have agreed to hold the “increase in global average temperature to well below 2°C above pre‐industrial levels and to pursue efforts to limit the temperature increase to 1.5°C”. Comparison of the costs and benefits for different warming limits requires an understanding of how risks vary between warming limits. As changes in risk are often associated with changes in exposure due to projected changes in local or regional climate extremes, we analyze differences in the risks of extreme daily temperatures and extreme daily precipitation amounts under different warming limits. We show that global warming of 2°C would result in substantially larger changes in the probabilities of the extreme events than global warming of 1.5°C. For example, over the global land area, the probability of a warm extreme that occurs once every 20‐years on average in the current climate is projected to increase 130% and 340% at the 1.5°C and 2.0°C warming levels respectively (median values). Moreover, the relative changes in probability are larger for rarer, more extreme events, implying that risk assessments need to carefully consider the extreme event thresholds at which vulnerabilities occur.
Quantified, localized health benefits of accelerated carbon dioxide emissions reductions
Drew Shindell et al.
Nature Climate Change, April 2018, Pages 291–295
Abstract:
Societal risks increase as Earth warms, and increase further for emissions trajectories accepting relatively high levels of near-term emissions while assuming future negative emissions will compensate, even if they lead to identical warming as trajectories with reduced near-term emissions. Accelerating carbon dioxide (CO2) emissions reductions, including as a substitute for negative emissions, hence reduces long-term risks but requires dramatic near-term societal transformations. A major barrier to emissions reductions is the difficulty of reconciling immediate, localized costs with global, long-term benefits. However, 2 °C trajectories not relying on negative emissions or 1.5 °C trajectories require elimination of most fossil-fuel-related emissions. This generally reduces co-emissions that cause ambient air pollution, resulting in near-term, localized health benefits. We therefore examine the human health benefits of increasing 21st-century CO2 reductions by 180 GtC, an amount that would shift a ‘standard’ 2 °C scenario to 1.5 °C or could achieve 2 °C without negative emissions. The decreased air pollution leads to 153 ± 43 million fewer premature deaths worldwide, with ~40% occurring during the next 40 years, and minimal climate disbenefits. More than a million premature deaths would be prevented in many metropolitan areas in Asia and Africa, and >200,000 in individual urban areas on every inhabited continent except Australia.
Climate, crops, and forests: A pan-tropical analysis of household income generation
Sven Wunder, Frederik Noack & Arild Angelsen
Environment and Development Economics, forthcoming
Abstract:
Rural households in developing countries depend on crops, forest extraction and other income sources for their livelihoods, but these livelihood contributions are sensitive to climate change. Combining socioeconomic data from about 8,000 smallholder households across the tropics with gridded precipitation and temperature data, we find that households have the highest crop income at 21°C temperature and 2,000 mm precipitation. Forest incomes increase on both sides of this agricultural maximum. We further find indications that crop income declines in response to weather shocks while forest income increases, suggesting that households may cope by reallocating inputs from agriculture to forests. Forest production may thus be less sensitive than crop production to climatic fluctuations, gaining comparative advantage in extreme climates and under weather anomalies. This suggests that well-managed forests might help poor rural households to cope with and adapt to future climate change.
The Risk of Termination Shock From Solar Geoengineering
Andy Parker & Peter Irvine
Earth's Future, March 2018, Pages 456-467
Abstract:
If solar geoengineering were to be deployed so as to mask a high level of global warming, and then stopped suddenly, there would be a rapid and damaging rise in temperatures. This effect is often referred to as termination shock, and it is an influential concept. Based on studies of its potential impacts, commentators often cite termination shock as one of the greatest risks of solar geoengineering. However, there has been little consideration of the likelihood of termination shock, so that conclusions about its risk are premature. This paper explores the physical characteristics of termination shock, then uses simple scenario analysis to plot out the pathways by which different driver events (such as terrorist attacks, natural disasters, or political action) could lead to termination. It then considers where timely policies could intervene to avert termination shock. We conclude that some relatively simple policies could protect a solar geoengineering system against most of the plausible drivers. If backup deployment hardware were maintained and if solar geoengineering were implemented by agreement among just a few powerful countries, then the system should be resilient against all but the most extreme catastrophes. If this analysis is correct, then termination shock should be much less likely, and therefore much less of a risk, than has previously been assumed. Much more sophisticated scenario analysis — going beyond simulations purely of worst-case scenarios — will be needed to allow for more insightful policy conclusions.