Do Environmental Worldviews and Distrust Influence Action for Adaptation to Environmental Change Among Small-Scale Woodland Managers?

2020 ◽  
Vol 19 (2) ◽  
pp. 159-185
Author(s):  
Bianca Ambrose-Oji ◽  
Mark Atkinson ◽  
Gillian Petrokofsky ◽  
Gabriel Hemery
Author(s):  
Sarah A. Ebel ◽  
Christine M. Beitl ◽  
Michael P. Torre

Environmental change requires individuals and institutions to facilitate adaptive governance. However, facilitating adaptive governance may be difficult because resource users’ perceptions of desirable ways of life vary. These perceptions influence preferences related to environmental governance and may stem from the ways individuals subjectively value their work and their connections to their environment. This paper uses a value-based approach to examine individual and institutional preferences for adaptive governance in Carelmapu, Chile. We show that two groups had different value frames rooted in divergent ontologies which influenced their actions related to adaptive governance, creating conflict.


Land ◽  
2019 ◽  
Vol 8 (12) ◽  
pp. 190 ◽  
Author(s):  
Christopher Poeplau ◽  
Julia Schroeder ◽  
Ed Gregorich ◽  
Irina Kurganova

Climate change may increase the importance of agriculture in the global Circumpolar North with potentially critical implications for pristine northern ecosystems and global biogeochemical cycles. With this in mind, a global online survey was conducted to understand northern agriculture and farmers’ perspective on environmental change north of 60° N. In the obtained dataset with 67 valid answers, Alaska and the Canadian territories were dominated by small-scale vegetable, herbs, hay, and flower farms; the Atlantic Islands were dominated by sheep farms; and Fennoscandia was dominated by cereal farming. In Alaska and Canada, farmers had mostly immigrated with hardly any background in farming, while farmers in Fennoscandia and on the Atlantic Islands mostly continued family traditions. Accordingly, the average time since conversion from native land was 28 ± 28 and 25 ± 12 years in Alaska and Canada, respectively, but 301 ± 291 and 255 ± 155 years on the Atlantic Islands and in Fennoscandia, respectively, revealing that American northern agriculture is expanding. Climate change was observed by 84% of all farmers, of which 67% have already started adapting their farming practices, by introducing new varieties or altering timings. Fourteen farmers reported permafrost on their land, with 50% observing more shallow permafrost on uncultivated land than on cultivated land. Cultivation might thus accelerate permafrost thawing, potentially with associated consequences for biogeochemical cycles and greenhouse gas emissions. About 87% of the surveyed farmers produced for the local market, reducing emissions of food transport. The dynamics of northern land-use change and agriculture with associated environmental changes should be closely monitored. The dataset is available for further investigations.


2019 ◽  
pp. 271-282 ◽  
Author(s):  
William K. Oestreich ◽  
Timothy H. Frawley ◽  
Elizabeth J. Mansfield ◽  
Kristen M. Green ◽  
Stephanie J. Green ◽  
...  

Africa ◽  
2001 ◽  
Vol 71 (3) ◽  
pp. 449-480 ◽  
Author(s):  
Dan Brockington ◽  
Katherine Homewood

AbstractThe Mkomazi Game Reserve is contested by people who wish to use its resources and by conservationists who have argued that the reserve should be set aside for wildlife. Underpinning the conservationist case is the argument that people are harmful to the reserve's environment. Former residents of the reserve, notably pastoralists, argue that human use of the reserve did not cause its degradation. The debate is characterised by a lack of data extraordinary in view of the assertions made. An earlier paper set out the contrasting views and defined the data that would be needed to test them. This paper assesses what data there are, and whether it is possible to evaluate the extent to which people caused environmental change at Mkomazi. Using physical data and comments about the environment made by observers it is argued that no firm conclusions can be drawn about small-scale change but that there are indications of large-scale resilience. As a result of this uncertainty the article goes on to consider the extent to which there can ever be clarity about environmental change at Mkomazi as a philosophical contention or as a researchable issue.


2021 ◽  
Author(s):  
Susan Kay ◽  
Arlene L. Avillanosa ◽  
Victoria V. Cheung ◽  
Ngoc Hung Dao ◽  
Benjamin J. Gonzales ◽  
...  

Abstract The seas of Southeast Asia are home to some of the world’s most diverse ecosystems and resources that support the livelihoods and wellbeing of millions of people. Climate change will bring temperature changes, acidification and other environmental change, with uncertain consequences for human and natural systems in the region. We present the first regional-scale projections of change in the marine environment up to the end of 21st century. A coupled physical-biogeochemical model with a resolution of 0.1° (approximately 11 km) was used to create projections of future environmental conditions under two greenhouse gas scenarios, RCP4.5 and RCP8.5. These show a sea that is warming by 1.1–2.9°C through the 21st century, with surface pH falling by up to 0.02 and dissolved oxygen decreasing by 5 to 13 mmol m− 3. Changes for different parts of the region, including four sensitive coastal sites, are presented. The changes reach all parts of the water column and many places are projected to experience conditions well outside the range seen at the start of the century. Altered species distribution and damage to coral reefs resulting from this environmental change would have consequences for biodiversity, for the livelihoods of small-scale fishers and for the food security of coastal communities across the region. Projections of this type are a key tool for communities planning how they will adapt to the challenge of climate change.


The Holocene ◽  
2018 ◽  
Vol 28 (11) ◽  
pp. 1818-1835 ◽  
Author(s):  
Henry Hooghiemstra ◽  
Thomas Olijhoek ◽  
Menno Hoogland ◽  
Maarten Prins ◽  
Bas van Geel ◽  
...  

Columbus’ arrival in the New World in AD 1492 on the northern coast of Hispaniola was followed by a suite of changes in land-use. We reconstruct environmental change from a 225-cm-long sediment core from site Los Indios from an abandoned and sediment-filled meander of the Yaque River, Cibao Valley, northeastern Dominican Republic. The sediment record starts ca. AD 195 (ca. 1755 cal. yr BP) and the history of the meander infill was monitored by changing grain size distributions, organic matter concentration and pollen from wetland plants. From ca. AD 200 to ca. AD 1525, the pollen record indicates a diverse forest assemblage; however, the presence of pollen from potential crop plants suggest nearby small-scale subsistence crop cultivation. More abundant charcoal after ca. AD 1410 shows Amerindians increasingly used fire. The record of grain size distributions shows that the meander was temporarily part of a low energetic drainage system in which bedload and suspended sediments accumulated. After European colonization of Hispaniola increasing spores of coprophilous fungi evidence that Europeans had introduced during the first decades of colonization cattle in the Cibao Valley which gradually resulted in more open forest. The charcoal record around ca. AD 1650 reflects intensive forest clearing, suggesting that small-scale Pre-Colonial practice of crop cultivation became replaced by large-scale agriculture on the moist and nutrient rich soils along the Yaque River. Further deforestation and signals of erosion suggest that the population of colonists and introduced enslaved labour force must have increased rapidly. After ca. AD 1740 charcoal influx decreased suggesting that last deforestation activities used selective cutting to produce fire wood and timber for construction, rather than burning forest in situ. Two centuries after European colonization, by the 18th century, land-use within the Cibao Valley had become a balance between substantial livestock and crop cultivation (pollen grains have evidenced cereals, maize, and potentially also sugar cane, amaranthaceous crops and tobacco). After ca. AD 1950, swamp vegetation of Typha and Cyperaceae decreased, pointing to an almost fully terrestrialized meander with only few bodies of standing water, reflecting the present-day setting. This multiproxy reconstruction of anthropogenic environmental change shows a clear differentiation between an immediate introduction of livestock and after some 150 years the development of a European style agriculture, providing a context for archaeological investigations.


2018 ◽  
Vol 17 (2) ◽  
pp. 145-154 ◽  
Author(s):  
Fatima Noor Khan ◽  
Andrea M. Collins ◽  
Prateep Kumar Nayak ◽  
Derek Armitage

Author(s):  
Simon Niemeyer

AbstractModern challenges, such as global environmental change, cannot be dealt with via the generation of knowledge alone. Even in-principle public support requires broad recognition of responsibility to translate knowledge into appropriate action. This cannot be achieved where minds are closed, in which case greater levels of knowledge can actually feed into perverse outcomes. Overcoming these dynamics is facilitated to the extent that individuals adopt a deliberative stance (Owen D, Smith G, J Political Philosophy 23:213–234, 2015), which involves, inter alia, openness to ideas and hastens the rush to judgement on issues involving uncertainty and complexity—a scepticism of the self. In this paper, the author demonstrates the effects of the deliberative stance and the conditions under which it is best achieved. I draw my evidence from small-scale settings described by deliberative minipublics, but the observed mechanisms can be “scaled up” to inform possibilities for wider reform of the processes governing the uptake and use of knowledge.


2020 ◽  
Vol 4 (2) ◽  
pp. 105-120
Author(s):  
Gemechu Y Ofgeha ◽  
◽  
Muluneh W Abshire ◽  

Purpose: Global environmental change of climate variability and land use dynamics are emerging livelihood challenges facing local poor. Although, the synergetic impacts of these processes have been cognate in Ethiopia, vulnerability researches were fixed to climate variability, inadequate on conceptual and methodological considerations of non-climate stressors. To this attention, we assessed small-scale farmers’ vulnerability situations in Anger watershed of southwestern Ethiopia. Methods: The case study design guided by mixed methods approach was used. Multistage sampling technique was used for the study. The data collected from 335 household heads were analyzed by multivariate analysis, measures of differences, and substantiated by qualitative enquiry based on focus group discussions and observations. Result: Household’s vulnerability magnitude ranges from high to moderate, while in aggregate, kolla agroecology was more vulnerable than highland. The effects of social adaptability and sensitivity to land resources were significantly contributed for the vulnerability differences. Although, climate variability was notable, structural land use dynamics was unequivocal stressor deepened the household’s vulnerability in kolla. Conclusions: Vulnerability is the result of interactive and interconnected processes of climate, non-climate stressors, and households’ internal capacity in the study area. Thus, attributing local vulnerability to only climate variability, neglecting local non-climatic disturbances could mislead development planning. Hence, future studies should consider such processes simultaneously to provide comprehensive evidences on vulnerability situations. The national adaptations program needs to integrate climate change with the emerging other global changes in planning rural resilience. Policy fortifying agricultural investments should synchronize win-win strategy for relationships between investors and local community.


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